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1. Rainfall on the Greenland Ice Sheet: Present‐Day Climatology From a High‐Resolution Non‐Hydrostatic Polar Regional Climate Model.

Author

Niwano, M., Box, J. E., Wehrlé, A., Vandecrux, B., Colgan, W. T., and Cappelen, J.

Subjects
*GREENLAND ice, *ICE sheets, *POLAR climate, *ATMOSPHERIC models, *CLIMATOLOGY, *MELTWATER
Abstract

Greenland ice sheet rainfall is expected to increase under a warming climate. Yet, there have been no active long‐term in‐situ rainfall records on the ice sheet due to observational difficulties. Here, we utilize the state‐of‐the‐art 5 km polar non‐hydrostatic regional climate model NHM‐SMAP to evaluate the ice sheet's rainfall over 40 years (1980–2019). The largest trends include a fourfold increase in annual rainfall for the northwestern ice sheet; 3.1 Gt year−1 or 12 mm m−2 year−1. September ice‐sheet‐wide rainfall amount and intensity increase by 7.5 Gt month−1 and 20.8 mm h−1 year−1. In the last two decades, the increasing September maximum hourly rainfall rate exceeded 50 mm h−1 six times. The increased surface water delivery has numerous implications, including for snow metamorphism and ice flow dynamics. Plain Language Summary: We find that rainfall has increased over the Greenland ice sheet from 1980 to 2019. Among the eight major ice‐sheet drainage areas, the northwestern sector stands out as an increasing rainfall hotspot where the annual rainfall has increased fourfold. For the entire ice sheet, September's total rainfall and its intensity increased by 224% and 54% above the 1981–2010 baseline over the last 40 years. An increase in late melt season rainfall is expected to contribute to an increase in late summer snow and ice melt. Our results provide the first detailed quantification of the state of ice sheet rainfall climatology. Key Points: A 5 km horizontal resolution non‐hydrostatic regional climate model is used to evaluate Greenland ice sheet rainfall from 1980 to 2019The northwestern sector stands out as a hotspot of increasing rainfallBoth the amount and intensity of September ice‐sheet‐wide rainfall have significantly increased in the 40 years from 1980 to 2019 [ABSTRACT FROM AUTHOR]

Published
2021
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2. State of the climate in 2016

Author

Aaron-Morrison, A. P., Ackerman, S. A., Adams, N. G., Adler, R. F., Albanil, A., Alfaro, E. J., Allan, R., Alves, L. M., Amador, J. A., Andreassen, L. M., Arendt, A., Arévalo, J., Arndt, D. S., Arzhanova, N. M., Aschan, M. M., Azorin-Molina, C., Banzon, V., Bardin, M. U., Barichivich, J., Baringer, M. O., Barreira, S., Baxter, S., Bazo, J., Becker, A., Bedka, K. M., Behrenfeld, M. J., Bell, G. D., Belmont, M., Benedetti, A., Bernhard, G., Berrisford, P., Berry, D. I., Bettolli, M. L., Bhatt, U. S., Bidegain, M., Bill, B. D., Billheimer, S., Bissolli, P., Blake, E. S., Blunden, J., Bosilovich, M. G., Boucher, O., Boudet, D., Box, J. E., Boyer, T., Braathen, G. O., Bromwich, D. H., Brown, R., Bulygina, O. N., Burgess, D., Calderón, B., Camargo, S. J., Campbell, J. D., Cappelen, J., Carrasco, G., Carter, B. R., Chambers, D. P., Chandler, E., Christiansen, H. H., Christy, J. R., Chung, D., Chung, E. S., Cinque, K., Clem, K. R., Coelho, C. A., Cogley, J. G., Coldewey-Egbers, M., Colwell, S., Cooper, O. R., Copland, L., Cosca, C. E., Cross, J. N., Crotwell, M. J., Crouch, J., Davis, S. M., Eyto, E., Jeu, R. A. M., Laat, J., Degasperi, C. L., Degenstein, D., Demircan, M., Derksen, C., Destin, D., Di Girolamo, L., Di Giuseppe, F., Diamond, H. J., Dlugokencky, E. J., Dohan, K., Dokulil, M. T., Dolgov, A. V., Dolman, A. J., Domingues, C. M., Donat, M. G., Dong, S., Dorigo, W. A., Dortch, Q., Doucette, G., Drozdov, D. S., Ducklow, H., Dunn, R. J. H., Durán-Quesada, A. M., Dutton, G. S., Ebrahim, A., Elkharrim, M., Elkins, J. W., Espinoza, J. C., Etienne-Leblanc, S., Evans, T. E., Famiglietti, J. S., Farrell, S., Fateh, S., Fausto, R. S., Fedaeff, N., Feely, R. A., Feng, Z., Fenimore, C., Fettweis, X., Fioletov, V. E., Flemming, J., Fogarty, C. T., Fogt, R. L., Folland, C., Fonseca, C., Fossheim, M., Foster, M. J., Fountain, A., Francis, S. D., Franz, B. A., Frey, R. A., Frith, S. M., Froidevaux, L., Ganter, C., Garzoli, S., Gerland, S., Gobron, N., Goldenberg, S. B., Gomez, R. S., Goni, G., Goto, A., Grooß, J. U., Gruber, A., Guard, C. C., Gugliemin, M., Gupta, S. K., Gutiérrez, J. M., Hagos, S., Hahn, S., Haimberger, L., Hakkarainen, J., Hall, B. D., Halpert, M. S., Hamlington, B. D., Hanna, E., Hansen, K., Hanssen-Bauer, I., Harris, I., Heidinger, A. K., Heikkilä, A., Heil, A., Heim, R. R., Hendricks, S., Hernández, M., Hidalgo, H. G., Hilburn, K., Ho, S. P. B., Holmes, R. M., Hu, Z. Z., Huang, B., Huelsing, H. K., Huffman, G. J., Hughes, C., Hurst, D. F., Ialongo, I., Ijampy, J. A., Ingvaldsen, R. B., Inness, A., Isaksen, K., Ishii, M., Jevrejeva, S., Jiménez, C., Jin, X., Johannesen, E., John, V., Johnsen, B., Johnson, B., Johnson, G. C., Jones, P. D., Joseph, A. C., Jumaux, G., Kabidi, K., Kaiser, J. W., Kato, S., Kazemi, A., Keller, L. M., Kendon, M., Kennedy, J., Kerr, K., Kholodov, A. L., Khoshkam, M., Killick, R., Kim, H., Kim, S. J., Kimberlain, T. B., Klotzbach, P. J., Knaff, J. A., Kobayashi, S., Kohler, J., Korhonen, J., Korshunova, N. N., Kovacs, K. M., Kramarova, N., Kratz, D. P., Kruger, A., Kruk, M. C., Kudela, R., Kumar, A., Lakatos, M., Lakkala, K., Lander, M. A., Landsea, C. W., Lankhorst, M., Lantz, K., Lazzara, M. A., Lemons, P., Leuliette, E., L’heureux, M., Lieser, J. L., Lin, I. I., Liu, H., Liu, Y., Locarnini, R., Loeb, N. G., Lo Monaco, C., Long, C. S., López Álvarez, L. A., Lorrey, A. M., Loyola, D., Lumpkin, R., Luo, J. J., Luojus, K., Lydersen, C., Lyman, J. M., Maberly, S. C., Maddux, B. C., Malheiros Ramos, A., Malkova, G. V., Manney, G., Marcellin, V., Marchenko, S. S., Marengo, J. A., Marra, J. J., Marszelewski, W., Martens, B., Martínez-Güingla, R., Massom, R. A., Mata, M. M., Mathis, J. T., May, L., Mayer, M., Mazloff, M., Mcbride, C., Mccabe, M. F., Mccarthy, M., Mcclelland, J. W., Mcgree, S., Mcvicar, T. R., Mears, C. A., Meier, W., Meinen, C. S., Mekonnen, A., Menéndez, M., Mengistu Tsidu, G., Menzel, W. P., Merchant, C. J., Meredith, M. P., Merrifield, M. A., Metzl, N., Minnis, P., Miralles, D. G., Mistelbauer, T., Mitchum, G. T., Monselesan, D., Monteiro, P., Montzka, S. A., Morice, C., Mote, T., Mudryk, L., Mühle, J., Mullan, A. B., Nash, E. R., Naveira-Garabato, A. C., Nerem, R. S., Newman, P. A., Nieto, J. J., Noetzli, J., O’neel, S., Osborn, T. J., Overland, J., Oyunjargal, L., Parinussa, R. M., Park, E. H., Parker, D., Parrington, M., Parsons, A. R., Pasch, R. J., Pascual-Ramírez, R., Paterson, A. M., Paulik, C., Pearce, P. R., Pelto, M. S., Peng, L., Perkins-Kirkpatrick, S. E., Perovich, D., Petropavlovskikh, I., Pezza, A. B., Phillips, D., Pinty, B., Pitts, M. C., Pons, M. R., Porter, A. O., Primicerio, R., Proshutinsky, A., Quegan, S., Quintana, J., Rahimzadeh, F., Rajeevan, M., Randriamarolaza, L., Razuvaev, V. N., Reagan, J., Reid, P., Reimer, C., Rémy, S., Renwick, J. A., Revadekar, J. V., Richter-Menge, J., Riffler, M., Rimmer, A., Rintoul, S., Robinson, D. A., Rodell, M., Rodríguez Solís, J. L., Romanovsky, V. E., Ronchail, J., Rosenlof, K. H., Roth, C., Rusak, J. A., Sabine, C. L., Sallée, J. B., Sánchez-Lugo, A., Santee, M. L., Sawaengphokhai, P., Sayouri, A., Scambos, T. A., Schemm, J., Schladow, S. G., Schmid, C., Schmid, M., Schmidtko, S., Schreck, C. J., Selkirk, H. B., Send, U., Sensoy, S., Setzer, A., Sharp, M., Shaw, A., Shi, L., Shiklomanov, A. I., Shiklomanov, N. I., Siegel, D. A., Signorini, S. R., Sima, F., Simmons, A. J., Smeets, C. J. P. P., Smith, S. L., Spence, J. M., Srivastava, A. K., Stackhouse, P. W., Stammerjohn, S., Steinbrecht, W., Stella, J. L., Stengel, M., Stennett-Brown, R., Stephenson, T. S., Strahan, S., Streletskiy, D. A., Sun-Mack, S., Swart, S., Sweet, W., Talley, L. D., Tamar, G., Tank, S. E., Taylor, M. A., Tedesco, M., Teubner, K., Thoman, R. L., Thompson, P., Thomson, L., Timmermans, M. L., Maxim Timofeyev, Tirnanes, J. A., Tobin, S., Trachte, K., Trainer, V. L., Tretiakov, M., Trewin, B. C., Trotman, A. R., Tschudi, M., As, D., Wal, R. S. W., A, R. J., Schalie, R., Schrier, G., Werf, G. R., Meerbeeck, C. J., Velicogna, I., Verburg, P., Vigneswaran, B., Vincent, L. A., Volkov, D., Vose, R. S., Wagner, W., Wåhlin, A., Wahr, J., Walsh, J., Wang, C., Wang, J., Wang, L., Wang, M., Wang, S. H., Wanninkhof, R., Watanabe, S., Weber, M., Weller, R. A., Weyhenmeyer, G. A., Whitewood, R., Wijffels, S. E., Wilber, A. C., Wild, J. D., Willett, K. M., Williams, M. J. M., Willie, S., Wolken, G., Wong, T., Wood, E. F., Woolway, R. I., Wouters, B., Xue, Y., Yamada, R., Yim, S. Y., Yin, X., Young, S. H., Yu, L., Zahid, H., Zambrano, E., Zhang, P., Zhao, G., Zhou, L., Ziemke, J. R., Love-Brotak, S. E., Gilbert, K., Maycock, T., Osborne, S., Sprain, M., Veasey, S. W., Ambrose, B. J., Griffin, J., Misch, D. J., Riddle, D. B., Young, T., Macias Fauria, M, Blunden, J, Arndt, D, Earth and Climate, Faculty of Earth and Life Sciences, Clinical Developmental Psychology, Climate Change and Landscape Dynamics, and Molecular Cell Physiology

Subjects
Meteor (satellite), Atmospheric Science, 010504 meteorology & atmospheric sciences, 0208 environmental biotechnology, 02 engineering and technology, 01 natural sciences, 020801 environmental engineering, Geography, 13. Climate action, Climatology, SDG 13 - Climate Action, SDG 14 - Life Below Water, 0105 earth and related environmental sciences
Abstract

In 2016, the dominant greenhouse gases released into Earth's atmosphere-carbon dioxide, methane, and nitrous oxide-continued to increase and reach new record highs. The 3.5 +/- 0.1 ppm rise in global annual mean carbon dioxide from 2015 to 2016 was the largest annual increase observed in the 58-year measurement record. The annual global average carbon dioxide concentration at Earth's surface surpassed 400 ppm (402.9 +/- 0.1 ppm) for the first time in the modern atmospheric measurement record and in ice core records dating back as far as 800000 years. One of the strongest El Nino events since at least 1950 dissipated in spring, and a weak La Nina evolved later in the year. Owing at least in part to the combination of El Nino conditions early in the year and a long-term upward trend, Earth's surface observed record warmth for a third consecutive year, albeit by a much slimmer margin than by which that record was set in 2015. Above Earth's surface, the annual lower troposphere temperature was record high according to all datasets analyzed, while the lower stratospheric temperature was record low according to most of the in situ and satellite datasets. Several countries, including Mexico and India, reported record high annual temperatures while many others observed near-record highs. A week-long heat wave at the end of April over the northern and eastern Indian peninsula, with temperatures surpassing 44 degrees C, contributed to a water crisis for 330 million people and to 300 fatalities. In the Arctic the 2016 land surface temperature was 2.0 degrees C above the 1981-2010 average, breaking the previous record of 2007, 2011, and 2015 by 0.8 degrees C, representing a 3.5 degrees C increase since the record began in 1900. The increasing temperatures have led to decreasing Arctic sea ice extent and thickness. On 24 March, the sea ice extent at the end of the growth season saw its lowest maximum in the 37-year satellite record, tying with 2015 at 7.2% below the 1981-2010 average. The September 2016 Arctic sea ice minimum extent tied with 2007 for the second lowest value on record, 33% lower than the 1981-2010 average. Arctic sea ice cover remains relatively young and thin, making it vulnerable to continued extensive melt. The mass of the Greenland Ice Sheet, which has the capacity to contribute similar to 7 m to sea level rise, reached a record low value. The onset of its surface melt was the second earliest, after 2012, in the 37-year satellite record. Sea surface temperature was record high at the global scale, surpassing the previous record of 2015 by about 0.01 degrees C. The global sea surface temperature trend for the 21st century-to-date of +0.162 degrees C decade(-1) is much higher than the longer term 1950-2016 trend of +0.100 degrees C decade(-1). Global annual mean sea level also reached a new record high, marking the sixth consecutive year of increase. Global annual ocean heat content saw a slight drop compared to the record high in 2015. Alpine glacier retreat continued around the globe, and preliminary data indicate that 2016 is the 37th consecutive year of negative annual mass balance. Across the Northern Hemisphere, snow cover for each month from February to June was among its four least extensive in the 47-year satellite record. Continuing a pattern below the surface, record high temperatures at 20-m depth were measured at all permafrost observatories on the North Slope of Alaska and at the Canadian observatory on northernmost Ellesmere Island. In the Antarctic, record low monthly surface pressures were broken at many stations, with the southern annular mode setting record high index values in March and June. Monthly high surface pressure records for August and November were set at several stations. During this period, record low daily and monthly sea ice extents were observed, with the November mean sea ice extent more than 5 standard deviations below the 1981-2010 average. These record low sea ice values contrast sharply with the record high values observed during 2012-14. Over the region, springtime Antarctic stratospheric ozone depletion was less severe relative to the 1991-2006 average, but ozone levels were still low compared to pre-1990 levels. Closer to the equator, 93 named tropical storms were observed during 2016, above the 1981-2010 average of 82, but fewer than the 101 storms recorded in 2015. Three basins-the North Atlantic, and eastern and western North Pacific-experienced above-normal activity in 2016. The Australian basin recorded its least active season since the beginning of the satellite era in 1970. Overall, four tropical cyclones reached the Saffir-Simpson category 5 intensity level. The strong El Nino at the beginning of the year that transitioned to a weak La Nina contributed to enhanced precipitation variability around the world. Wet conditions were observed throughout the year across southern South America, causing repeated heavy flooding in Argentina, Paraguay, and Uruguay. Wetter-than-usual conditions were also observed for eastern Europe and central Asia, alleviating the drought conditions of 2014 and 2015 in southern Russia. In the United States, California had its first wetter-than-average year since 2012, after being plagued by drought for several years. Even so, the area covered by drought in 2016 at the global scale was among the largest in the post-1950 record. For each month, at least 12% of land surfaces experienced severe drought conditions or worse, the longest such stretch in the record. In northeastern Brazil, drought conditions were observed for the fifth consecutive year, making this the longest drought on record in the region. Dry conditions were also observed in western Bolivia and Peru; it was Bolivia's worst drought in the past 25 years. In May, with abnormally warm and dry conditions already prevailing over western Canada for about a year, the human-induced Fort McMurray wildfire burned nearly 590000 hectares and became the costliest disaster in Canadian history, with $3 billion (U.S. dollars) in insured losses.

Published
2017
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3. State of the Climate in 2014

Author

Aaron-Morrison, Arlene P., Ackerman, Steven A., Adams, Nicolaus G., Adler, Robert F., Albanil, Adelina, Alfaro, E. J., Allan, Rob, Alves, Lincoln M., Amador, Jorge A., Andreassen, L. M., Arendt, A., Arévalo, Juan, Arndt, Derek S., Arzhanova, N. M., Aschan, M. M., Azorin-Molina, César, Banzon, Viva, Bardin, M. U., Barichivich, Jonathan, Baringer, Molly O., Barreira, Sandra, Baxter, Stephen, Bazo, Juan, Becker, Andreas, Bedka, Kristopher M., Behrenfeld, Michael J., Bell, Gerald D., Belmont, M., Benedetti, Angela, Bernhard, G., Berrisford, Paul, Berry, David I., Bettolli, María L., Bhatt, U. S., Bidegain, Mario, Bill, Brian D., Billheimer, Sam, Bissolli, Peter, Blake, Eric S., Blunden, Jessica, Bosilovich, Michael G., Boucher, Olivier, Boudet, Dagne, Box, J. E., Boyer, Tim, Braathen, Geir O., Bromwich, David H., Brown, R., Bulygina, Olga N., Burgess, D., Calderón, Blanca, Camargo, Suzana J., Campbell, Jayaka D., Cappelen, J., Carrasco, Gualberto, Carter, Brendan R., Chambers, Don P., Chandler, Elise, Christiansen, Hanne H., Christy, John R., Chung, Daniel, Chung, E. S., Cinque, Kathy, Clem, Kyle R., Coelho, Caio A., Cogley, J. G., Coldewey-Egbers, Melanie, Colwell, Steve, Cooper, Owen R., Copland, L., Cosca, Catherine E., Cross, Jessica N., Crotwell, Molly J., Crouch, Jake, Davis, Sean M., De Eyto, Elvira, De Jeu, Richard A.M., De Laat, Jos, Degasperi, Curtis L., Degenstein, Doug, Demircan, M., Derksen, C., Destin, Dale, Di Girolamo, Larry, Di Giuseppe, F., Diamond, Howard J., Dlugokencky, Ed J., Dohan, Kathleen, Dokulil, Martin T., Dolgov, A. V., Dolman, A. Johannes, Domingues, Catia M., Donat, Markus G., Dong, Shenfu, Dorigo, Wouter A., Dortch, Quay, Doucette, Greg, Drozdov, D. S., Ducklow, Hugh, Dunn, Robert J.H., Durán-Quesada, Ana M., Dutton, Geoff S., Ebrahim, A., Elkharrim, M., Elkins, James W., Espinoza, Jhan C., Etienne-Leblanc, Sheryl, Evans, Thomas E., Famiglietti, James S., Farrell, S., Fateh, S., Fausto, Robert S., Fedaeff, Nava, Feely, Richard A., Feng, Z., Fenimore, Chris, Fettweis, X., Fioletov, Vitali E., Flemming, Johannes, Fogarty, Chris T., Fogt, Ryan L., Folland, Chris, Fonseca, C., Fossheim, M., Foster, Michael J., Fountain, Andrew, Francis, S. D., Franz, Bryan A., Frey, Richard A., Frith, Stacey M., Froidevaux, Lucien, Ganter, Catherine, Garzoli, Silvia, Gerland, S., Gobron, Nadine, Goldenberg, Stanley B., Gomez, R. Sorbonne, Goni, Gustavo, Goto, A., Grooß, J. U., Gruber, Alexander, Guard, Charles Chip, Gugliemin, Mauro, Gupta, S. K., Gutiérrez, J. M., Hagos, S., Hahn, Sebastian, Haimberger, Leo, Hakkarainen, J., Hall, Brad D., Halpert, Michael S., Hamlington, Benjamin D., Hanna, E., Hansen, K., Hanssen-Bauer, I., Harris, Ian, Heidinger, Andrew K., Heikkilä, A., Heil, A., Heim, Richard R., Hendricks, S., Hernández, Marieta, Hidalgo, Hugo G., Hilburn, Kyle, Ho, Shu Peng Ben, Holmes, R. M., Hu, Zeng Zhen, Huang, Boyin, Huelsing, Hannah K., Huffman, George J., Hughes, C., Hurst, Dale F., Ialongo, I., Ijampy, J. A., Ingvaldsen, R. B., Inness, Antje, Isaksen, K., Ishii, Masayoshi, Jevrejeva, Svetlana, Jiménez, C., Jin, Xiangze, Johannesen, E., John, Viju, Johnsen, B., Johnson, Bryan, Johnson, Gregory C., Jones, Philip D., Joseph, Annie C., Jumaux, Guillaume, Kabidi, Khadija, Kaiser, Johannes W., Kato, Seiji, Kazemi, A., Keller, Linda M., Kendon, Mike, Kennedy, John, Kerr, Kenneth, Kholodov, A. L., Khoshkam, Mahbobeh, Killick, Rachel, Kim, Hyungjun, Kim, S. J., Kimberlain, Todd B., Klotzbach, Philip J., Knaff, John A., Kobayashi, Shinya, Kohler, J., Korhonen, Johanna, Korshunova, Natalia N., Kovacs, K. M., Kramarova, Natalya, Kratz, D. P., Kruger, Andries, Kruk, Michael C., Kudela, Raphael, Kumar, Arun, Lakatos, M., Lakkala, K., Lander, Mark A., Landsea, Chris W., Lankhorst, Matthias, Lantz, Kathleen, Lazzara, Matthew A., Lemons, P., Leuliette, Eric, L’Heureux, Michelle, Lieser, Jan L., Lin, I. I., Liu, Hongxing, Liu, Yinghui, Locarnini, Ricardo, Loeb, Norman G., Lo Monaco, Claire, Long, Craig S., López Álvarez, Luis Alfonso, Lorrey, Andrew M., Loyola, Diego, Lumpkin, Rick, Luo, Jing Jia, Luojus, K., Lydersen, C., Lyman, John M., Maberly, Stephen C., Maddux, Brent C., Malheiros Ramos, Andrea, Malkova, G. V., Manney, G., Marcellin, Vernie, Marchenko, S. S., Marengo, José A., Marra, John J., Marszelewski, Wlodzimierz, Martens, B., Martínez-Güingla, Rodney, Massom, Robert A., Mata, Mauricio M., Mathis, Jeremy T., May, Linda, Mayer, Michael, Mazloff, Matthew, McBride, Charlotte, McCabe, M. F., McCarthy, M., McClelland, J. W., McGree, Simon, McVicar, Tim R., Mears, Carl A., Meier, W., Meinen, Christopher S., Mekonnen, A., Menéndez, Melisa, Mengistu Tsidu, G., Menzel, W. Paul, Merchant, Christopher J., Meredith, Michael P., Merrifield, Mark A., Metzl, N., Minnis, Patrick, Miralles, Diego G., Mistelbauer, T., Mitchum, Gary T., Monselesan, Didier, Monteiro, Pedro, Montzka, Stephen A., Morice, Colin, Mote, T., Mudryk, L., Mühle, Jens, Mullan, A. Brett, Nash, Eric R., Naveira-Garabato, Alberto C., Nerem, R. Steven, Newman, Paul A., Nieto, Juan José, Noetzli, Jeannette, O’Neel, S., Osborn, Tim J., Overland, J., Oyunjargal, Lamjav, Parinussa, Robert M., Park, E. Hyung, Parker, David, Parrington, M., Parsons, A. Rost, Pasch, Richard J., Pascual-Ramírez, Reynaldo, Paterson, Andrew M., Paulik, Christoph, Pearce, Petra R., Pelto, Mauri S., Peng, Liang, Perkins-Kirkpatrick, Sarah E., Perovich, D., Petropavlovskikh, Irina, Pezza, Alexandre B., Phillips, David, Pinty, Bernard, Pitts, Michael C., Pons, M. R., Porter, Avalon O., Primicerio, R., Proshutinsky, A., Quegan, Sean, Quintana, Juan, Rahimzadeh, Fatemeh, Rajeevan, Madhavan, Randriamarolaza, L., Razuvaev, Vyacheslav N., Reagan, James, Reid, Phillip, Reimer, Christoph, Rémy, Samuel, Renwick, James A., Revadekar, Jayashree V., Richter-Menge, J., Riffler, Michael, Rimmer, Alon, Rintoul, Steve, Robinson, David A., Rodell, Matthew, Rodríguez Solís, José L., Romanovsky, Vladimir E., Ronchail, Josyane, Rosenlof, Karen H., Roth, Chris, Rusak, James A., Sabine, Christopher L., Sallée, Jean Bapiste, Sánchez-Lugo, Ahira, Santee, Michelle L., Sawaengphokhai, P., Sayouri, Amal, Scambos, Ted A., Schemm, Jae, Schladow, S. Geoffrey, Schmid, Claudia, Schmid, Martin, Schmidtko, Sunke, Schreck, Carl J., Selkirk, H. B., Send, Uwe, Sensoy, Serhat, Setzer, Alberto, Sharp, M., Shaw, Adrian, Shi, Lei, Shiklomanov, A. I., Shiklomanov, Nikolai I., Siegel, David A., Signorini, Sergio R., Sima, Fatou, Simmons, Adrian J., Smeets, C. J.P.P., Smith, Sharon L., Spence, Jaqueline M., Srivastava, A. K., Stackhouse, Paul W., Stammerjohn, Sharon, Steinbrecht, Wolfgang, Stella, José L., Stengel, Martin, Stennett-Brown, Roxann, Stephenson, Tannecia S., Strahan, Susan, Streletskiy, D. A., Sun-Mack, Sunny, Swart, Sebastiaan, Sweet, William, Talley, Lynne D., Tamar, Gerard, Tank, S. E., Taylor, Michael A., Tedesco, M., Teubner, Katrin, Thoman, R. L., Thompson, Philip, Thomson, L., Timmermans, M. L., Tirnanes, Joaquin A., Tobin, Skie, Trachte, Katja, Trainer, Vera L., Tretiakov, M., Trewin, Blair C., Trotman, Adrian R., Tschudi, M., Van As, D., Van De Wal, R. S.W., van der A., Ronald J., Van Der Schalie, Robin, Van Der Schrier, Gerard, Van Der Werf, Guido R., Van Meerbeeck, Cedric J., Velicogna, I., Verburg, Piet, Vigneswaran, Bala, Vincent, Lucie A., Volkov, Denis, Vose, Russell S., Wagner, Wolfgang, Wåhlin, Anna, Wahr, J., Walsh, J., Wang, Chunzai, Wang, Junhong, Wang, Lei, Wang, M., Wang, Sheng Hung, Wanninkhof, Rik, Watanabe, Shohei, Weber, Mark, Weller, Robert A., Weyhenmeyer, Gesa A., Whitewood, Robert, Wijffels, Susan E., Wilber, Anne C., Wild, Jeanette D., Willett, Kate M., Williams, Michael J.M., Willie, Shem, Wolken, G., Wong, Takmeng, Wood, E. F., Woolway, R. Iestyn, Wouters, B., Xue, Yan, Yamada, Ryuji, Yim, So Young, Yin, Xungang, Young, Steven H., Yu, Lisan, Zahid, H., Zambrano, Eduardo, Zhang, Peiqun, Zhao, Guanguo, Zhou, Lin, Ziemke, Jerry R., Love-Brotak, S. Elizabeth, Gilbert, Kristin, Maycock, Tom, Osborne, Susan, Sprain, Mara, Veasey, Sara W., Ambrose, Barbara J., Griffin, Jessicca, Misch, Deborah J., Riddle, Deborah B., Young, Teresa, Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] (LSCE), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), ICOS-ATC (ICOS-ATC), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Modélisation INVerse pour les mesures atmosphériques et SATellitaires (SATINV), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), and Earth and Climate

Subjects
0106 biological sciences, [SDU.OCEAN]Sciences of the Universe [physics]/Ocean, Atmosphere, Atmospheric Science, 010504 meteorology & atmospheric sciences, 010604 marine biology & hydrobiology, Perspective (graphical), 15. Life on land, 01 natural sciences, El Niño Southern Oscillation, 13. Climate action, Climatology, SDG 13 - Climate Action, Environmental science, SDG 14 - Life Below Water, [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces, environment, ComputingMilieux_MISCELLANEOUS, 0105 earth and related environmental sciences
Abstract

Most of the dozens of essential climate variables monitored each year in this report continued to follow their long-term trends in 2014, with several setting new records. Carbon dioxide, methane, and nitrous oxide-the major greenhouse gases released into Earth's atmosphere-once again all reached record high average atmospheric concentrations for the year. Carbon dioxide increased by 1.9 ppm to reach a globally averaged value of 397.2 ppm for 2014. Altogether, 5 major and 15 minor greenhouse gases contributed 2.94 W m-2 of direct radiative forcing, which is 36% greater than their contributions just a quarter century ago. Accompanying the record-high greenhouse gas concentrations was nominally the highest annual global surface temperature in at least 135 years of modern record keeping, according to four independent observational analyses. The warmth was distributed widely around the globe's land areas, Europe observed its warmest year on record by a large margin, with close to two dozen countries breaking their previous national temperature records; many countries in Asia had annual temperatures among their 10 warmest on record; Africa reported above-average temperatures across most of the continent throughout 2014; Australia saw its third warmest year on record, following record heat there in 2013; Mexico had its warmest year on record; and Argentina and Uruguay each had their second warmest year on record. Eastern North America was the only major region to observe a below-average annual temperature. But it was the oceans that drove the record global surface temperature in 2014. Although 2014 was largely ENSO-neutral, the globally averaged sea surface temperature (SST) was the highest on record. The warmth was particularly notable in the North Pacific Ocean where SST anomalies signaled a transition from a negative to positive phase of the Pacific decadal oscillation. In the winter of 2013/14, unusually warm water in the northeast Pacific was associated with elevated ocean heat content anomalies and elevated sea level in the region. Globally, upper ocean heat content was record high for the year, reflecting the continued increase of thermal energy in the oceans, which absorb over 90% of Earth's excess heat from greenhouse gas forcing. Owing to both ocean warming and land ice melt contributions, global mean sea level in 2014 was also record high and 67 mm greater than the 1993 annual mean, when satellite altimetry measurements began. Sea surface salinity trends over the past decade indicate that salty regions grew saltier while fresh regions became fresher, suggestive of an increased hydrological cycle over the ocean expected with global warming. As in previous years, these patterns are reflected in 2014 subsurface salinity anomalies as well. With a now decade-long trans-basin instrument array along 26°N, the Atlantic meridional overturning circulation shows a decrease in transport of-4.2 ± 2.5 Sv decade-1. Precipitation was quite variable across the globe. On balance, precipitation over the world's oceans was above average, while below average across land surfaces. Drought continued in southeastern Brazil and the western United States. Heavy rain during April-June led to devastating floods in Canada's Eastern Prairies. Above-normal summer monsoon rainfall was observed over the southern coast of West Africa, while drier conditions prevailed over the eastern Sahel. Generally, summer monsoon rainfall over eastern Africa was above normal, except in parts of western South Sudan and Ethiopia. The south Asian summer monsoon in India was below normal, with June record dry. Across the major tropical cyclone basins, 91 named storms were observed during 2014, above the 1981-2010 global average of 82. The Eastern/Central Pacific and South Indian Ocean basins experienced significantly above-normal activity in 2014; all other basins were either at or below normal. The 22 named storms in the Eastern/Central Pacific was the basin's most since 1992. Similar to 2013, the North Atlantic season was quieter than most years of the last two decades with respect to the number of storms, despite the absence of El Niño conditions during both years. In higher latitudes and at higher elevations, increased warming continued to be visible in the decline of glacier mass balance, increasing permafrost temperatures, and a deeper thawing layer in seasonally frozen soil. In the Arctic, the 2014 temperature over land areas was the fourth highest in the 115-year period of record and snow melt occurred 20-30 days earlier than the 1998-2010 average. The Greenland Ice Sheet experienced extensive melting in summer 2014. The extent of melting was above the 1981-2010 average for 90% of the melt season, contributing to the second lowest average summer albedo over Greenland since observations began in 2000 and a record-low albedo across the ice sheet for August. On the North Slope of Alaska, new record high temperatures at 20-m depth were measured at four of five permafrost observatories. In September, Arctic minimum sea ice extent was the sixth lowest since satellite records began in 1979. The eight lowest sea ice extents during this period have occurred in the last eight years. Conversely, in the Antarctic, sea ice extent countered its declining trend and set several new records in 2014, including record high monthly mean sea ice extent each month from April to November. On 20 September, a record large daily Antarctic sea ice extent of 20.14 × 106 km2 occurred. The 2014 Antarctic stratospheric ozone hole was 20.9 million km2 when averaged from 7 September to 13 October, the sixth smallest on record and continuing a decrease, albeit statistically insignificant, in area since 1998.

Published
2015
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4. Glacier dynamics at Helheim and Kangerdlugssuaq glaciers, southeast Greenland, since the Little Ice Age

Author

Khan, S. A., Kjeldsen, K. K., Kjaer, K. H., Bevan, S., Luckman, A., Aschwanden, A., Bjork, A. A., Korsgaard, N. J., Box, J. E., van den Broeke, M., van Dam, T. M., Fitzner, A., Sub Dynamics Meteorology, Marine and Atmospheric Research, Sub Dynamics Meteorology, and Marine and Atmospheric Research

Subjects
Glacier ice accumulation, Glacier terminus, Ice stream, SEA-LEVEL RISE, ACCELERATION, WEST GREENLAND, Glacier mass balance, lcsh:Environmental sciences, Earth-Surface Processes, Water Science and Technology, JAKOBSHAVN ISBRAE, lcsh:GE1-350, geography, geography.geographical_feature_category, lcsh:QE1-996.5, Tidewater glacier cycle, Glacier, MASS-LOSS, RETREAT, Glacier morphology, CLIMATE, lcsh:Geology, EAST GREENLAND, OUTLET GLACIERS, Climatology, SHEET, Ice sheet, Geology
Abstract

Observations over the past decade show significant ice loss associated with the speed-up of glaciers in southeast Greenland from 2003, followed by a deceleration from 2006. These short-term, episodic, dynamic perturbations have a major impact on the mass balance on the decadal scale. To improve the projection of future sea level rise, a long-term data record that reveals the mass balance beyond such episodic events is required. Here, we extend the observational record of marginal thinning of Helheim and Kangerdlugssuaq glaciers from 10 to more than 80 years. We show that, although the frontal portion of Helheim Glacier thinned by more than 100 m between 2003 and 2006, it thickened by more than 50 m during the previous two decades. In contrast, Kangerdlugssuaq Glacier underwent minor thinning of 40–50 m from 1981 to 1998 and major thinning of more than 100 m after 2003. Extending the record back to the end of the Little Ice Age (prior to 1930) shows no thinning of Helheim Glacier from its maximum extent during the Little Ice Age to 1981, while Kangerdlugssuaq Glacier underwent substantial thinning of 230 to 265 m. Comparison of sub-surface water temperature anomalies and variations in air temperature to records of thickness and velocity change suggest that both glaciers are highly sensitive to short-term atmospheric and ocean forcing, and respond very quickly to small fluctuations. On century timescales, however, multiple external parameters (e.g. outlet glacier shape) may dominate the mass change. These findings suggest that special care must be taken in the projection of future dynamic ice loss.

Published
2014
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5. Drivers of Firn Density on the Greenland Ice Sheet Revealed by Weather Station Observations and Modeling.

Author

Vandecrux, B., Fausto, R. S., Langen, P. L., As, D., MacFerrin, M., Colgan, W. T., Ingeman‐Nielsen, T., Steffen, K., Jensen, N. S., Møller, M. T., and Box, J. E.

Subjects
ATMOSPHERIC temperature, X-ray diffraction, CLIMATE change, GLACIATION, CLIMATOLOGY
Abstract

Recent Arctic atmospheric warming induces more frequent surface melt in the accumulation area of the Greenland ice sheet. This increased melting modifies the near‐surface firn structure and density and may reduce the firn's capacity to retain meltwater. Yet few long‐term observational records are available to determine the evolution and drivers of firn density. In this study, we compile and gap‐fill Greenland Climate Network (GC‐Net) automatic weather station data from Crawford Point, Dye‐2, NASA‐SE, and Summit between 1998 and 2015. These records then force a coupled surface energy balance and firn evolution model. We find at all sites except Summit that increasing summer turbulent heat fluxes to the surface are compensated by decreasing net radiative fluxes. After evaluating the model against firn cores, we find that, starting from 2006, the density of the top 20 m of firn at Dye‐2 increased by 11%, decreasing the pore volume by 18%. Crawford Point and Summit show stable near‐surface firn density over 1998–2010 and 2000–2015 respectively, while we calculate a 4% decrease of firn density at NASA‐SE over 1998–2015. For each year, the model identifies the drivers of density change in the top 20‐m firn and quantifies their contributions. The key driver, snowfall, explains alone 72 to 92% of the variance in day‐to‐day change in firn density while melt explains from 7 to 33%. Our result indicates that correct estimates of the magnitude and variability of precipitation are necessary to interpret or simulate the evolution of the firn. Plain Language Summary: Arctic warming has led to more intense melt on the Greenland ice sheet. In recent decades this melt moved upglacier and started to alter the structure of perennial snow, or firn, in areas where melt was rarely recorded. In this study, we process 12–17 years of observations from four weather stations located in the vast high‐elevation area of the ice sheet. From these climate records, we calculate how much melt occurred each summer and why (e.g., warm air or sunlight absorption). We found that heat transfer from the air to the surface has become more intense but is compensated by a brightening of the surface, causing less sunlight to be absorbed and used for melting. We use a computer model that simulates firn evolution and shows a good match with independent observations of the firn density. Our simulations identify increasing firn density at a first site, stable density at two sites, and decreasing firn density at the last one. Day‐to‐day and year‐to‐year changes in the density of the top 20 m of firn were mostly due to the snowfall variability followed by surface melt. This work underlines the importance of accurate precipitation estimates in order to understand firn evolution. Key Points: We gathered, processed, and gap‐filled underexploited climate observations at four sites from the Greenland ice sheet accumulation areaIncreasing turbulent heat fluxes were found at three sites over the 1998–2015 period, compensated by decreasing net radiative fluxesOur simulation of near‐surface firn density quantifies the role of its climatic drivers among which snowfall and surface melt are dominant [ABSTRACT FROM AUTHOR]

Published
2018
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6. Recent changes in north-west Greenland climate documented by NEEM shallow ice core data and simulations, and implications for past-temperature reconstructions.

Author

Masson-Delmotte, V., Steen-Larsen, H. C., Ortega, P., Swingedouw, D., Popp, T., Vinther, B. M., Oerter, H., Sveinbjornsdottir, A. E., Gudlaugsdottir, H., Box, J. E., Falourd, S., Fettweis, X., Gallée, H., Garnier, E., Gkinis, V., Jouzel, J., Landais, A., Minster, B., Paradis, N., and Orsi, A.

Subjects
CLIMATOLOGY, METEOROLOGY, ICE, SNOW, WEATHER
Abstract

Combined records of snow accumulation rate, δ18O and deuterium excess were produced from several shallow ice cores and snow pits at NEEM (North Greenland Eemian Ice Drilling), covering the period from 1724 to 2007. They are used to investigate recent climate variability and characterise the isotope-temperature relationship. We find that NEEM records are only weakly affected by inter-annual changes in the North Atlantic Oscillation. Decadal δ18O and accumulation variability is related to North Atlantic sea surface temperature and is enhanced at the beginning of the 19th century. No long-term trend is observed in the accumulation record. By contrast, NEEM δ18O shows multidecadal increasing trends in the late 19th century and since the 1980s. The strongest annual positive δ18O values are recorded at NEEM in 1928 and 2010, while maximum accumulation occurs in 1933. The last decade is the most enriched in δ18O (warmest), while the 11-year periods with the strongest depletion (coldest) are depicted at NEEM in 1815-1825 and 1836-1846, which are also the driest 11-year periods. The NEEM accumulation and δ18O records are strongly correlated with outputs from atmospheric models, nudged to atmospheric reanalyses. Best performance is observed for ERA reanalyses. Gridded temperature reconstructions, instrumental data and model outputs at NEEM are used to estimate the multidecadal accumulation-temperature and δ18O-temperature relationships for the strong warming period in 1979-2007. The accumulation sensitivity to temperature is estimated at 11±2% °C-1 and the δ18O-temperature slope at 1.1±0.2‰ °C-1, about twice as large as previously used to estimate last interglacial temperature change from the bottom part of the NEEM deep ice core. [ABSTRACT FROM AUTHOR]

Published
2015
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7. State of the climate in 2017

Author

Abernethy, R., Ackerman, S. A., Adler, R., Albanil Encarnación, A., Aldeco, L. S., Alfaro, E. J., Aliaga-Nestares, V., Allan, R. P., Allan, R., Alves, L. M., Amador, J. A., Anderson, J., Andreassen, L. M., Argüez, A., Armitage, C., Arndt, D. S., Avalos, G., Azorin-Molina, C., Báez, J., Bardin, M. Yu, Barichivich, J., Baringer, M. O., Barreira, S., Baxter, S., Beck, H. E., Becker, A., Bedka, K. M., Behe, C., Bell, G. D., Bellouin, N., Belmont, M., Benedetti, A., Bernhard, G. H., Berrisford, P., Berry, D. I., Bhatt, U. S., Bissolli, P., Bjerke, J., Blake, E. S., Blenkinsop, S., Blunden, J., Bolmgren, K., Bosilovich, M. G., Boucher, O., Bouchon, M., Box, J. E., Boyer, T., Braathen, G. O., Bromwich, D. H., Brown, R., Buehler, S., Bulygina, O. N., Burgess, D., Calderón, B., Camargo, S. J., Campbell, E. C., Campbell, J. D., Cappelen, J., Carrea, L., Carter, B. R., Castro, A., Chambers, D. P., lijing cheng, Christiansen, H. H., Christy, J. R., Chung, E. -S, Clem, K. R., Coelho, C. A. S., Coldewey-Egbers, M., Colwell, S., Cooper, O. R., Copland, L., Costanza, C., Covey, C., Coy, L., Cronin, T., Crouch, J., Cruzado, L., Daniel, R., Davis, S. M., Davletshin, S. G., Eyto, E., Jeu, R. A. M., La Cour, J. L., Laat, J., Gasperi, C. L., Degenstein, D., Deline, P., Demircan, M., Derksen, C., Dewitte, B., Dhurmea, R., Di Girolamo, L., Diamond, H. J., Dickerson, C., Dlugokencky, E. J., Dohan, K., Dokulil, M. T., Dolman, A. J., Domingues, C. M., Domingues, R., Donat, M. G., Dong, S., Dorigo, W. A., Drozdov, D. S., Dunn, R. J. H., Durre, I., Dutton, G. S., Eakin, C. M., El Kharrim, M., Elkins, J. W., Epstein, H. E., Espinoza, J. C., Famiglietti, J. S., Farmer, J., Farrell, S., Fauchald, P., Fausto, R. S., Feely, R. A., Feng, Z., Fenimore, C., Fettweis, X., Fioletov, V. E., Flemming, J., Fogt, R. L., Folland, C., Forbes, B. C., Foster, M. J., Francis, S. D., Franz, B. A., Frey, R. A., Frith, S. M., Froidevaux, L., Ganter, C., Geiger, E. F., Gerland, S., Gilson, J., Gobron, N., Goldenberg, S. B., Gomez, A. M., Goni, G., Grooß, J. U., Gruber, A., Guard, C. P., Gugliemin, M., Gupta, S. K., Gutiérrez, D., Haas, C., Hagos, S., Hahn, S., Haimberger, L., Hall, B. D., Halpert, M. S., Hamlington, B. D., Hanna, E., Hansen, K., Hanssen-Bauer, L., Harris, I., Hartfield, G., Heidinger, A. K., Heim, R. R., Helfrich, S., Hemming, D. L., Hendricks, S., Hernández, R., Hernández, S. M., Heron, S. F., Heuzé, C., Hidalgo, H. G., Ho, S. -P, Hobbs, W. R., Horstkotte, T., Huang, B., Hubert, D., Hueuzé, C., Hurst, D. F., Ialongo, I., Ibrahim, M. M., Ijampy, J. A., Inness, A., Isaac, V., Isaksen, K., Ishii, M., Jacobs, S. J., Jeffries, M. O., Jevrejeva, S., Jiménez, C., Jin, X., John, V., Johns, W. E., Johnsen, B., Johnson, B., Johnson, G. C., Johnson, K. S., Jones, P. D., Jumaux, G., Kabidi, K., Kaiser, J. W., Karaköylü, E. M., Kato, S., Kazemi, A., Keller, L. M., Kennedy, J., Kerr, K., Khan, M. S., Kholodov, A. L., Khoshkam, M., Killick, R., Kim, H., Kim, S. -J, Klotzbach, P. J., Knaff, J. A., Kohler, J., Korhonen, J., Korshunova, N. N., Kramarova, N., Kratz, D. P., Kruger, A., Kruk, M. C., Krumpen, T., Ladd, C., Lakatos, M., Lakkala, K., Lander, M. A., Landschützer, P., Landsea, C. W., Lankhorst, M., Lavado-Casimiro, W., Lazzara, M. A., Lee, S. -E, Lee, T. C., Leuliette, E., L Heureux, M., Li, T., Lieser, J. L., Lin, I. -I, Mears, C. A., Liu, G., Li, B., Liu, H., Locarnini, R., Loeb, N. G., Long, C. S., López, L. A., Lorrey, A. M., Loyola, D., Lumpkin, R., Luo, J. -J, Luojus, K., Luthcke, S., Macias-Fauria, M., Malkova, G. V., Manney, G. L., Marcellin, V., Marchenko, S. S., Marengo, J. A., Marín, D., Marra, J. J., Marszelewski, W., Martens, B., Martin, A., Martínez, A. G., Martínez-Güingla, R., Martínez-Sánchez, O., Marsh, B. L., Lyman, J. M., Massom, R. A., May, L., Mayer, M., Mazloff, M., Mcbride, C., Mccabe, M. F., Mccarthy, M., Meier, W., Meijers, A. J. S., Mekonnen, A., Mengistu Tsidu, G., Menzel, W. P., Merchant, C. J., Meredith, M. P., Merrifield, M. A., Miller, B., Miralles, D. G., Mitchum, G. T., Mitro, S., Moat, B., Mochizuki, Y., Monselesan, D., Montzka, S. A., Mora, N., Morice, C., Mosquera-Vásquez, K., Mostafa, A. E., Mote, T., Mudryk, L., Mühle, J., Mullan, A. B., Müller, R., Myneni, R., Nash, E. R., Nerem, R. S., Newman, L., Newman, P. A., Nielsen-Gammon, J. W., Nieto, J. J., Noetzli, J., Noll, B. E., O Neel, S., Osborn, T. J., Osborne, E., Overland, J., Oyunjargal, L., Park, T., Pasch, R. J., Pascual-Ramírez, R., Pastor Saavedra, M. A., Paterson, A. M., Paulik, C., Pearce, P. R., Peltier, A., Pelto, M. S., Peng, L., Perkins-Kirkpatrick, S. E., Perovich, D., Petropavlovskikh, I., Pezza, A. B., Phillips, C., Phillips, D., Phoenix, G., Pinty, B., Pinzon, J., Po-Chedley, S., Polashenski, C., Purkey, S. G., Quispe, N., Rajeevan, M., Rakotoarimalala, C., Rayner, D., Raynolds, M. K., Reagan, J., Reid, P., Reimer, C., Rémy, S., Revadekar, J. V., Richardson, A. D., Richter-Menge, J., Ricker, R., Rimmer, A., Robinson, D. A., Rodell, M., Rodriguez Camino, E., Romanovsky, V. E., Ronchail, J., Rosenlof, K. H., Rösner, B., Roth, C., Roth, D. M., Rusak, J. A., Rutishäuser, T., Sallée, J. -B, Sánchez-Lugo, A., Santee, M. L., Sasgen, L., Sawaengphokhai, P., Sayad, T. A., Sayouri, A., Scambos, T. A., Scanlon, T., Schenzinger, V., Schladow, S. G., Schmid, C., Schmid, M., Schreck, C. J., Selkirk, H. B., Send, U., Sensoy, S., Sharp, M., Shi, L., Shiklomanov, N. I., Shimaraeva, S. V., Siegel, D. A., Silow, E., Sima, F., Simmons, A. J., Skirving, W. J., Smeed, D. A., Smeets, C. J. P. P., Smith, A., Smith, S. L., Soden, B., Sofieva, V., Sparks, T. H., Spence, J. M., Spillane, S., Srivastava, A. K., Stackhouse, P. W., Stammerjohn, S., Stanitski, D. M., Steinbrecht, W., Stella, J. L., Stengel, M., Stephenson, K., Stephenson, T. S., Strahan, S., Streletskiy, D. A., Strong, A. E., Sun-Mack, S., Sutton, A. J., Swart, S., Sweet, W., Takahashi, K. S., Tamar, G., Taylor, M. A., Tedesco, M., Thackeray, S. J., Thoman, R. L., Thompson, P., Thomson, L., Thorsteinsson, T., Timbal, B., Timmermans, M. -L, Timofeyev, M. A., Tirak, K. V., Tobin, S., Togawa, H., Tømmervik, H., Tourpali, K., Trachte, K., Trewin, B. C., Triñanes, J. A., Trotman, A. R., Tschudi, M., Tucker, C. J., Tye, M. R., As, D., Wal, R. S. W., Ronald, J. A., Schalie, R., Schrier, G., Werf, G. R., Meerbeeck, C. J., Velden, C. S., Velicogna, I., Verburg, P., Vickers, H., Vincent, L. A., Vömel, H., Vose, R. S., Wagner, W., Walker, D. A., Walsh, J., Wang, B., Wang, J., Wang, L., Wang, M., Wang, R., Wang, S. -H, Wanninkhof, R., Watanabe, S., Weber, M., Webster, M., Weller, R. A., Westberry, T. K., Weyhenmeyer, G. A., Whitewood, R., Widlansky, M. J., Wiese, D. N., Wijffels, S. E., Wilber, A. C., Wild, J. D., Willett, K. M., Willis, J. K., Wolken, G., Wong, T., Wood, E. F., Wood, K., Woolway, R. I., Wouters, B., Xue, Y., Yin, X., Yoon, H., York, A., Yu, L., Zambrano, E., Zhang, H. -M, Zhang, P., Zhao, G., Zhao, L., Zhu, Z., Ziel, R., Ziemke, J. R., Ziese, M. G., Griffin, J., Hammer, G., Love-Brotak, S. E., Misch, D. J., Riddle, D. B., Slagle, M., Sprain, M., Veasey, S. W., and Mcvicar, T. R.

Subjects
Meteor (satellite), Atmospheric Science, Climate Research, 010504 meteorology & atmospheric sciences, Climate change, 010501 environmental sciences, 01 natural sciences, SDG 11 - Sustainable Cities and Communities, Klimatforskning, El Niño Southern Oscillation, 13. Climate action, Climatology, ComputingMethodologies_DOCUMENTANDTEXTPROCESSING, Environmental science, SDG 14 - Life Below Water, GeneralLiterature_REFERENCE(e.g.,dictionaries,encyclopedias,glossaries), 0105 earth and related environmental sciences
Abstract

In 2017, the dominant greenhouse gases released into Earth's atmosphere-carbon dioxide, methane, and nitrous oxide-reached new record highs. The annual global average carbon dioxide concentration at Earth's surface for 2017 was 405.0 ± 0.1 ppm, 2.2 ppm greater than for 2016 and the highest in the modern atmospheric measurement record and in ice core records dating back as far as 800 000 years. The global growth rate of CO2 has nearly quadrupled since the early 1960s. With ENSO-neutral conditions present in the central and eastern equatorial Pacific Ocean during most of the year and weak La Niña conditions notable at the start and end, the global temperature across land and ocean surfaces ranked as the second or third highest, depending on the dataset, since records began in the mid-to-late 1800s. Notably, it was the warmest non-El Niño year in the instrumental record. Above Earth's surface, the annual lower tropospheric temperature was also either second or third highest according to all datasets analyzed. The lower stratospheric temperature was about 0.2°C higher than the record cold temperature of 2016 according to most of the in situ and satellite datasets. Several countries, including Argentina, Uruguay, Spain, and Bulgaria, reported record high annual temperatures. Mexico broke its annual record for the fourth consecutive year. On 27 January, the temperature reached 43.4°C at Puerto Madryn, Argentina-the highest temperature recorded so far south (43°S) anywhere in the world. On 28 May in Turbat, western Pakistan, the high of 53.5°C tied Pakistan's all-time highest temperature and became the world-record highest temperature for May. In the Arctic, the 2017 land surface temperature was 1.6°C above the 1981-2010 average, the second highest since the record began in 1900, behind only 2016. The five highest annual Arctic temperatures have all occurred since 2007. Exceptionally high temperatures were observed in the permafrost across the Arctic, with record values reported in much of Alaska and northwestern Canada. In August, high sea surface temperature (SST) records were broken for the Chukchi Sea, with some regions as warm as +11°C, or 3° to 4°C warmer than the longterm mean (1982-present). According to paleoclimate studies, today's abnormally warm Arctic air and SSTs have not been observed in the last 2000 years. The increasing temperatures have led to decreasing Arctic sea ice extent and thickness. On 7 March, sea ice extent at the end of the growth season saw its lowest maximum in the 37-year satellite record, covering 8% less area than the 1981-2010 average. The Arctic sea ice minimum on 13 September was the eighth lowest on record and covered 25% less area than the long-term mean. Preliminary data indicate that glaciers across the world lost mass for the 38th consecutive year on record; the declines are remarkably consistent from region to region. Cumulatively since 1980, this loss is equivalent to slicing 22 meters off the top of the average glacier. Antarctic sea ice extent remained below average for all of 2017, with record lows during the first four months. Over the continent, the austral summer seasonal melt extent and melt index were the second highest since 2005, mostly due to strong positive anomalies of air temperature over most of the West Antarctic coast. In contrast, the East Antarctic Plateau saw record low mean temperatures in March. The year was also distinguished by the second smallest Antarctic ozone hole observed since 1988. Across the global oceans, the overall long-term SST warming trend remained strong. Although SST cooled slightly from 2016 to 2017, the last three years produced the three highest annual values observed; these high anomalies have been associated with widespread coral bleaching. The most recent global coral bleaching lasted three full years, June 2014 to May 2017, and was the longest, most widespread, and almost certainly most destructive such event on record. Global integrals of 0-700-m and 0-2000-m ocean heat content reached record highs in 2017, and global mean sea level during the year became the highest annual average in the 25-year satellite altimetry record, rising to 77 mm above the 1993 average. In the tropics, 2017 saw 85 named tropical storms, slightly above the 1981-2010 average of 82. The North Atlantic basin was the only basin that featured an above-normal season, its seventh most active in the 164-year record. Three hurricanes in the basin were especially notable. Harvey produced record rainfall totals in areas of Texas and Louisiana, including a storm total of 1538.7 mm near Beaumont, Texas, which far exceeds the previous known U.S. tropical cyclone record of 1320.8 mm. Irma was the strongest tropical cyclone globally in 2017 and the strongest Atlantic hurricane outside of the Gulf of Mexico and Caribbean on record with maximum winds of 295 km h-1. Maria caused catastrophic destruction across the Caribbean Islands, including devastating wind damage and flooding across Puerto Rico. Elsewhere, the western North Pacific, South Indian, and Australian basins were all particularly quiet. Precipitation over global land areas in 2017 was clearly above the long-term average. Among noteworthy regional precipitation records in 2017, Russia reported its second wettest year on record (after 2013) and Norway experienced its sixth wettest year since records began in 1900. Across India, heavy rain and flood-related incidents during the monsoon season claimed around 800 lives. In August and September, above-normal precipitation triggered the most devastating floods in more than a decade in the Venezuelan states of Bolívar and Delta Amacuro. In Nigeria, heavy rain during August and September caused the Niger and Benue Rivers to overflow, bringing floods that displaced more than 100 000 people. Global fire activity was the lowest since at least 2003; however, high activity occurred in parts of North America, South America, and Europe, with an unusually long season in Spain and Portugal, which had their second and third driest years on record, respectively. Devastating fires impacted British Columbia, destroying 1.2 million hectares of timber, bush, and grassland, due in part to the region's driest summer on record. In the United States, an extreme western wildfire season burned over 4 million hectares; the total costs of $18 billion tripled the previous U.S. annual wildfire cost record set in 1991.

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