269 results on '"Alin, Simone"'
Search Results
2. CAN SEASONAL FORECASTS OF OCEAN CONDITIONS AID FISHERY MANAGERS? : EXPERIENCES FROM 10 YEARS OF J-SCOPE
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Siedlecki, Samantha Ann, Alin, Simone R., Norton, Emily L., Bond, Nicholas A., Hermann, Albert J., Feely, Richard A., and Newton, Jan A.
- Published
- 2023
3. EVALUATING THE EVOLVING OCEAN ACIDIFICATION RISK TO DUNGENESS CRAB : TIME-SERIES OBSERVATIONS AND MODELING ON THE OLYMPIC COAST, WASHINGTON, USA
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Alin, Simone R., Siedlecki, Samantha A., Berger, Halle, Feely, Richard A., Waddell, Jeannette E., Carter, Brendan R., Newton, Jan A., Schumacker, Ervin Joe, and Ayres, Daniel
- Published
- 2023
4. Best Practice Data Standards for Discrete Chemical Oceanographic Observations
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Jiang, Li-Qing, Pierrot, Denis, Wanninkhof, Rik, Feely, Richard A, Tilbrook, Bronte, Alin, Simone, Barbero, Leticia, Byrne, Robert H, Carter, Brendan R, Dickson, Andrew G, Gattuso, Jean-Pierre, Greeley, Dana, Hoppema, Mario, Humphreys, Matthew P, Karstensen, Johannes, Lange, Nico, Lauvset, Siv K, Lewis, Ernie R, Olsen, Are, Pérez, Fiz F, Sabine, Christopher, Sharp, Jonathan D, Tanhua, Toste, Trull, Thomas W, Velo, Anton, Allegra, Andrew J, Barker, Paul, Burger, Eugene, Cai, Wei-Jun, Chen, Chen-Tung A, Cross, Jessica, Garcia, Hernan, Hernandez-Ayon, Jose Martin, Hu, Xinping, Kozyr, Alex, Langdon, Chris, Lee, Kitack, Salisbury, Joe, Wang, Zhaohui Aleck, and Xue, Liang
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Life Below Water ,data standard for chemical oceanography ,discrete chemical oceanographic observations ,column header abbreviations ,WOCE WHP exchange formats ,quality control flags ,content vs.& nbsp ,concentration ,CO2SYS ,TEOS-10 ,Oceanography ,Ecology - Abstract
Effective data management plays a key role in oceanographic research as cruise-based data, collected from different laboratories and expeditions, are commonly compiled to investigate regional to global oceanographic processes. Here we describe new and updated best practice data standards for discrete chemical oceanographic observations, specifically those dealing with column header abbreviations, quality control flags, missing value indicators, and standardized calculation of certain properties. These data standards have been developed with the goals of improving the current practices of the scientific community and promoting their international usage. These guidelines are intended to standardize data files for data sharing and submission into permanent archives. They will facilitate future quality control and synthesis efforts and lead to better data interpretation. In turn, this will promote research in ocean biogeochemistry, such as studies of carbon cycling and ocean acidification, on regional to global scales. These best practice standards are not mandatory. Agencies, institutes, universities, or research vessels can continue using different data standards if it is important for them to maintain historical consistency. However, it is hoped that they will be adopted as widely as possible to facilitate consistency and to achieve the goals stated above.
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- 2022
5. Physiological responses of scallops and mussels to environmental variability: Implications for future shellfish aquaculture
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Alma, Lindsay, Fiamengo, Courtney J., Alin, Simone R., Jackson, Molly, Hiromoto, Kris, and Padilla-Gamiño, Jacqueline L.
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- 2023
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6. Controls on surface water carbonate chemistry along North American ocean margins.
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Cai, Wei-Jun, Xu, Yuan-Yuan, Feely, Richard, Wanninkhof, Rik, Jönsson, Bror, Alin, Simone, Barbero, Leticia, Cross, Jessica, Azetsu-Scott, Kumiko, Fassbender, Andrea, Carter, Brendan, Jiang, Li-Qing, Pepin, Pierre, Chen, Baoshan, Hussain, Najid, Reimer, Janet, Xue, Liang, Salisbury, Joseph, Hernández-Ayón, José, Langdon, Chris, Li, Qian, Sutton, Adrienne, Chen, Chen-Tung, and Gledhill, Dwight
- Abstract
Syntheses of carbonate chemistry spatial patterns are important for predicting ocean acidification impacts, but are lacking in coastal oceans. Here, we show that along the North American Atlantic and Gulf coasts the meridional distributions of dissolved inorganic carbon (DIC) and carbonate mineral saturation state (Ω) are controlled by partial equilibrium with the atmosphere resulting in relatively low DIC and high Ω in warm southern waters and the opposite in cold northern waters. However, pH and the partial pressure of CO2 (pCO2) do not exhibit a simple spatial pattern and are controlled by local physical and net biological processes which impede equilibrium with the atmosphere. Along the Pacific coast, upwelling brings subsurface waters with low Ω and pH to the surface where net biological production works to raise their values. Different temperature sensitivities of carbonate properties and different timescales of influencing processes lead to contrasting property distributions within and among margins.
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- 2020
7. Multi-Stressor Observations and Modeling to Build Understanding of and Resilience to the Coastal Impacts of Climate Change
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Newton, Jan, MacCready, Parker, Siedlecki, Samantha, Manalang, Dana, Mickett, John, Alin, Simone, Schumacker, Ervin “Joe”, Hagen, Jennifer, Moore, Stephanie, Sutton, Adrienne, and Carini, Roxanne
- Published
- 2021
8. The Combined Effects of Ocean Acidification and Respiration on Habitat Suitability for Marine Calcifiers Along the West Coast of North America
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Feely, Richard A., primary, Carter, Brendan R., additional, Alin, Simone R., additional, Greeley, Dana, additional, and Bednaršek, Nina, additional
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- 2024
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9. Climatological distribution of ocean acidification variables along the North American ocean margins.
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Jiang, Li-Qing, Boyer, Tim P., Paver, Christopher R., Yoo, Hyelim, Reagan, James R., Alin, Simone R., Barbero, Leticia, Carter, Brendan R., Feely, Richard A., and Wanninkhof, Rik
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OCEAN acidification ,FISHERIES ,HYDROGEN ions ,CARBON dioxide ,AQUACULTURE industry ,CALCITE - Abstract
Climatologies, which depict mean fields of oceanographic variables on a regular geographic grid, and atlases, which provide graphical depictions of specific areas, play pivotal roles in comprehending the societal vulnerabilities linked to ocean acidification (OA). This significance is particularly pronounced in coastal regions where most economic activities, such as commercial and recreational fisheries and aquaculture industries, occur. In this paper, we unveil a comprehensive data product featuring coastal ocean acidification climatologies and atlases, encompassing the fugacity of carbon dioxide, pH on the total scale, total hydrogen ion content, free hydrogen ion content, carbonate ion content, aragonite saturation state, calcite saturation state, Revelle factor, total dissolved inorganic carbon content, and total alkalinity content. These variables are provided on 1° × 1° spatial grids at 14 standardized depth levels, ranging from the surface to a depth of 500 m, along the North American ocean margins, defined as the region between the coastline and a distance of 200 nautical miles (∼370 km) offshore. The climatologies and atlases were developed using the World Ocean Atlas (WOA) gridding methods of the NOAA National Centers for Environmental Information (NCEI) based on the recently released Coastal Ocean Data Analysis Product in North America (CODAP-NA), along with the 2021 update to the Global Ocean Data Analysis Project version 2 (GLODAPv2.2021) data product. The relevant variables were adjusted to the index year of 2010. The data product is available in NetCDF (https://doi.org/10.25921/g8pb-zy76 , Jiang et al., 2022b) on the NOAA Ocean Carbon and Acidification Data System: https://www.ncei.noaa.gov/data/oceans/ncei/ocads/metadata/0270962.html (last access: 15 July 2024). It is recommended to use the objectively analyzed mean fields (with "_an" suffix) for each variable. The atlases can be accessed at https://www.ncei.noaa.gov/access/ocean-carbon-acidification-data-system/synthesis/nacoastal.html (last access: 15 July 2024). [ABSTRACT FROM AUTHOR]
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- 2024
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10. Climatological distribution of ocean acidification indicators along the North American ocean margins
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Jiang, Li-Qing, primary, Boyer, Tim P., additional, Paver, Christopher R., additional, Yoo, Hyelim, additional, Reagan, James R., additional, Alin, Simone R., additional, Barbero, Leticia, additional, Carter, Brendan R., additional, Feely, Richard A., additional, and Wanninkhof, Rik, additional
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- 2024
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11. Comment on essd-2023-445
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Alin, Simone R., primary
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- 2024
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12. Seasonality and response of ocean acidification and hypoxia to major environmental anomalies in the southern Salish Sea, North America (2014–2018).
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Alin, Simone R., Newton, Jan A., Feely, Richard A., Siedlecki, Samantha, and Greeley, Dana
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OCEAN acidification ,MARINE heatwaves ,TERRITORIAL waters ,HYPOXEMIA ,CARBON dioxide ,SOUTHERN oscillation ,CORAL reefs & islands - Abstract
Coastal and estuarine ecosystems fringing the North Pacific Ocean are particularly vulnerable to ocean acidification, hypoxia, and intense marine heatwaves as a result of interactions among natural and anthropogenic processes. Here, we characterize variability during a seasonally resolved cruise time series (2014–2018) in the southern Salish Sea (Puget Sound, Strait of Juan de Fuca) and nearby coastal waters for select physical (temperature, T ; salinity, S) and biogeochemical (oxygen, O 2 ; carbon dioxide fugacity, f CO 2 ; aragonite saturation state, Ωarag) parameters. Medians for some parameters peaked (T , Ωarag) in surface waters in summer, whereas others (S , O 2 , f CO 2) changed progressively across spring–fall, and all parameters changed monotonically or were relatively stable at depth. Ranges varied considerably for all parameters across basins within the study region, with stratified basins consistently the most variable. Strong environmental anomalies occurred during the time series, allowing us to also qualitatively assess how these anomalies affected seasonal patterns and interannual variability. The peak temperature anomaly associated with the 2013–2016 northeast Pacific marine heatwave–El Niño event was observed in boundary waters during the October 2014 cruise, but Puget Sound cruises revealed the largest temperature increases during the 2015–2016 timeframe. The most extreme hypoxia and acidification measurements to date were recorded in Hood Canal (which consistently had the most extreme conditions) during the same period; however, they were shifted earlier in the year relative to previous events. During autumn 2017, after the heat anomaly, a distinct carbonate system anomaly with unprecedentedly low Ωarag values and high f CO 2 values occurred in parts of the southern Salish Sea that are not normally so acidified. This novel "CO 2 storm" appears to have been driven by anomalously high river discharge earlier in 2017, which resulted in enhanced stratification and inferred primary productivity anomalies, indicated by persistently and anomalously high O 2 , low f CO 2 , and high chlorophyll. Unusually, this CO 2 anomaly was decoupled from O 2 dynamics compared with past Salish Sea hypoxia and acidification events. The complex interplay of weather, hydrological, and circulation anomalies revealed distinct multi-stressor scenarios that will potentially affect regional ecosystems under a changing climate. Further, the frequencies at which Salish cruise observations crossed known or preliminary species' sensitivity thresholds illustrates the relative risk landscape of temperature, hypoxia, and acidification anomalies in the southern Salish Sea in the present day, with implications for how multiple stressors may combine to present potential migration, survival, or physiological challenges to key regional species. The Salish cruise data product used in this publication is available at https://doi.org/10.25921/zgk5-ep63 (Alin et al., 2022), with an additional data product including all calculated CO 2 system parameters available at https://doi.org/10.25921/5g29-q841 (Alin et al., 2023). [ABSTRACT FROM AUTHOR]
- Published
- 2024
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13. Reply on RC1
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Alin, Simone R., primary
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- 2023
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14. Global Carbon Budget 2023
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Friedlingstein, Pierre, primary, O'Sullivan, Michael, additional, Jones, Matthew W., additional, Andrew, Robbie M., additional, Bakker, Dorothee C. E., additional, Hauck, Judith, additional, Landschützer, Peter, additional, Le Quéré, Corinne, additional, Luijkx, Ingrid T., additional, Peters, Glen P., additional, Peters, Wouter, additional, Pongratz, Julia, additional, Schwingshackl, Clemens, additional, Sitch, Stephen, additional, Canadell, Josep G., additional, Ciais, Philippe, additional, Jackson, Robert B., additional, Alin, Simone R., additional, Anthoni, Peter, additional, Barbero, Leticia, additional, Bates, Nicholas R., additional, Becker, Meike, additional, Bellouin, Nicolas, additional, Decharme, Bertrand, additional, Bopp, Laurent, additional, Brasika, Ida Bagus Mandhara, additional, Cadule, Patricia, additional, Chamberlain, Matthew A., additional, Chandra, Naveen, additional, Chau, Thi-Tuyet-Trang, additional, Chevallier, Frédéric, additional, Chini, Louise P., additional, Cronin, Margot, additional, Dou, Xinyu, additional, Enyo, Kazutaka, additional, Evans, Wiley, additional, Falk, Stefanie, additional, Feely, Richard A., additional, Feng, Liang, additional, Ford, Daniel J., additional, Gasser, Thomas, additional, Ghattas, Josefine, additional, Gkritzalis, Thanos, additional, Grassi, Giacomo, additional, Gregor, Luke, additional, Gruber, Nicolas, additional, Gürses, Özgür, additional, Harris, Ian, additional, Hefner, Matthew, additional, Heinke, Jens, additional, Houghton, Richard A., additional, Hurtt, George C., additional, Iida, Yosuke, additional, Ilyina, Tatiana, additional, Jacobson, Andrew R., additional, Jain, Atul, additional, Jarníková, Tereza, additional, Jersild, Annika, additional, Jiang, Fei, additional, Jin, Zhe, additional, Joos, Fortunat, additional, Kato, Etsushi, additional, Keeling, Ralph F., additional, Kennedy, Daniel, additional, Klein Goldewijk, Kees, additional, Knauer, Jürgen, additional, Korsbakken, Jan Ivar, additional, Körtzinger, Arne, additional, Lan, Xin, additional, Lefèvre, Nathalie, additional, Li, Hongmei, additional, Liu, Junjie, additional, Liu, Zhiqiang, additional, Ma, Lei, additional, Marland, Greg, additional, Mayot, Nicolas, additional, McGuire, Patrick C., additional, McKinley, Galen A., additional, Meyer, Gesa, additional, Morgan, Eric J., additional, Munro, David R., additional, Nakaoka, Shin-Ichiro, additional, Niwa, Yosuke, additional, O'Brien, Kevin M., additional, Olsen, Are, additional, Omar, Abdirahman M., additional, Ono, Tsuneo, additional, Paulsen, Melf, additional, Pierrot, Denis, additional, Pocock, Katie, additional, Poulter, Benjamin, additional, Powis, Carter M., additional, Rehder, Gregor, additional, Resplandy, Laure, additional, Robertson, Eddy, additional, Rödenbeck, Christian, additional, Rosan, Thais M., additional, Schwinger, Jörg, additional, Séférian, Roland, additional, Smallman, T. Luke, additional, Smith, Stephen M., additional, Sospedra-Alfonso, Reinel, additional, Sun, Qing, additional, Sutton, Adrienne J., additional, Sweeney, Colm, additional, Takao, Shintaro, additional, Tans, Pieter P., additional, Tian, Hanqin, additional, Tilbrook, Bronte, additional, Tsujino, Hiroyuki, additional, Tubiello, Francesco, additional, van der Werf, Guido R., additional, van Ooijen, Erik, additional, Wanninkhof, Rik, additional, Watanabe, Michio, additional, Wimart-Rousseau, Cathy, additional, Yang, Dongxu, additional, Yang, Xiaojuan, additional, Yuan, Wenping, additional, Yue, Xu, additional, Zaehle, Sönke, additional, Zeng, Jiye, additional, and Zheng, Bo, additional
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- 2023
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15. Supplementary material to "Global Carbon Budget 2023"
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Friedlingstein, Pierre, primary, O'Sullivan, Michael, additional, Jones, Matthew W., additional, Andrew, Robbie M., additional, Bakker, Dorothee C. E., additional, Hauck, Judith, additional, Landschützer, Peter, additional, Le Quéré, Corinne, additional, Luijkx, Ingrid T., additional, Peters, Glen P., additional, Peters, Wouter, additional, Pongratz, Julia, additional, Schwingshackl, Clemens, additional, Sitch, Stephen, additional, Canadell, Josep G., additional, Ciais, Philippe, additional, Jackson, Robert B., additional, Alin, Simone R., additional, Anthoni, Peter, additional, Barbero, Leticia, additional, Bates, Nicholas R., additional, Becker, Meike, additional, Bellouin, Nicolas, additional, Decharme, Bertrand, additional, Bopp, Laurent, additional, Brasika, Ida Bagus Mandhara, additional, Cadule, Patricia, additional, Chamberlain, Matthew A., additional, Chandra, Naveen, additional, Chau, Thi-Tuyet-Trang, additional, Chevallier, Frédéric, additional, Chini, Louise P., additional, Cronin, Margot, additional, Dou, Xinyu, additional, Enyo, Kazutaka, additional, Evans, Wiley, additional, Falk, Stefanie, additional, Feely, Richard A., additional, Feng, Liang, additional, Ford, Daniel. J., additional, Gasser, Thomas, additional, Ghattas, Josefine, additional, Gkritzalis, Thanos, additional, Grassi, Giacomo, additional, Gregor, Luke, additional, Gruber, Nicolas, additional, Gürses, Özgür, additional, Harris, Ian, additional, Hefner, Matthew, additional, Heinke, Jens, additional, Houghton, Richard A., additional, Hurtt, George C., additional, Iida, Yosuke, additional, Ilyina, Tatiana, additional, Jacobson, Andrew R., additional, Jain, Atul, additional, Jarníková, Tereza, additional, Jersild, Annika, additional, Jiang, Fei, additional, Jin, Zhe, additional, Joos, Fortunat, additional, Kato, Etsushi, additional, Keeling, Ralph F., additional, Kennedy, Daniel, additional, Klein Goldewijk, Kees, additional, Knauer, Jürgen, additional, Korsbakken, Jan Ivar, additional, Körtzinger, Arne, additional, Lan, Xin, additional, Lefèvre, Nathalie, additional, Li, Hongmei, additional, Liu, Junjie, additional, Liu, Zhiqiang, additional, Ma, Lei, additional, Marland, Greg, additional, Mayot, Nicolas, additional, McGuire, Patrick C., additional, McKinley, Galen A., additional, Meyer, Gesa, additional, Morgan, Eric J., additional, Munro, David R., additional, Nakaoka, Shin-Ichiro, additional, Niwa, Yosuke, additional, O'Brien, Kevin M., additional, Olsen, Are, additional, Omar, Abdirahman M., additional, Ono, Tsuneo, additional, Paulsen, Melf E., additional, Pierrot, Denis, additional, Pocock, Katie, additional, Poulter, Benjamin, additional, Powis, Carter M., additional, Rehder, Gregor, additional, Resplandy, Laure, additional, Robertson, Eddy, additional, Rödenbeck, Christian, additional, Rosan, Thais M., additional, Schwinger, Jörg, additional, Séférian, Roland, additional, Smallman, T. Luke, additional, Smith, Stephen M., additional, Sospedra-Alfonso, Reinel, additional, Sun, Qing, additional, Sutton, Adrienne J., additional, Sweeney, Colm, additional, Takao, Shintaro, additional, Tans, Pieter P., additional, Tian, Hanqin, additional, Tilbrook, Bronte, additional, Tsujino, Hiroyuki, additional, Tubiello, Francesco, additional, van der Werf, Guido R., additional, van Ooijen, Erik, additional, Wanninkhof, Rik, additional, Watanabe, Michio, additional, Wimart-Rousseau, Cathy, additional, Yang, Dongxu, additional, Yang, Xiaojuan, additional, Yuan, Wenping, additional, Yue, Xu, additional, Zaehle, Sönke, additional, Zeng, Jiye, additional, and Zheng, Bo, additional
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- 2023
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16. Pteropods make thinner shells in the upwelling region of the California Current Ecosystem
- Author
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Mekkes, Lisette, Renema, Willem, Bednaršek, Nina, Alin, Simone R., Feely, Richard A., Huisman, Jef, Roessingh, Peter, and Peijnenburg, Katja T. C. A.
- Published
- 2021
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17. Climatological distribution of ocean acidification indicators along the North American ocean margins.
- Author
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Jiang, Li-Qing, Boyer, Tim P., Paver, Christopher R., Yoo, Hyelim, Reagan, James R., Alin, Simone R., Barbero, Leticia, Carter, Brendan R., Feely, Richard A., and Wanninkhof, Rik
- Subjects
OCEAN acidification ,CALCITE ,FISHERIES ,OCEAN ,HYDROGEN ions ,CARBON dioxide - Abstract
Climatologies, which depict mean fields of oceanographic variables on a regular geographic grid, and atlases, which provide graphical depictions of specific areas, play pivotal roles in comprehending the societal vulnerabilities linked to ocean acidification (OA). This significance is particularly pronounced in coastal regions where most economic activities related to commercial and recreational fisheries as well as aquaculture industries occur. In this paper, we unveil a comprehensive data product featuring coastal climatologies and atlases for ten OA indicators, including fugacity of carbon dioxide, pH on the total scale, total hydrogen ion content, free hydrogen ion content, carbonate ion content, aragonite saturation state, calcite saturation state, Revelle Factor, total dissolved inorganic carbon content, and total alkalinity content. These indicators are provided on 1°×1° degree spatial grids at 14 standardized depth levels, ranging from the surface to a depth of 500 meters, along the North American ocean margins – defined as the region between the coastline and a distance of 200 nautical miles (∼370 km) offshore. The climatologies and atlases were developed using the World Ocean Atlas (WOA) gridding methods of the NOAA National Centers for Environmental Information (NCEI), based on the recently released Coastal Ocean Data Analysis Product in North America (CODAP-NA), along with the 2021 update to the Global Ocean Data Analysis Project version 2 (GLODAPv2.2021) data product. The relevant variables were adjusted to the index year of 2010. The data product is available in NetCDF (DOI: 10.25921/g8pb-zy76) at the NOAA Ocean Carbon and Acidification Data System: https://www.ncei.noaa.gov/data/oceans/ncei/ocads/metadata/0270962.html. It is recommended to use the objectively analyzed mean fields (with '_an' suffix) for each variable. The atlases can be accessed at: https://www.ncei.noaa.gov/access/ocean-carbon-acidification-data-system/synthesis/nacoastal.html. [ABSTRACT FROM AUTHOR]
- Published
- 2024
- Full Text
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18. A decade-long cruise time series (2008–2018) of physical and biogeochemical conditions in the southern Salish Sea, North America.
- Author
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Alin, Simone R., Newton, Jan A., Feely, Richard A., Greeley, Dana, Curry, Beth, Herndon, Julian, and Warner, Mark
- Subjects
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HYPOXIA (Water) , *DISSOLVED oxygen in water , *TIME series analysis , *WATER quality management , *TERRITORIAL waters , *MARINE heatwaves , *OCEAN acidification , *AMMONIUM - Abstract
Coastal and estuarine waters of the northern California Current system and southern Salish Sea host an observational network capable of characterizing biogeochemical dynamics related to ocean acidification, hypoxia, and marine heatwaves. Here, we compiled data sets from a set of cruises conducted in estuarine waters of Puget Sound (southern Salish Sea) and its boundary waters (Strait of Juan de Fuca and Washington coast). This data product provides data from a decade of cruises with consistent formatting, extended data quality control, and multiple units for parameters such as oxygen with different end use needs and conventions. All cruises obtained high-quality temperature, salinity, inorganic carbon, nutrient, and oxygen observations to provide insight into the dynamic distribution of physical and biogeochemical conditions in this large urban estuary complex on the west coast of North America. At all sampling stations, conductivity–temperature–depth (CTD) casts included sensors for measuring temperature, conductivity, pressure, and oxygen concentrations. Laboratory analyses of discrete water samples collected at all stations throughout the water column in Niskin bottles provided measurements of dissolved inorganic carbon (DIC), dissolved oxygen, nutrient (nitrate, nitrite, ammonium, phosphate, and silicate), and total alkalinity (TA) content. This data product includes observations from 35 research cruises, including 715 oceanographic profiles, with >7490 sensor measurements of temperature, salinity, and oxygen; ≥6070 measurements of discrete oxygen and nutrient samples; and ≥4462 measurements of inorganic carbon variables (i.e., DIC and TA). The observations comprising this cruise compilation collectively characterize the spatial and temporal variability in a region with large dynamic ranges of the physical (temperature = 6.0–21.8 ∘ C, salinity = 15.6–34.0) and biogeochemical (oxygen = 12–481 µmolkg-1 , dissolved inorganic carbon = 1074–2362 µmolkg-1 , total alkalinity = 1274–2296 µmolkg-1) parameters central to understanding ocean acidification and hypoxia in this productive estuary system with numerous interacting human impacts on its ecosystems. All observations conform to the climate-quality observing guidelines of the Global Ocean Acidification Observing Network, the US National Oceanic and Atmospheric Administration's Ocean Acidification Program, and ocean carbon community best practices. This ongoing cruise time series supports the estuarine and coastal monitoring and research objectives of the Washington Ocean Acidification Center and US National Oceanic and Atmospheric Administration (NOAA) Ocean and Atmospheric Research programs, and it provides diverse end users with the information needed to frame biological impacts research, validate numerical models, inform state and tribal water quality and fisheries management, and support decision-makers. All 2008–2018 cruise time-series measurements used in this publication are available at 10.25921/zgk5-ep63 (Alin et al., 2022). [ABSTRACT FROM AUTHOR]
- Published
- 2024
- Full Text
- View/download PDF
19. Supplementary material to "A decade-long cruise time-series (2008–2018) of physical and biogeochemical conditions in the southern Salish Sea, North America"
- Author
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Alin, Simone R., primary, Newton, Jan A., additional, Feely, Richard A., additional, Greeley, Dana, additional, Curry, Beth, additional, Herndon, Julian, additional, and Warner, Mark, additional
- Published
- 2023
- Full Text
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20. A decade-long cruise time-series (2008–2018) of physical and biogeochemical conditions in the southern Salish Sea, North America
- Author
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Alin, Simone R., primary, Newton, Jan A., additional, Feely, Richard A., additional, Greeley, Dana, additional, Curry, Beth, additional, Herndon, Julian, additional, and Warner, Mark, additional
- Published
- 2023
- Full Text
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21. Age of riverine carbon suggests rapid export of terrestrial primary production in tropics
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Martin, Erin E, Ingalls, Anitra E, Richey, Jeffrey E, Keil, Richard G, Santos, Guaciara M, Truxal, Laura T, Alin, Simone R, and Druffel, Ellen R. M
- Subjects
Mekong ,lignin ,residence time ,tropics ,radiocarbon - Abstract
The balance between the storage of vascular plant carbon in soils, oxidation to carbon dioxide, and export via rivers affects calculations of the strength of terrestrial ecosystems as carbon sinks. The magnitude and timescale of the riverine export pathway are not well constrained. Here we use radiocarbon dating of lignin phenols to show that plant-derived carbon carried by suspended sediment of the Mekong River is very young, having been produced within the last 18 years. Further, this plant-derived carbon remains young during times of the year when bulk carbon varies from modern to over 3000 radiocarbon years old. Our results demonstrate that primary-production derivatives are exported rapidly and suggest that the age of riverine lignin is similar to estimates of the residence time of terrestrial organic carbon in tropical catchments. These results are relevant for modeling predictions of the influence of the terrestrial biosphere on atmospheric carbon dioxide levels.
- Published
- 2013
22. Robust empirical relationships for estimating the carbonate system in the southern California Current System and application to CalCOFI hydrographic cruise data (2005–2011)
- Author
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Alin, Simone R, Feely, Richard A, Dickson, Andrew G, Hernández‐Ayón, J Martín, Juranek, Lauren W, Ohman, Mark D, and Goericke, Ralf
- Subjects
Life Below Water ,Meteorology & Atmospheric Sciences - Abstract
The California Current System (CCS) is expected to experience the ecological impacts of ocean acidification (OA) earlier than most other ocean regions because coastal upwelling brings old, CO2-rich water relatively close to the surface ocean. Historical inorganic carbon measurements are scarce, so the progression of OA in the CCS is unknown. We used a multiple linear regression approach to generate empirical models using oxygen (O 2), temperature (T), salinity (S), and sigma theta (sq) as proxy variables to reconstruct pH, carbonate saturation states, carbonate ion concentration ([CO32-]), dissolved inorganic carbon (DIC) concentration, and total alkalinity (TA) in the southern CCS. The calibration data included high-quality measurements of carbon, oxygen, and other hydrographic variables, collected during a cruise from British Columbia to Baja California in May-June 2007. All resulting empirical relationships were robust, with r2 values >0.92 and low root mean square errors. Estimated and measured carbon chemistry matched very well for independent data sets from the CalCOFI and IMECOCAL programs. Reconstructed CCS pH and saturation states for 2005-2011 reveal a pronounced seasonal cycle and inter-annual variability in the upper water column. Deeper in the water column, conditions are stable throughout the annual cycle, with perennially low pH and saturation states. Over sub-decadal time scales, these empirical models provide a valuable tool for reconstructing carbonate chemistry related to ocean acidification where direct observations are limited. However, progressive increases in anthropogenic CO2 content of southern CCS water masses must be carefully addressed to apply the models over longer time scales. © Copyright 2012 by the American Geophysical Union.
- Published
- 2012
23. The Live, the Dead, and the Very Dead: Taphonomic Calibration of the Recent Record of Paleoecological Change in Lake Tanganyika, East Africa
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Alin, Simone R. and Cohen, Andrew S.
- Published
- 2004
24. Estimating Total Alkalinity in the Washington State Coastal Zone: Complexities and Surprising Utility for Ocean Acidification Research
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Fassbender, Andrea J., Alin, Simone R., Feely, Richard A., Sutton, Adrienne J., Newton, Jan A., and Byrne, Robert H.
- Published
- 2017
25. Seasonality and response of ocean acidification and hypoxia to major environmental anomalies in the southern Salish Sea, North America (2014-2018).
- Author
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Alin, Simone R., Newton, Jan A., Feely, Richard A., Siedlecki, Samantha, and Greeley, Dana
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OCEAN acidification ,MARINE heatwaves ,HYPOXEMIA ,TERRITORIAL waters ,SPRING ,SOUTHERN oscillation ,CORAL reefs & islands - Abstract
Coastal and estuarine ecosystems fringing the North Pacific Ocean are particularly vulnerable to ocean acidification, hypoxia, and intense marine heatwaves as a result of interactions among natural and anthropogenic processes. Here we characterize variability during a seasonally resolved cruise time series in the southern Salish Sea (Puget Sound, Strait of Juan de Fuca) and nearby coastal waters for select physical (temperature, T; salinity, S) and biogeochemical (oxygen, O
2 ; carbon dioxide fugacity, fCO2 ; aragonite saturation state, Ωarag) parameters. Medians for some parameters peaked (T, Ωarag) in surface waters in summer, while others (S, O2 , fCO2 ) changed progressively across spring--fall, and all parameters changed monotonically or were relatively stable at depth. Ranges varied considerably for all parameters across basins within the study region, with stratified basins consistently the most variable. Strong environmental anomalies occurred during the time series, allowing us to also qualitatively assess how these anomalies affected seasonal patterns and interannual variability. The peak temperature anomaly associated with the 2013-2016 northeast Pacific marine heatwave--El Nino event was observed in boundary waters during the October 2014 cruise, but Puget Sound cruises revealed the largest temperature increases during 2015--2016 timeframe. The most extreme hypoxia and acidification measurements to date were recorded in Hood Canal (which consistently has the most extreme conditions) during the same period; however, they were shifted earlier in the year relative to previous events. During autumn 2017, after the heat anomaly, a distinct carbonate system anomaly with unprecedentedly low Ωarag and high fCO2 occurred in parts of the southern Salish Sea that are not normally so acidified. This novel "CO2 storm" appears to have been driven by anomalous river discharge earlier in 2017, which resulted in enhanced stratification and inferred primary productivity anomalies, indicated by persistently and anomalously high O2 , low fCO2 , and high chlorophyll. Unusually, this CO2 anomaly was decoupled from O2 dynamics compared to past Salish Sea hypoxia and acidification events. The complex interplay of weather, hydrological, and circulation anomalies revealed distinct multiple stressor scenarios that will potentially affect regional ecosystems under a changing climate. Further, the frequencies at which Salish cruise observations crossed known or preliminary species sensitivity thresholds illustrates the relative risk landscape of temperature, hypoxia, and acidification anomalies in the southern Salish Sea in the present-day, with implications for how multiple stressors may combine to present potential migration, survival, or physiological challenges to key regional species in the future. [ABSTRACT FROM AUTHOR]- Published
- 2023
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26. Effects of Landscape Disturbance on Animal Communities in Lake Tanganyika, East Africa
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Alin, Simone R., Cohen, Andrew S., Bills, Roger, Gashagaza, Masta Mukwaya, Michel, Ellinor, Tiercelin, Jean-Jacques, Martens, Koen, Coveliers, Peter, Mboko, Sima Keita, West, Kelly, Soreghan, Michael, Kimbadi, Sona, and Ntakimazi, Gaspard
- Published
- 1999
27. Chemical and biological impacts of ocean acidification along the west coast of North America
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Feely, Richard A., Alin, Simone R., Carter, Brendan, Bednaršek, Nina, Hales, Burke, Chan, Francis, Hill, Tessa M., Gaylord, Brian, Sanford, Eric, Byrne, Robert H., Sabine, Christopher L., Greeley, Dana, and Juranek, Lauren
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- 2016
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28. Global Surface Ocean Acidification Indicators From 1750 to 2100
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Jiang, Li‐Qing, primary, Dunne, John, additional, Carter, Brendan R., additional, Tjiputra, Jerry F., additional, Terhaar, Jens, additional, Sharp, Jonathan D., additional, Olsen, Are, additional, Alin, Simone, additional, Bakker, Dorothee C. E., additional, Feely, Richard A., additional, Gattuso, Jean‐Pierre, additional, Hogan, Patrick, additional, Ilyina, Tatiana, additional, Lange, Nico, additional, Lauvset, Siv K., additional, Lewis, Ernie R., additional, Lovato, Tomas, additional, Palmieri, Julien, additional, Santana‐Falcón, Yeray, additional, Schwinger, Jörg, additional, Séférian, Roland, additional, Strand, Gary, additional, Swart, Neil, additional, Tanhua, Toste, additional, Tsujino, Hiroyuki, additional, Wanninkhof, Rik, additional, Watanabe, Michio, additional, Yamamoto, Akitomo, additional, and Ziehn, Tilo, additional
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- 2023
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29. Seasonal ocean forecasts to improve predictions of Dungeness crab catch rates, co-developed with state and tribal fishery managers
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Norton, Emily L, primary, Kaplan, Isaac C, additional, Siedlecki, Samantha, additional, Hermann, Albert J, additional, Alin, Simone R, additional, Newton, Jan, additional, Corbett, Kelly, additional, Ayres, Daniel, additional, Schumacker, Ervin Joe, additional, Bond, Nicholas A, additional, Richerson, Kate, additional, and Alexander, Michael A, additional
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- 2023
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30. Effects of the Pandemic on Observing the Global Ocean
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Boyer, Tim, primary, Zhang, Huai-Min, additional, O’Brien, Kevin, additional, Reagan, James, additional, Diggs, Stephen, additional, Freeman, Eric, additional, Garcia, Hernan, additional, Heslop, Emma, additional, Hogan, Patrick, additional, Huang, Boyin, additional, Jiang, Li-Qing, additional, Kozyr, Alex, additional, Liu, Chunying, additional, Locarnini, Ricardo, additional, Mishonov, Alexey V., additional, Paver, Christopher, additional, Wang, Zhankun, additional, Zweng, Melissa, additional, Alin, Simone, additional, Barbero, Leticia, additional, Barth, John A., additional, Belbeoch, Mathieu, additional, Cebrian, Just, additional, Connell, Kenneth J., additional, Cowley, Rebecca, additional, Dukhovskoy, Dmitry, additional, Galbraith, Nancy R., additional, Goni, Gustavo, additional, Katz, Fred, additional, Kramp, Martin, additional, Kumar, Arun, additional, Legler, David M., additional, Lumpkin, Rick, additional, McMahon, Clive R., additional, Pierrot, Denis, additional, Plueddemann, Albert J., additional, Smith, Emily A., additional, Sutton, Adrienne, additional, Turpin, Victor, additional, Jiang, Long, additional, Suneel, V., additional, Wanninkhof, Rik, additional, Weller, Robert A., additional, and Wong, Annie P. S., additional
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- 2023
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31. Global surface ocean acidification indicators from 1750 to 2100
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Jiang, Li‐Qing, Dunne, John, Carter, Brendan R., Tjiputra, Jerry F., Terhaar, Jens, Sharp, Jonathan D., Olsen, Are, Alin, Simone, Bakker, Dorothee C. E., Feely, Richard A., Gattuso, Jean‐Pierre, Hogan, Patrick, Ilyina, Tatiana, Lange, Nico, Lauvset, Siv K., Lewis, Ernie R., Lovato, Tomas, Palmieri, Julien, Santana‐Falcón, Yeray, Schwinger, Jörg, Séférian, Roland, Strand, Gary, Swart, Neil, Tanhua, Toste, Tsujino, Hiroyuki, Wanninkhof, Rik, Watanabe, Michio, Yamamoto, Akitomo, and Ziehn, Tilo
- Subjects
Shared Socioeconomic Pathways ,global surface ocean ,Global and Planetary Change ,aragonite saturation state ,pH ,Earth System Models ,ocean acidification indicators ,General Earth and Planetary Sciences ,Environmental Chemistry - Abstract
Accurately predicting future ocean acidification (OA) conditions is crucial for advancing OA research at regional and global scales, and guiding society's mitigation and adaptation efforts. This study presents a new model-data fusion product covering 10 global surface OA indicators based on 14 Earth System Models (ESMs) from the Coupled Model Intercomparison Project Phase 6 (CMIP6), along with three recent observational ocean carbon data products. The indicators include fugacity of carbon dioxide, pH on total scale, total hydrogen ion content, free hydrogen ion content, carbonate ion content, aragonite saturation state, calcite saturation state, Revelle Factor, total dissolved inorganic carbon content, and total alkalinity content. The evolution of these OA indicators is presented on a global surface ocean 1 degrees x 1 degrees grid as decadal averages every 10 years from preindustrial conditions (1750), through historical conditions (1850-2010), and to five future Shared Socioeconomic Pathways (2020-2100): SSP1-1.9, SSP1-2.6, SSP2-4.5, SSP3-7.0, and SSP5-8.5. These OA trajectories represent an improvement over previous OA data products with respect to data quantity, spatial and temporal coverage, diversity of the underlying data and model simulations, and the provided SSPs. The generated data product offers a state-of-the-art research and management tool for the 21st century under the combined stressors of global climate change and ocean acidification. The gridded data product is available in NetCDF at the National Oceanic and Atmospheric Administration (NOAA) National Centers for Environmental Information: https://www.ncei.noaa.gov/data/oceans/ncei/ocads/metadata/0259391.html, and global maps of these indicators are available in jpeg at: https://www.ncei.noaa.gov/access/ocean-carbon-acidification-datasystem/synthesis/surface-oa-indicators.html. Plain Language Summary A new data product, based on the latest computer simulations and observational data, offers improved projections of ocean acidification (OA) conditions from the start of the Industrial Revolution in 1750 to the end of the 21st century. These projections will support OA research at regional and global scales, and provide essential information to guide OA mitigation and adaptation efforts for various sectors, including fisheries, aquaculture, tourism, marine resource decision-makers, and the general public.
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- 2023
32. A decade-long cruise time-series (2008-2018) of physical and biogeochemical conditions in the southern Salish Sea, North America.
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Alin, Simone R., Newton, Jan A., Feely, Richard A., Greeley, Dana, Curry, Beth, Herndon, Julian, and Warner, Mark
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- *
HYPOXIA (Water) , *DISSOLVED oxygen in water , *WATER quality management , *TERRITORIAL waters , *MARINE heatwaves , *OCEAN acidification , *PHYSICAL training & conditioning , *AMMONIUM - Abstract
Coastal and estuarine waters of the northern California Current System and southern Salish Sea host an observational network capable of characterizing biogeochemical dynamics related to ocean acidification, hypoxia, and marine heatwaves. Here we compiled data sets from a set of cruises conducted in estuarine waters of Puget Sound (southern Salish Sea) and its boundary waters (Strait of Juan de Fuca and Washington coast). This data product provides data from a decade of cruises with consistent formatting, extended data quality control, and multiple units for parameters such as oxygen with different end use needs and conventions. All cruises obtained high-quality temperature, salinity, inorganic carbon, nutrient, and oxygen observations to provide insight into the dynamic distribution of physical and biogeochemical conditions in this large urban estuary complex on the west coast of North America. At all sampling stations, CTD casts included sensors for measuring temperature, conductivity, pressure, and oxygen concentrations. Laboratory analyses of discrete water samples collected at all stations throughout the water column in Niskin bottles provided measurements of dissolved inorganic carbon (DIC), dissolved oxygen, nutrient (nitrate, nitrite, ammonium, phosphate, silicate), and total alkalinity (TA) content. This data product includes observations from 35 research cruises, including 715 oceanographic profiles, with >7490 sensor measurements of temperature, salinity, and oxygen; =6070 measurements of discrete oxygen and nutrient samples; and =4462 measurements of inorganic carbon variables (i.e., DIC and TA). The observations comprising this cruise compilation collectively characterize the spatial and temporal variability of a region with large dynamic ranges of the physical (temperature = 6.0-21.8 °C, salinity = 15.6-34.0) and biogeochemical parameters (oxygen = 12-481 µmol kg-1, dissolved inorganic carbon = 1074-2362 µmol kg-1, total alkalinity = 1274-2296 µmol kg-1) central to understanding ocean acidification and hypoxia in this productive estuary system with numerous interacting human impacts on its ecosystems. All observations conform to the climate-quality observing guidelines of the Global Ocean Acidification Observing Network, the U.S. National Oceanic and Atmospheric Administration's Ocean Acidification Program, and ocean carbon community best practices. This on-going cruise time-series supports the estuarine and coastal monitoring and research objectives of the Washington Ocean Acidification Center and U.S. National Oceanic and Atmospheric Administration (NOAA) Ocean and Atmospheric Research programs, and provides diverse end users information needed to frame biological impacts research, validate numerical models, inform state and tribal water quality and fisheries management, and support decision makers. All 2008-2018 cruise time-series measurements used in this publication are available at https://doi.org/10.25921/zgk5-ep63 (Alin et al., 2022). [ABSTRACT FROM AUTHOR]
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- 2023
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33. Advancing best practices for assessing trends of ocean acidification time series
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Sutton, Adrienne J., primary, Battisti, Roman, additional, Carter, Brendan, additional, Evans, Wiley, additional, Newton, Jan, additional, Alin, Simone, additional, Bates, Nicholas R., additional, Cai, Wei-Jun, additional, Currie, Kim, additional, Feely, Richard A., additional, Sabine, Christopher, additional, Tanhua, Toste, additional, Tilbrook, Bronte, additional, and Wanninkhof, Rik, additional
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- 2022
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34. GLODAPv2.2022: the latest version of the global interior ocean biogeochemical data product
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Lauvset, Siv K., primary, Lange, Nico, additional, Tanhua, Toste, additional, Bittig, Henry C., additional, Olsen, Are, additional, Kozyr, Alex, additional, Alin, Simone, additional, Álvarez, Marta, additional, Azetsu-Scott, Kumiko, additional, Barbero, Leticia, additional, Becker, Susan, additional, Brown, Peter J., additional, Carter, Brendan R., additional, da Cunha, Leticia Cotrim, additional, Feely, Richard A., additional, Hoppema, Mario, additional, Humphreys, Matthew P., additional, Ishii, Masao, additional, Jeansson, Emil, additional, Jiang, Li-Qing, additional, Jones, Steve D., additional, Lo Monaco, Claire, additional, Murata, Akihiko, additional, Müller, Jens Daniel, additional, Pérez, Fiz F., additional, Pfeil, Benjamin, additional, Schirnick, Carsten, additional, Steinfeldt, Reiner, additional, Suzuki, Toru, additional, Tilbrook, Bronte, additional, Ulfsbo, Adam, additional, Velo, Anton, additional, Woosley, Ryan J., additional, and Key, Robert M., additional
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- 2022
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35. Global Carbon Budget 2022
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Friedlingstein, Pierre, primary, O'Sullivan, Michael, additional, Jones, Matthew W., additional, Andrew, Robbie M., additional, Gregor, Luke, additional, Hauck, Judith, additional, Le Quéré, Corinne, additional, Luijkx, Ingrid T., additional, Olsen, Are, additional, Peters, Glen P., additional, Peters, Wouter, additional, Pongratz, Julia, additional, Schwingshackl, Clemens, additional, Sitch, Stephen, additional, Canadell, Josep G., additional, Ciais, Philippe, additional, Jackson, Robert B., additional, Alin, Simone R., additional, Alkama, Ramdane, additional, Arneth, Almut, additional, Arora, Vivek K., additional, Bates, Nicholas R., additional, Becker, Meike, additional, Bellouin, Nicolas, additional, Bittig, Henry C., additional, Bopp, Laurent, additional, Chevallier, Frédéric, additional, Chini, Louise P., additional, Cronin, Margot, additional, Evans, Wiley, additional, Falk, Stefanie, additional, Feely, Richard A., additional, Gasser, Thomas, additional, Gehlen, Marion, additional, Gkritzalis, Thanos, additional, Gloege, Lucas, additional, Grassi, Giacomo, additional, Gruber, Nicolas, additional, Gürses, Özgür, additional, Harris, Ian, additional, Hefner, Matthew, additional, Houghton, Richard A., additional, Hurtt, George C., additional, Iida, Yosuke, additional, Ilyina, Tatiana, additional, Jain, Atul K., additional, Jersild, Annika, additional, Kadono, Koji, additional, Kato, Etsushi, additional, Kennedy, Daniel, additional, Klein Goldewijk, Kees, additional, Knauer, Jürgen, additional, Korsbakken, Jan Ivar, additional, Landschützer, Peter, additional, Lefèvre, Nathalie, additional, Lindsay, Keith, additional, Liu, Junjie, additional, Liu, Zhu, additional, Marland, Gregg, additional, Mayot, Nicolas, additional, McGrath, Matthew J., additional, Metzl, Nicolas, additional, Monacci, Natalie M., additional, Munro, David R., additional, Nakaoka, Shin-Ichiro, additional, Niwa, Yosuke, additional, O'Brien, Kevin, additional, Ono, Tsuneo, additional, Palmer, Paul I., additional, Pan, Naiqing, additional, Pierrot, Denis, additional, Pocock, Katie, additional, Poulter, Benjamin, additional, Resplandy, Laure, additional, Robertson, Eddy, additional, Rödenbeck, Christian, additional, Rodriguez, Carmen, additional, Rosan, Thais M., additional, Schwinger, Jörg, additional, Séférian, Roland, additional, Shutler, Jamie D., additional, Skjelvan, Ingunn, additional, Steinhoff, Tobias, additional, Sun, Qing, additional, Sutton, Adrienne J., additional, Sweeney, Colm, additional, Takao, Shintaro, additional, Tanhua, Toste, additional, Tans, Pieter P., additional, Tian, Xiangjun, additional, Tian, Hanqin, additional, Tilbrook, Bronte, additional, Tsujino, Hiroyuki, additional, Tubiello, Francesco, additional, van der Werf, Guido R., additional, Walker, Anthony P., additional, Wanninkhof, Rik, additional, Whitehead, Chris, additional, Willstrand Wranne, Anna, additional, Wright, Rebecca, additional, Yuan, Wenping, additional, Yue, Chao, additional, Yue, Xu, additional, Zaehle, Sönke, additional, Zeng, Jiye, additional, and Zheng, Bo, additional
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- 2022
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36. Spatiotemporal Assessment of CO2–Carbonic Acid System Dynamics in a Pristine Coral Reef Ecosystem, French Frigate Shoals, Northwestern Hawaiian Islands
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Kealoha, Andrea K., Mackenzie, Fred T., Kahng, Samuel E., Kosaki, Randall K., Alin, Simone R., and Winn, Christopher D.
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- 2017
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37. Characterizing the Natural System : Toward Sustained, Integrated Coastal Ocean Acidification Observing Networks to Facilitate Resource Management and Decision Support
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Alin, Simone R., Brainard, Russell E., Price, Nichole N., Newton, Jan A., Cohen, Anne, Peterson, William T., DeCarlo, Eric H., Shadwick, Elizabeth H., Noakes, Scott, and Bednaršek, Nina
- Published
- 2015
38. Biogeochemical Effects of Rising Atmospheric CO2 on Terrestrial and Ocean Systems
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Moore, David J. P, Cooley, Sarah R, Alin, Simone R, Butman, David E, Clow, David W, French, Nancy H. F, Feely, Richard A, Johnson, Zackary, Keppel-Aleks, Gretchen, Lohrenz, Steven E, Ocko, Ilissa, Shadwick, Elizabeth H, Sutton, Adrienne J, Potter, Christopher S, Takatsuka, Yuki, and Yu, Rita
- Subjects
Earth Resources And Remote Sensing - Abstract
Rising carbon dioxide (CO2) has decreased seawater pH at long-term observing stations around the world, including in the open ocean north of Oahu, Hawaii, near Alaska's Aleutian Islands, the Gulf of Maine shore, and on Gray's Reef in the southeastern United States. This ocean acidification process has already affected some marine species and altered fundamental ecosystem processes, and further effects are likely. While atmospheric CO rises at approximately the same rate all over the globe, its non-climate effects on land vary depending on climate and dominant species. In terrestrial ecosystems, rising atmospheric CO concentrations are expected to increase plant photosynthesis, growth, and water-use efficiency, though these effects are reduced when nutrients, drought or other factors limit plant growth. Rising CO would likely change carbon storage and influence terrestrial hydrology and biogeochemical cycling, but concomitant effects on vegetation composition and nutrient feedbacks are challenging to predict, making decadal forecasts uncertain. Consequences of rising atmospheric CO are expected to include difficult-to-predict changes in the ecosystem services that terrestrial and ocean systems provide to humans. For instance, ocean acidification resulting from rising CO has decreased the supply of larvae that sustains commercial shellfish production in the northwestern United States. In addition, CO fertilization (increases) plus warming (decreases) are changing terrestrial crop yields. Continued persistence of uptake of carbon by the land and ocean is uncertain. Climate and environmental change create complex feedbacks to the carbon cycle and it is not clear how feedbacks modulate future effects of rising CO on carbon sinks. These are several mechanisms that could reduce future sink capacity.
- Published
- 2018
39. Supplementary material to "Global Carbon Budget 2022"
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Friedlingstein, Pierre, primary, O'Sullivan, Michael, additional, Jones, Matthew W., additional, Andrew, Robbie M., additional, Gregor, Luke, additional, Hauck, Judith, additional, Le Quéré, Corinne, additional, Luijkx, Ingrid T., additional, Olsen, Are, additional, Peters, Glen P., additional, Peters, Wouter, additional, Pongratz, Julia, additional, Schwingshackl, Clemens, additional, Sitch, Stephen, additional, Canadell, Josep G., additional, Ciais, Philippe, additional, Jackson, Robert B., additional, Alin, Simone R., additional, Alkama, Ramdane, additional, Arneth, Almut, additional, Arora, Vivek K., additional, Bates, Nicholas R., additional, Becker, Meike, additional, Bellouin, Nicolas, additional, Bittig, Henry C., additional, Bopp, Laurent, additional, Chevallier, Frédéric, additional, Chini, Louise P., additional, Cronin, Margot, additional, Evans, Wiley, additional, Falk, Stefanie, additional, Feely, Richard A., additional, Gasser, Thomas, additional, Gehlen, Marion, additional, Gkritzalis, Thanos, additional, Gloege, Lucas, additional, Grassi, Giacomo, additional, Gruber, Nicolas, additional, Gürses, Özgür, additional, Harris, Ian, additional, Hefner, Matthew, additional, Houghton, Richard A., additional, Hurtt, George C., additional, Iida, Yosuke, additional, Ilyina, Tatiana, additional, Jain, Atul K., additional, Jersild, Annika, additional, Kadono, Koji, additional, Kato, Etsushi, additional, Kennedy, Daniel, additional, Klein Goldewijk, Kees, additional, Knauer, Jürgen, additional, Korsbakken, Jan Ivar, additional, Landschützer, Peter, additional, Lefèvre, Nathalie, additional, Lindsay, Keith, additional, Liu, Junjie, additional, Liu, Zhu, additional, Marland, Gregg, additional, Mayot, Nicolas, additional, McGrath, Matthew J., additional, Metzl, Nicolas, additional, Monacci, Natalie M., additional, Munro, David R., additional, Nakaoka, Shin-Ichiro, additional, Niwa, Yosuke, additional, O'Brien, Kevin, additional, Ono, Tsuneo, additional, Palmer, Paul I., additional, Pan, Naiqing, additional, Pierrot, Denis, additional, Pocock, Katie, additional, Poulter, Benjamin, additional, Resplandy, Laure, additional, Robertson, Eddy, additional, Rödenbeck, Christian, additional, Rodriguez, Carmen, additional, Rosan, Thais M., additional, Schwinger, Jörg, additional, Séférian, Roland, additional, Shutler, Jamie D., additional, Skjelvan, Ingunn, additional, Steinhoff, Tobias, additional, Sun, Qing, additional, Sutton, Adrienne J., additional, Sweeney, Colm, additional, Takao, Shintaro, additional, Tanhua, Toste, additional, Tans, Pieter P., additional, Tian, Xiangjun, additional, Tian, Hanqin, additional, Tilbrook, Bronte, additional, Tsujino, Hiroyuki, additional, Tubiello, Francesco, additional, van der Werf, Guido, additional, Walker, Anthony P., additional, Wanninkhof, Rik, additional, Whitehead, Chris, additional, Willstrand Wranne, Anna, additional, Wright, Rebecca, additional, Yuan, Wenping, additional, Yue, Chao, additional, Yue, Xu, additional, Zaehle, Sönke, additional, Zeng, Jiye, additional, and Zheng, Bo, additional
- Published
- 2022
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40. Supplementary material to "GLODAPv2.2022: the latest version of the global interior ocean biogeochemical data product"
- Author
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Lauvset, Siv K., primary, Lange, Nico, additional, Tanhua, Toste, additional, Bittig, Henry C., additional, Olsen, Are, additional, Kozyr, Alex, additional, Alin, Simone R., additional, Álvarez, Marta, additional, Azetsu-Scott, Kumiko, additional, Barbero, Leticia, additional, Becker, Susan, additional, Brown, Peter J., additional, Carter, Brendan R., additional, da Cunha, Leticia Cotrim, additional, Feely, Richard A., additional, Hoppema, Mario, additional, Humphreys, Matthew P., additional, Ishii, Masao, additional, Jeansson, Emil, additional, Jiang, Li-Qing, additional, Jones, Steve D., additional, Lo Monaco, Claire, additional, Murata, Akihiko, additional, Müller, Jens Daniel, additional, Pérez, Fiz F., additional, Pfeil, Benjamin, additional, Schirnick, Carsten, additional, Steinfeldt, Reiner, additional, Suzuki, Toru, additional, Tilbrook, Bronte, additional, Ulfsbo, Adam, additional, Velo, Anton, additional, Woosley, Ryan J., additional, and Key, Robert M., additional
- Published
- 2022
- Full Text
- View/download PDF
41. Global Carbon Budget 2021
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Friedlingstein, Pierre, Jones, Matthew W., O'Sullivan, Michael, Andrew, Robbie M., Bakker, Dorothee C.E., Hauck, Judith, Le Quéré, Corinne, Peters, Glen P., Peters, Wouter, Pongratz, Julia, Sitch, Stephen, Canadell, Josep G., Ciais, Philippe, Jackson, Rob B., Alin, Simone R., Anthoni, Peter, Bates, Nicholas R., Becker, Meike, Bellouin, Nicolas, Bopp, Laurent, Chau, Thi Tuyet Trang, Chevallier, Frédéric, Chini, Louise P., Cronin, Margot, Currie, Kim I., Decharme, Bertrand, Djeutchouang, Laique M., Dou, Xinyu, Evans, Wiley, Feely, Richard A., Feng, Liang, Gasser, Thomas, Gilfillan, Dennis, Gkritzalis, Thanos, Grassi, Giacomo, Gregor, Luke, Gruber, Nicolas, Gürses, Özgür, Harris, Ian, Houghton, Richard A., Hurtt, George C., Iida, Yosuke, Ilyina, Tatiana, Luijkx, Ingrid T., Jain, Atul, Jones, Steve D., Kato, Etsushi, Kennedy, Daniel, Goldewijk, Kees Klein, Knauer, Jürgen, Korsbakken, Jan Ivar, Körtzinger, Arne, Landschützer, Peter, Lauvset, Siv K., Lefèvre, Nathalie, Lienert, Sebastian, Liu, Junjie, Marland, Gregg, McGuire, Patrick C., Melton, Joe R., Munro, David R., Nabel, Julia E.M.S., Nakaoka, Shin Ichiro, Niwa, Yosuke, Ono, Tsuneo, Pierrot, Denis, Poulter, Benjamin, Rehder, Gregor, Resplandy, Laure, Robertson, Eddy, Rödenbeck, Christian, Rosan, Thais M., Schwinger, Jörg, Schwingshackl, Clemens, Séférian, Roland, Sutton, Adrienne J., Sweeney, Colm, Tanhua, Toste, Tans, Pieter P., Tian, Hanqin, Tilbrook, Bronte, Tubiello, Francesco, Van Der Werf, Guido R., Vuichard, Nicolas, Wada, Chisato, Wanninkhof, Rik, Watson, Andrew J., Willis, David, Wiltshire, Andrew J., Yuan, Wenping, Yue, Chao, Yue, Xu, Zaehle, Sönke, Zeng, Jiye, Integr. Assessm. Global Environm. Change, and Environmental Sciences
- Subjects
Earth and Planetary Sciences(all) - Abstract
Accurate assessment of anthropogenic carbon dioxide (CO2) emissions and their redistribution among the atmosphere, ocean, and terrestrial biosphere in a changing climate is critical to better understand the global carbon cycle, support the development of climate policies, and project future climate change. Here we describe and synthesize datasets and methodology to quantify the five major components of the global carbon budget and their uncertainties. Fossil CO2 emissions (EFOS) are based on energy statistics and cement production data, while emissions from land-use change (ELUC), mainly deforestation, are based on land use and land-use change data and bookkeeping models. Atmospheric CO2 concentration is measured directly, and its growth rate (GATM) is computed from the annual changes in concentration. The ocean CO2 sink (SOCEAN) is estimated with global ocean biogeochemistry models and observation-based data products. The terrestrial CO2 sink (SLAND) is estimated with dynamic global vegetation models. The resulting carbon budget imbalance (BIM), the difference between the estimated total emissions and the estimated changes in the atmosphere, ocean, and terrestrial biosphere, is a measure of imperfect data and understanding of the contemporary carbon cycle. All uncertainties are reported as ±1σ. For the first time, an approach is shown to reconcile the difference in our ELUC estimate with the one from national greenhouse gas inventories, supporting the assessment of collective countries' climate progress. For the year 2020, EFOS declined by 5.4% relative to 2019, with fossil emissions at 9.5±0.5GtCyr-1 (9.3±0.5GtCyr-1 when the cement carbonation sink is included), and ELUC was 0.9±0.7GtCyr-1, for a total anthropogenic CO2 emission of 10.2±0.8GtCyr-1 (37.4±2.9GtCO2). Also, for 2020, GATM was 5.0±0.2GtCyr-1 (2.4±0.1ppmyr-1), SOCEAN was 3.0±0.4GtCyr-1, and SLAND was 2.9±1GtCyr-1, with a BIM of -0.8GtCyr-1. The global atmospheric CO2 concentration averaged over 2020 reached 412.45±0.1ppm. Preliminary data for 2021 suggest a rebound in EFOS relative to 2020 of +4.8% (4.2% to 5.4%) globally. Overall, the mean and trend in the components of the global carbon budget are consistently estimated over the period 1959-2020, but discrepancies of up to 1GtCyr-1 persist for the representation of annual to semi-decadal variability in CO2 fluxes. Comparison of estimates from multiple approaches and observations shows (1) a persistent large uncertainty in the estimate of land-use changes emissions, (2) a low agreement between the different methods on the magnitude of the land CO2 flux in the northern extra-tropics, and (3) a discrepancy between the different methods on the strength of the ocean sink over the last decade. This living data update documents changes in the methods and datasets used in this new global carbon budget and the progress in understanding of the global carbon cycle compared with previous publications of this dataset (Friedlingstein et al., 2020, 2019; Le Quéré et al., 2018b, a, 2016, 2015b, a, 2014, 2013). The data presented in this work are available at 10.18160/gcp-2021 (Friedlingstein et al., 2021).
- Published
- 2022
42. Latitudinal Trends and Drivers in the CO2–Carbonic Acid System of Papahānaumokuākea Marine National Monument
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Kealoha, Andrea K., Kahng, Samuel E., Mackenzie, Fred T., Alin, Simone R., Kosaki, Randall K., Brainard, Russell E., and Winn, Christopher D.
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- 2015
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43. Seasonal variation in dissolved carbon concentrations and fluxes in the upper Purus River, southwestern Amazon
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Salimon, Cleber, dos Santos Sousa, Eliete, Alin, Simone R., Krusche, Alex Vladimir, and Ballester, Maria Victoria
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- 2013
44. Best Practice Data Standards for Discrete Chemical Oceanographic Observations
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Jiang, Li-Qing, primary, Pierrot, Denis, additional, Wanninkhof, Rik, additional, Feely, Richard A., additional, Tilbrook, Bronte, additional, Alin, Simone, additional, Barbero, Leticia, additional, Byrne, Robert H., additional, Carter, Brendan R., additional, Dickson, Andrew G., additional, Gattuso, Jean-Pierre, additional, Greeley, Dana, additional, Hoppema, Mario, additional, Humphreys, Matthew P., additional, Karstensen, Johannes, additional, Lange, Nico, additional, Lauvset, Siv K., additional, Lewis, Ernie R., additional, Olsen, Are, additional, Pérez, Fiz F., additional, Sabine, Christopher, additional, Sharp, Jonathan D., additional, Tanhua, Toste, additional, Trull, Thomas W., additional, Velo, Anton, additional, Allegra, Andrew J., additional, Barker, Paul, additional, Burger, Eugene, additional, Cai, Wei-Jun, additional, Chen, Chen-Tung A., additional, Cross, Jessica, additional, Garcia, Hernan, additional, Hernandez-Ayon, Jose Martin, additional, Hu, Xinping, additional, Kozyr, Alex, additional, Langdon, Chris, additional, Lee, Kitack, additional, Salisbury, Joe, additional, Wang, Zhaohui Aleck, additional, and Xue, Liang, additional
- Published
- 2022
- Full Text
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45. Physiological Responses of Scallops and Mussels to Environmental Variability: Implications for Future Shellfish Aquaculture
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Alma, Lindsay, primary, Fiamengo, Courtney J., additional, Alin, Simone R., additional, Jackson, Molly, additional, Hiromoto, Kris, additional, and Padilla-Gamiño, Jacqueline L., additional
- Published
- 2022
- Full Text
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46. Riverine coupling of biogeochemical cycles between land, oceans, and atmosphere
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Aufdenkampe, Anthony K, Mayorga, Emilio, Raymond, Peter A, Melack, John M, Doney, Scott C, Alin, Simone R, Aalto, Rolf E, and Yoo, Kyungsoo
- Published
- 2011
47. State of the Carbon Cycle - Consequences of Rising Atmospheric CO2
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Moore, David J, Cooley, Sarah R, Alin, Simone R, Brown, Molly, Butman, David E, French, Nancy H. F, Johnson, Zackary I, Keppel-Aleks, Lohrenz, Steven E, Ocko, Ilissa, Shadwick, Elizabeth H, Sutton, Adrienne J, Potter, Christopher S, and Yu, Rita M. S
- Subjects
Earth Resources And Remote Sensing - Abstract
The rise of atmospheric CO2, largely attributable to human activity through fossil fuel emissions and land-use change, has been dampened by carbon uptake by the ocean and terrestrial biosphere. We outline the consequences of this carbon uptake as direct and indirect effects on terrestrial and oceanic systems and processes for different regions of North America and the globe. We assess the capacity of these systems to continue to act as carbon sinks. Rising CO2 has decreased seawater pH; this process of ocean acidification has impacted some marine species and altered fundamental ecosystem processes with further effects likely. In terrestrial ecosystems, increased atmospheric CO2 causes enhanced photosynthesis, net primary production, and increased water-use efficiency. Rising CO2 may change vegetation composition and carbon storage, and widespread increases in water use efficiency likely influence terrestrial hydrology and biogeochemical cycling. Consequences for human populations include changes to ecosystem services including cultural activities surrounding land use, agricultural or harvesting practices. Commercial fish stocks have been impacted and crop production yields have been changed as a result of rising CO2. Ocean and terrestrial effects are contingent on, and feedback to, global climate change. Warming and modified precipitation regimes impact a variety of ecosystem processes, and the combination of climate change and rising CO2 contributes considerable uncertainty to forecasting carbon sink capacity in the ocean and on land. Disturbance regime (fire and insects) are modified with increased temperatures. Fire frequency and intensity increase, and insect lifecycles are disrupted as temperatures move out of historical norms. Changes in disturbance patterns modulate the effects of rising CO2 depending on ecosystem type, disturbance frequency, and magnitude of events. We discuss management strategies designed to limit the rise of atmospheric CO2 and reduce uncertainty in forecasts of decadal and centennial feedbacks of rising atmospheric CO2 on carbon storage.
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- 2016
48. Global Carbon Budget 2016
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Quéré, Corinne Le, Andrew, Robbie M, Canadell, Josep G, Sitch, Stephen, Korsbakken, Jan Ivar, Peters, Glen P, Manning, Andrew C, Boden, Thomas A, Tans, Pieter P, Houghton, Richard A, Keeling, Ralph F, Alin, Simone, Andrews, Oliver D, Anthoni, Peter, Barbero, Leticia, Bopp, Laurent, Chevallier, Frédéric, Chini, Louise P, Ciais, Philippe, Currie, Kim, Delire, Christine, Doney, Scott C, Friedlingstein, Pierre, Gkritzalis, Thanos, Harris, Ian, Hauck, Judith, Haverd, Vanessa, Hoppema, Mario, Goldewijk, Kees Klein, Jain, Atul K, Kato, Etsushi, Koertzinger, Arne, Landschuetzer, Peter, Lefèvre, Nathalie, Lenton, Andrew, Lienert, Sebastian, Lombardozzi, Danica, Melton, Joe R, Metzl, Nicolas, Millero, Frank, Monteiro, Pedro M. S, Munro, David R, Nabel, Julia E. M. S, Nakaoka, Shin-ichiro, O’Brien, Kevin, Olsen, Are, Omar, Abdirahman M, Ono, Tsuneo, Pierrot, Denis, Poulter, Benjamin, Roedenbeck, Christian, Salisbury, Joe, Schuster, Ute, Schwinger, Joerg, Séférian, Roland, Skjelvan, Ingunn, Stocker, Benjamin D, Sutton, Adrienne J, Takahashi, Taro, Tian, Hanqin, Tilbrook, Bronte, van der Laan-Luijkx, Ingrid T, van der Werf, Guido R, Viovy, Nicolas, Walker, Anthony P, Wiltshire, Andrew J, and Zaehle, Soenke
- Subjects
Meteorology And Climatology - Abstract
Accurate assessment of anthropogenic carbon dioxide (CO2) emissions and their redistribution among the atmosphere, ocean, and terrestrial biosphere the global carbon budget is important to better understand the global carbon cycle, support the development of climate policies, and project future climate change. Here we describe data sets and methodology to quantify all major components of the global carbon budget, including their uncertainties, based on the combination of a range of data, algorithms, statistics, and model estimates and their interpretation by a broad scientific community. We discuss changes compared to previous estimates and consistency within and among components, alongside methodology and data limitations. CO2 emissions from fossil fuels and industry (EFF) are based on energy statistics and cement production data, respectively, while emissions from land-use change (ELUC), mainly deforestation, are based on combined evidence from land-cover change data, fire activity associated with deforestation, and models. The global atmospheric CO2 concentration is measured directly and its rate of growth (GATM) is computed from the annual changes in concentration. The mean ocean CO2 sink (SOCEAN) is based on observations from the 1990s, while the annual anomalies and trends are estimated with ocean models. The variability in SOCEAN is evaluated with data products based on surveys of ocean CO2 measurements. The global residual terrestrial CO2 sink (SLAND) is estimated by the difference of the other terms of the global carbon budget and compared to results of independent dynamic global vegetation models. We compare the mean land and ocean fluxes and their variability to estimates from three atmospheric inverse methods for three broad latitude bands. All uncertainties are reported as +/- 1(sigma), reflecting the current capacity to characterize the annual estimates of each component of the global carbon budget. For the last decade available (2006-2015), EFF was 9.3+/-0.5 GtC/yr, ELUC 1.0+/-0.5 GtC/yr,GATM 4.5+/-0.1 GtC/yr, SOCEAN 2.6+/-0.5 GtC/yr, and SLAND 3.1+/-0.9 GtC/yr. For year 2015 alone, the growth in EFF was approximately zero and emissions remained at 9.9+/-0.5 GtC/yr, showing a slowdown in growth of these emissions compared to the average growth of 1.8/yr that took place during 2006-2015.Also, for 2015, ELUC was 1.3+/-0.5 GtC/yr, GATM was 6.3+/-0.2 GtC/yr, SOCEAN was 3.0+/-0.5 GtC/yr, and SLAND was 1.9+/-0.9 GtC/yr. GATM was higher in 2015 compared to the past decade (2006-2015), reflecting a smaller SLAND for that year. The global atmospheric CO2 concentration reached 399.4+/-0.1 ppm averaged over 2015. For 2016, preliminary data indicate the continuation of low growth in EFF with +0.2% (range of -1.0 to +1.8% ) based on national emissions projections for China and USA, and projections of gross domestic product corrected for recent changes in the carbon intensity of the economy for the rest of the world. In spite of the low growth of EFF in 2016, the growth rate in atmospheric CO2 concentration is expected to be relatively high because of the persistence of the smaller residual terrestrial sink (SLAND) in response to El Nino conditions of 2015-2016. From this projection of EFF and assumed constant ELUC for 2016, cumulative emissions of CO2 will reach 565+/-55 GtC (2075+/-205 GtCO2) for 1870-2016, about 75% from EFF and 25% from ELUC. This living data update documents changes in the methods and data sets used in this new carbon budget compared with previous publications of this data set.
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- 2016
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49. OCEAN ACIDIFICATION IN THE CALIFORNIA CURRENT SYSTEM
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HAURI, CLAUDINE, GRUBER, NICOLAS, PLATTNER, GIAN-KASPER, ALIN, SIMONE, FEELY, RICHARD A., HALES, BURKE, and WHEELER, PATRICIA A.
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- 2009
50. Global Carbon Budget 2021
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Friedlingstein, Pierre, primary, Jones, Matthew W., additional, O'Sullivan, Michael, additional, Andrew, Robbie M., additional, Bakker, Dorothee C. E., additional, Hauck, Judith, additional, Le Quéré, Corinne, additional, Peters, Glen P., additional, Peters, Wouter, additional, Pongratz, Julia, additional, Sitch, Stephen, additional, Canadell, Josep G., additional, Ciais, Philippe, additional, Jackson, Rob B., additional, Alin, Simone R., additional, Anthoni, Peter, additional, Bates, Nicholas R., additional, Becker, Meike, additional, Bellouin, Nicolas, additional, Bopp, Laurent, additional, Chau, Thi T. T., additional, Chevallier, Frédéric, additional, Chini, Louise P., additional, Cronin, Margot, additional, Currie, Kim I., additional, Decharme, Bertrand, additional, Djeutchouang, Laique, additional, Dou, Xinyu, additional, Evans, Wiley, additional, Feely, Richard A., additional, Feng, Liang, additional, Gasser, Thomas, additional, Gilfillan, Dennis, additional, Gkritzalis, Thanos, additional, Grassi, Giacomo, additional, Gregor, Luke, additional, Gruber, Nicolas, additional, Gürses, Özgür, additional, Harris, Ian, additional, Houghton, Richard A., additional, Hurtt, George C., additional, Iida, Yosuke, additional, Ilyina, Tatiana, additional, Luijkx, Ingrid T., additional, Jain, Atul K., additional, Jones, Steve D., additional, Kato, Etsushi, additional, Kennedy, Daniel, additional, Klein Goldewijk, Kees, additional, Knauer, Jürgen, additional, Korsbakken, Jan Ivar, additional, Körtzinger, Arne, additional, Landschützer, Peter, additional, Lauvset, Siv K., additional, Lefèvre, Nathalie, additional, Lienert, Sebastian, additional, Liu, Junjie, additional, Marland, Gregg, additional, McGuire, Patrick C., additional, Melton, Joe R., additional, Munro, David R., additional, Nabel, Julia E. M. S., additional, Nakaoka, Shin-Ichiro, additional, Niwa, Yosuke, additional, Ono, Tsuneo, additional, Pierrot, Denis, additional, Poulter, Benjamin, additional, Rehder, Gregor, additional, Resplandy, Laure, additional, Robertson, Eddy, additional, Rödenbeck, Christian, additional, Rosan, Thais M., additional, Schwinger, Jörg, additional, Schwingshackl, Clemens, additional, Séférian, Roland, additional, Sutton, Adrienne J., additional, Sweeney, Colm, additional, Tanhua, Toste, additional, Tans, Pieter P., additional, Tian, Hanqin, additional, Tilbrook, Bronte, additional, Tubiello, Francesco, additional, van der Werf, Guido, additional, Vuichard, Nicolas, additional, Wada, Chisato, additional, Wanninkhof, Rik, additional, Watson, Andrew, additional, Willis, David, additional, Wiltshire, Andrew J., additional, Yuan, Wenping, additional, Yue, Chao, additional, Yue, Xu, additional, Zaehle, Sönke, additional, and Zeng, Jiye, additional
- Published
- 2021
- Full Text
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