376 results on '"Etiope, Giuseppe"'
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2. A direct observation of a hydrogen-rich pressurized reservoir within an ophiolite (Tișovița, Romania)
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Baciu, Calin, primary and Etiope, Giuseppe, additional
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- 2024
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3. Massive release of natural hydrogen from a geological seep (Chimaera, Turkey): Gas advection as a proxy of subsurface gas migration and pressurised accumulations
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Etiope, Giuseppe
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- 2023
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4. Supplementary material to "Global Methane Budget 2000–2020"
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Saunois, Marielle, primary, Martinez, Adrien, additional, Poulter, Benjamin, additional, Zhang, Zhen, additional, Raymond, Peter, additional, Regnier, Pierre, additional, Canadell, Joseph G., additional, Jackson, Robert B., additional, Patra, Prabir K., additional, Bousquet, Philippe, additional, Ciais, Philippe, additional, Dlugokencky, Edward J., additional, Lan, Xin, additional, Allen, George H., additional, Bastviken, David, additional, Beerling, David J., additional, Belikov, Dmitry A., additional, Blake, Donald R., additional, Castaldi, Simona, additional, Crippa, Monica, additional, Deemer, Bridget R., additional, Dennison, Fraser, additional, Etiope, Giuseppe, additional, Gedney, Nicola, additional, Höglund-Isaksson, Lena, additional, Holgerson, Meredith A., additional, Hopcroft, Peter O., additional, Hugelius, Gustaf, additional, Ito, Akihito, additional, Jain, Atul K., additional, Janardanan, Rajesh, additional, Johnson, Matthew S., additional, Kleinen, Thomas, additional, Krummel, Paul, additional, Lauerwald, Ronny, additional, Li, Tingting, additional, Liu, Xiangyu, additional, McDonald, Kyle C., additional, Melton, Joe R., additional, Mühle, Jens, additional, Müller, Jurek, additional, Murguia-Flores, Fabiola, additional, Niwa, Yosuke, additional, Noce, Sergio, additional, Pan, Shufen, additional, Parker, Robert J., additional, Peng, Changhui, additional, Ramonet, Michel, additional, Riley, William J., additional, Rocher-Ros, Gerard, additional, Rosentreter, Judith A., additional, Sasakawa, Motoki, additional, Segers, Arjo, additional, Smith, Steven J., additional, Stanley, Emily H., additional, Thanwerdas, Joel, additional, Tian, Hanquin, additional, Tsuruta, Aki, additional, Tubiello, Francesco N., additional, Weber, Thomas S., additional, van der Werf, Guido, additional, Worthy, Doug E., additional, Xi, Yi, additional, Yoshida, Yukio, additional, Zhang, Wenxin, additional, Zheng, Bo, additional, Zhu, Qing, additional, Zhu, Qiuan, additional, and Zhuang, Qianlai, additional
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- 2024
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5. Global Methane Budget 2000–2020
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Saunois, Marielle, primary, Martinez, Adrien, additional, Poulter, Benjamin, additional, Zhang, Zhen, additional, Raymond, Peter, additional, Regnier, Pierre, additional, Canadell, Joseph G., additional, Jackson, Robert B., additional, Patra, Prabir K., additional, Bousquet, Philippe, additional, Ciais, Philippe, additional, Dlugokencky, Edward J., additional, Lan, Xin, additional, Allen, George H., additional, Bastviken, David, additional, Beerling, David J., additional, Belikov, Dmitry A., additional, Blake, Donald R., additional, Castaldi, Simona, additional, Crippa, Monica, additional, Deemer, Bridget R., additional, Dennison, Fraser, additional, Etiope, Giuseppe, additional, Gedney, Nicola, additional, Höglund-Isaksson, Lena, additional, Holgerson, Meredith A., additional, Hopcroft, Peter O., additional, Hugelius, Gustaf, additional, Ito, Akihito, additional, Jain, Atul K., additional, Janardanan, Rajesh, additional, Johnson, Matthew S., additional, Kleinen, Thomas, additional, Krummel, Paul, additional, Lauerwald, Ronny, additional, Li, Tingting, additional, Liu, Xiangyu, additional, McDonald, Kyle C., additional, Melton, Joe R., additional, Mühle, Jens, additional, Müller, Jurek, additional, Murguia-Flores, Fabiola, additional, Niwa, Yosuke, additional, Noce, Sergio, additional, Pan, Shufen, additional, Parker, Robert J., additional, Peng, Changhui, additional, Ramonet, Michel, additional, Riley, William J., additional, Rocher-Ros, Gerard, additional, Rosentreter, Judith A., additional, Sasakawa, Motoki, additional, Segers, Arjo, additional, Smith, Steven J., additional, Stanley, Emily H., additional, Thanwerdas, Joel, additional, Tian, Hanquin, additional, Tsuruta, Aki, additional, Tubiello, Francesco N., additional, Weber, Thomas S., additional, van der Werf, Guido, additional, Worthy, Doug E., additional, Xi, Yi, additional, Yoshida, Yukio, additional, Zhang, Wenxin, additional, Zheng, Bo, additional, Zhu, Qing, additional, Zhu, Qiuan, additional, and Zhuang, Qianlai, additional
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- 2024
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6. Comment on egusphere-2024-611
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Etiope, Giuseppe, primary
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- 2024
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7. Methane on Mars and Habitability: Challenges and Responses
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Yung, Yuk L, Chen, Pin, Nealson, Kenneth, Atreya, Sushil, Beckett, Patrick, Blank, Jennifer G, Ehlmann, Bethany, Eiler, John, Etiope, Giuseppe, Ferry, James G, Forget, Francois, Gao, Peter, Hu, Renyu, Kleinböhl, Armin, Klusman, Ronald, Lefèvre, Franck, Miller, Charles, Mischna, Michael, Mumma, Michael, Newman, Sally, Oehler, Dorothy, Okumura, Mitchio, Oremland, Ronald, Orphan, Victoria, Popa, Radu, Russell, Michael, Shen, Linhan, Lollar, Barbara Sherwood, Staehle, Robert, Stamenković, Vlada, Stolper, Daniel, Templeton, Alexis, Vandaele, Ann C, Viscardy, Sébastien, Webster, Christopher R, Wennberg, Paul O, Wong, Michael L, and Worden, John
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Exobiology ,Extraterrestrial Environment ,Mars ,Methane ,Spectrum Analysis ,Time Factors ,CH4 ,Subsurface redox conditions ,Mars instrumentation ,Astrobiology 18 ,xxx-xxx ,Astronomical and Space Sciences ,Geochemistry ,Geology ,Astronomy & Astrophysics - Abstract
Recent measurements of methane (CH4) by the Mars Science Laboratory (MSL) now confront us with robust data that demand interpretation. Thus far, the MSL data have revealed a baseline level of CH4 (∼0.4 parts per billion by volume [ppbv]), with seasonal variations, as well as greatly enhanced spikes of CH4 with peak abundances of ∼7 ppbv. What do these CH4 revelations with drastically different abundances and temporal signatures represent in terms of interior geochemical processes, or is martian CH4 a biosignature? Discerning how CH4 generation occurs on Mars may shed light on the potential habitability of Mars. There is no evidence of life on the surface of Mars today, but microbes might reside beneath the surface. In this case, the carbon flux represented by CH4 would serve as a link between a putative subterranean biosphere on Mars and what we can measure above the surface. Alternatively, CH4 records modern geochemical activity. Here we ask the fundamental question: how active is Mars, geochemically and/or biologically? In this article, we examine geological, geochemical, and biogeochemical processes related to our overarching question. The martian atmosphere and surface are an overwhelmingly oxidizing environment, and life requires pairing of electron donors and electron acceptors, that is, redox gradients, as an essential source of energy. Therefore, a fundamental and critical question regarding the possibility of life on Mars is, "Where can we find redox gradients as energy sources for life on Mars?" Hence, regardless of the pathway that generates CH4 on Mars, the presence of CH4, a reduced species in an oxidant-rich environment, suggests the possibility of redox gradients supporting life and habitability on Mars. Recent missions such as ExoMars Trace Gas Orbiter may provide mapping of the global distribution of CH4. To discriminate between abiotic and biotic sources of CH4 on Mars, future studies should use a series of diagnostic geochemical analyses, preferably performed below the ground or at the ground/atmosphere interface, including measurements of CH4 isotopes, methane/ethane ratios, H2 gas concentration, and species such as acetic acid. Advances in the fields of Mars exploration and instrumentation will be driven, augmented, and supported by an improved understanding of atmospheric chemistry and dynamics, deep subsurface biogeochemistry, astrobiology, planetary geology, and geophysics. Future Mars exploration programs will have to expand the integration of complementary areas of expertise to generate synergistic and innovative ideas to realize breakthroughs in advancing our understanding of the potential of life and habitable conditions having existed on Mars. In this spirit, we conducted a set of interdisciplinary workshops. From this series has emerged a vision of technological, theoretical, and methodological innovations to explore the martian subsurface and to enhance spatial tracking of key volatiles, such as CH4.
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- 2018
8. Natural hydrogen extracted from ophiolitic rocks: A first dataset.
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Etiope, Giuseppe
- Abstract
Serpentinization is an important geochemical process producing natural hydrogen (H 2), and mafic and ultramafic serpentinized rocks, typically occurring in ophiolites and peridotite massifs, are major targets for H 2 exploration. Understanding the volumes of H 2 stored in these rocks is a key step towards establishing the potential of sepentinized systems to host H 2 sources and reservoirs. Nonetheless, published data on the concentration of H 2 directly extracted from serpentinized rocks are extremely scarce. This work provides a first dataset of H 2 extracted by planetary ball mill from 58 rock samples from different ophiolites in Greece, peridotites of the Tekirova ophiolite in Turkey, and chromitites and surrounding talc schist from an Archean-Paleoproterozoic greenstone belt in Brazil. The highest H 2 concentrations, from 0.1 mL/kg (considered as a threshold above which artificial H 2 by milling is negligible) to 16.2 mL/kg, were found in serpentinized harzburgites or dunites, and in chromitites hosted within serpentinized peridotites. The H 2 content of other mafic rocks that are not in contact or influenced by a serpentinized system, mostly basalts, is below 0.1 mL/kg. Serpentinized peridotites represent the logical source rocks of H 2 (i.e., hydrogen in peridotites is generally autochtonous) and chromitites, lacking significant olivine and serpentinized minerals, may host H 2 derived by the surrounding serpentinized rocks (hydrogen in chromitites is mostly allochtonous). The H 2 dataset of this work can be used as a reference for further studies on the capacity of ophiolitic rocks to produce and host natural hydrogen. • First dataset on H 2 concentration in mL/kg in different ophiolitic rocks. • Serpentinized harzburgites/dunites and chromitites host the highest H 2 concentrations. • Hypothesis of autochtonous hydrogen in peridotites, allochtonous hydrogen in chromitites. [ABSTRACT FROM AUTHOR]
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- 2024
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9. Evidence for massive emission of methane from a deep-water gas field during the Pliocene
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Foschi, Martino, Cartwright, Joseph A., MacMinn, Christopher W., and Etiope, Giuseppe
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- 2020
10. Methane clumped isotopes: Progress and potential for a new isotopic tracer
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Douglas, Peter MJ, Stolper, Daniel A, Eiler, John M, Sessions, Alex L, Lawson, Michael, Shuai, Yanhua, Bishop, Andrew, Podlaha, Olaf G, Ferreira, Alexandre A, Neto, Eugenio V Santos, Niemann, Martin, Steen, Arne S, Huang, Ling, Chimiak, Laura, Valentine, David L, Fiebig, Jens, Luhmann, Andrew J, Seyfried, William E, Etiope, Giuseppe, Schoell, Martin, Inskeep, William P, Moran, James J, and Kitchen, Nami
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Methane ,Clumped isotopes ,Geothermometry ,Petroleum systems ,Biogeochemistry ,Chemical Sciences ,Earth Sciences ,Environmental Sciences ,Geochemistry & Geophysics - Abstract
The isotopic composition of methane is of longstanding geochemical interest, with important implications for understanding petroleum systems, atmospheric greenhouse gas concentrations, the global carbon cycle, and life in extreme environments. Recent analytical developments focusing on multiply substituted isotopologues (‘clumped isotopes’) are opening a valuable new window into methane geochemistry. When methane forms in internal isotopic equilibrium, clumped isotopes can provide a direct record of formation temperature, making this property particularly valuable for identifying different methane origins. However, it has also become clear that in certain settings methane clumped isotope measurements record kinetic rather than equilibrium isotope effects. Here we present a substantially expanded dataset of methane clumped isotope analyses, and provide a synthesis of the current interpretive framework for this parameter. In general, clumped isotope measurements indicate plausible formation temperatures for abiotic, thermogenic, and microbial methane in many geological environments, which is encouraging for the further development of this measurement as a geothermometer, and as a tracer for the source of natural gas reservoirs and emissions. We also highlight, however, instances where clumped isotope derived temperatures are higher than expected, and discuss possible factors that could distort equilibrium formation temperature signals. In microbial methane from freshwater ecosystems, in particular, clumped isotope values appear to be controlled by kinetic effects, and may ultimately be useful to study methanogen metabolism.
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- 2017
11. Supplementary material to "Reconciliation of observation- and inventory- based methane emissions for eight large global emitters"
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Petrescu, Ana Maria Roxana, primary, Peters, Glen P., additional, Engelen, Richard, additional, Houweling, Sander, additional, Brunner, Dominik, additional, Tsuruta, Aki, additional, Matthews, Bradley, additional, Patra, Prabir K., additional, Belikov, Dmitry, additional, Thompson, Rona L., additional, Höglund-Isaksson, Lena, additional, Zhang, Wenxin, additional, Segers, Arjo J., additional, Etiope, Giuseppe, additional, Ciotoli, Giancarlo, additional, Peylin, Philippe, additional, Chevallier, Frédéric, additional, Aalto, Tuula, additional, Andrew, Robbie M., additional, Bastviken, David, additional, Berchet, Antoine, additional, Broquet, Grégoire, additional, Conchedda, Giulia, additional, Gütschow, Johannes, additional, Haussaire, Jean-Matthieu, additional, Lauerwald, Ronny, additional, Markkanen, Tiina, additional, van Peet, Jacob C. A., additional, Pison, Isabelle, additional, Regnier, Pierre, additional, Solum, Espen, additional, Scholze, Marko, additional, Tenkanen, Maria, additional, Tubiello, Francesco N., additional, van der Werf, Guido R., additional, and Worden, John R., additional
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- 2024
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12. Reconciliation of observation- and inventory- based methane emissions for eight large global emitters
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Petrescu, Ana Maria Roxana, primary, Peters, Glen P., additional, Engelen, Richard, additional, Houweling, Sander, additional, Brunner, Dominik, additional, Tsuruta, Aki, additional, Matthews, Bradley, additional, Patra, Prabir K., additional, Belikov, Dmitry, additional, Thompson, Rona L., additional, Höglund-Isaksson, Lena, additional, Zhang, Wenxin, additional, Segers, Arjo J., additional, Etiope, Giuseppe, additional, Ciotoli, Giancarlo, additional, Peylin, Philippe, additional, Chevallier, Frédéric, additional, Aalto, Tuula, additional, Andrew, Robbie M., additional, Bastviken, David, additional, Berchet, Antoine, additional, Broquet, Grégoire, additional, Conchedda, Giulia, additional, Gütschow, Johannes, additional, Haussaire, Jean-Matthieu, additional, Lauerwald, Ronny, additional, Markkanen, Tiina, additional, van Peet, Jacob C. A., additional, Pison, Isabelle, additional, Regnier, Pierre, additional, Solum, Espen, additional, Scholze, Marko, additional, Tenkanen, Maria, additional, Tubiello, Francesco N., additional, van der Werf, Guido R., additional, and Worden, John R., additional
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- 2024
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13. Variability and quasi-decadal changes in the methane budget over the period 2000–2012
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Saunois, Marielle, Bousquet, Philippe, Poulter, Ben, Peregon, Anna, Ciais, Philippe, Canadell, Josep G, Dlugokencky, Edward J, Etiope, Giuseppe, Bastviken, David, Houweling, Sander, Janssens-Maenhout, Greet, Tubiello, Francesco N, Castaldi, Simona, Jackson, Robert B, Alexe, Mihai, Arora, Vivek K, Beerling, David J, Bergamaschi, Peter, Blake, Donald R, Brailsford, Gordon, Bruhwiler, Lori, Crevoisier, Cyril, Crill, Patrick, Covey, Kristofer, Frankenberg, Christian, Gedney, Nicola, Höglund-Isaksson, Lena, Ishizawa, Misa, Ito, Akihiko, Joos, Fortunat, Kim, Heon-Sook, Kleinen, Thomas, Krummel, Paul, Lamarque, Jean-François, Langenfelds, Ray, Locatelli, Robin, Machida, Toshinobu, Maksyutov, Shamil, Melton, Joe R, Morino, Isamu, Naik, Vaishali, O'Doherty, Simon, Parmentier, Frans-Jan W, Patra, Prabir K, Peng, Changhui, Peng, Shushi, Peters, Glen P, Pison, Isabelle, Prinn, Ronald, Ramonet, Michel, Riley, William J, Saito, Makoto, Santini, Monia, Schroeder, Ronny, Simpson, Isobel J, Spahni, Renato, Takizawa, Atsushi, Thornton, Brett F, Tian, Hanqin, Tohjima, Yasunori, Viovy, Nicolas, Voulgarakis, Apostolos, Weiss, Ray, Wilton, David J, Wiltshire, Andy, Worthy, Doug, Wunch, Debra, Xu, Xiyan, Yoshida, Yukio, Zhang, Bowen, Zhang, Zhen, and Zhu, Qiuan
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Earth Sciences ,Atmospheric Sciences ,Climate Action ,Astronomical and Space Sciences ,Meteorology & Atmospheric Sciences ,Atmospheric sciences ,Climate change science - Abstract
Following the recent Global Carbon Project (GCP) synthesis of the decadal methane (CH4) budget over 2000-2012 (Saunois et al., 2016), we analyse here the same dataset with a focus on quasi-decadal and inter-annual variability in CH4 emissions. The GCP dataset integrates results from top-down studies (exploiting atmospheric observations within an atmospheric inverse-modelling framework) and bottom-up models (including process-based models for estimating land surface emissions and atmospheric chemistry), inventories of anthropogenic emissions, and data-driven approaches. The annual global methane emissions from top-down studies, which by construction match the observed methane growth rate within their uncertainties, all show an increase in total methane emissions over the period 2000-2012, but this increase is not linear over the 13 years. Despite differences between individual studies, the mean emission anomaly of the top-down ensemble shows no significant trend in total methane emissions over the period 2000-2006, during the plateau of atmospheric methane mole fractions, and also over the period 2008-2012, during the renewed atmospheric methane increase. However, the top-down ensemble mean produces an emission shift between 2006 and 2008, leading to 22 [16-32]Tg CH4yr-1 higher methane emissions over the period 2008-2012 compared to 2002-2006. This emission increase mostly originated from the tropics, with a smaller contribution from mid-latitudes and no significant change from boreal regions. The regional contributions remain uncertain in top-down studies. Tropical South America and South and East Asia seem to contribute the most to the emission increase in the tropics. However, these two regions have only limited atmospheric measurements and remain therefore poorly constrained. The sectorial partitioning of this emission increase between the periods 2002-2006 and 2008-2012 differs from one atmospheric inversion study to another. However, all top-down studies suggest smaller changes in fossil fuel emissions (from oil, gas, and coal industries) compared to the mean of the bottom-up inventories included in this study. This difference is partly driven by a smaller emission change in China from the top-down studies compared to the estimate in the Emission Database for Global Atmospheric Research (EDGARv4.2) inventory, which should be revised to smaller values in a near future. We apply isotopic signatures to the emission changes estimated for individual studies based on five emission sectors and find that for six individual top-down studies (out of eight) the average isotopic signature of the emission changes is not consistent with the observed change in atmospheric 13CH4. However, the partitioning in emission change derived from the ensemble mean is consistent with this isotopic constraint. At the global scale, the top-down ensemble mean suggests that the dominant contribution to the resumed atmospheric CH4 growth after 2006 comes from microbial sources (more from agriculture and waste sectors than from natural wetlands), with an uncertain but smaller contribution from fossil CH4 emissions. In addition, a decrease in biomass burning emissions (in agreement with the biomass burning emission databases) makes the balance of sources consistent with atmospheric 13CH4 observations. In most of the top-down studies included here, OH concentrations are considered constant over the years (seasonal variations but without any inter-annual variability). As a result, the methane loss (in particular through OH oxidation) varies mainly through the change in methane concentrations and not its oxidants. For these reasons, changes in the methane loss could not be properly investigated in this study, although it may play a significant role in the recent atmospheric methane changes as briefly discussed at the end of the paper.
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- 2017
14. The Global Methane Budget: 2000–2012
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Saunois, Marielle, Bousquet, Philippe, Poulter, Ben, Peregon, Anna, Ciais, Philippe, Canadell, Josep G, Dlugokencky, Edward J, Etiope, Giuseppe, Bastviken, David, Houweling, Sander, Janssens-Maenhout, Greet, Tubiello, Francesco N, Castaldi, Simona, Jackson, Robert B, Alexe, Mihai, Arora, Vivek K, Beerling, David J, Bergamaschi, Peter, Blake, Donald R, Brailsford, Gordon, Brovkin, Victor, Bruhwiler, Lori, Crevoisier, Cyril, Crill, Patrick, Curry, Charles, Frankenberg, Christian, Gedney, Nicola, Höglund-Isaksson, Lena, Ishizawa, Misa, Ito, Akihiko, Joos, Fortunat, Kim, Heon-Sook, Kleinen, Thomas, Krummel, Paul, Lamarque, Jean-François, Langenfelds, Ray, Locatelli, Robin, Machida, Toshinobu, Maksyutov, Shamil, McDonald, Kyle C, Marshall, Julia, Melton, Joe R, Morino, Isamu, O'Doherty, Simon, Parmentier, Frans-Jan W, Patra, Prabir K, Peng, Changhui, Peng, Shushi, Peters, Glen P, Pison, Isabelle, Prigent, Catherine, Prinn, Ronald, Ramonet, Michel, Riley, William J, Saito, Makoto, Schroeder, Ronny, Simpson, Isobel J, Spahni, Renato, Steele, Paul, Takizawa, Atsushi, Thornton, Brett F, Tian, Hanqin, Tohjima, Yasunori, Viovy, Nicolas, Voulgarakis, Apostolos, van Weele, Michiel, van der Werf, Guido, Weiss, Ray, Wiedinmyer, Christine, Wilton, David J, Wiltshire, Andy, Worthy, Doug, Wunch, Debra B, Xu, Xiyan, Yoshida, Yukio, Zhang, Bowen, Zhang, Zhen, and Zhu, Qiuan
- Abstract
Abstract. The global methane (CH4) budget is becoming an increasingly important component for managing realistic pathways to mitigate climate change. This relevance, due to a shorter atmospheric lifetime and a stronger warming potential than carbon dioxide, is challenged by the still unexplained changes of atmospheric CH4 over the past decade. Emissions and concentrations of CH4 are continuing to increase making CH4 the second most important human-induced greenhouse gas after carbon dioxide. Two major difficulties in reducing uncertainties come from the large variety of diffusive CH4 sources that overlap geographically, and from the destruction of CH4 by the very short-lived hydroxyl radical (OH). To address these difficulties, we have established a consortium of multi-disciplinary scientists under the umbrella of the Global Carbon Project to synthesize and stimulate research on the methane cycle, and producing regular (~biennial) updates of the global methane budget. This consortium includes atmospheric physicists and chemists, biogeochemists of surface and marine emissions, and socio-economists who study anthropogenic emissions. Following Kirschke et al. (2013), we propose here the first version of a living review paper that integrates results of top-down studies (T-D, exploiting atmospheric observations within an atmospheric inverse-modelling framework) and bottom-up models, inventories, and data-driven approaches (B-U, including process-based models for estimating land surface emissions and atmospheric chemistry, and inventories for anthropogenic emissions, data-driven extrapolations). For the 2003–2012 decade, global methane emissions are estimated by T-D inversions at 558 Tg CH4 yr−1 (range [540–568]). About 60 % of global emissions are anthropogenic (range [50–65 %]). B-U approaches suggest larger global emissions (736 Tg CH4 yr−1 [596–884]) mostly because of larger natural emissions from individual sources such as inland waters, natural wetlands and geological sources. Considering the atmospheric constraints on the T-D budget, it is likely that some of the individual emissions reported by the B-U approaches are overestimated, leading to too large global emissions. Latitudinal data from T-D emissions indicate a predominance of tropical emissions (~64 % of the global budget,
- Published
- 2016
15. Relevant methane emission to the atmosphere from a geological gas manifestation
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Mazzini, Adriano, Sciarra, Alessandra, Etiope, Giuseppe, Sadavarte, Pankaj, Houweling, Sander, Pandey, Sudhanshu, and Husein, Alwi
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- 2021
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16. Methane on Mars: subsurface sourcing and conflicting atmospheric measurements
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Oehler, Dorothy Z., primary and Etiope, Giuseppe, additional
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- 2021
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17. Contributors
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Bahia, Rickbir, primary, Baumgartner, Raphael, additional, Bills, Bruce G., additional, Bontognali, Tomaso R.R., additional, Citron, Robert I., additional, Conway, Susan J., additional, Daubar, Ingrid, additional, Davila, Alfonso F., additional, DiRuggiero, Jocelyne, additional, Djokic, Tara, additional, Dundas, Colin M., additional, Edgett, Kenneth S., additional, El-Maarry, M. Ramy, additional, Etiope, Giuseppe, additional, A. Fraeman, Abigail, additional, Fries, Marc, additional, Gallagher, Colman J., additional, Garvin, James B., additional, Kiyokawa, Shoichi, additional, Leverington, David W., additional, Levy, Joseph S., additional, Oehler, Dorothy Z., additional, Paige, David A., additional, Parker, Timothy J., additional, Powell, Tyler M., additional, Roberts, James H., additional, Rubanenko, Lior, additional, Salvatore, Mark R., additional, Soare, Richard J., additional, Stillman, David E., additional, Sugitani, Kenichiro, additional, Van Kranendonk, Martin J., additional, Viola, Donna, additional, Walter, Malcolm R., additional, Warren-Rhodes, Kimberly, additional, and Williams, Jean-Pierre, additional
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- 2021
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18. Natural Gas
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Etiope, Giuseppe, White, William M., editor, Casey, William H., Associate Editor, Marty, Bernhard, Associate Editor, and Yurimoto, Hisayoshi, Associate Editor
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- 2018
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19. Methane sources and sinks in karst systems: The Nerja cave and its vadose environment (Spain)
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Ojeda, Lucía, Vadillo, Iñaki, Etiope, Giuseppe, Benavente, José, Liñán, Cristina, del Rosal, Yolanda, Tapia, Silvana Teresa, Moríñigo, Miguel Ángel, and Carrasco, Francisco
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- 2019
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20. Reconciliation of observation- and inventory- based methane emissions for eight large global emitters.
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Roxana Petrescu, Ana Maria, Peters, Glen P., Engelen, Richard, Houweling, Sander, Brunner, Dominik, Tsuruta, Aki, Matthews, Bradley, Patra, Prabir K., Belikov, Dmitry, Thompson, Rona L., Höglund-Isaksson, Lena, Wenxin Zhang, Segers, Arjo J., Etiope, Giuseppe, Ciotoli, Giancarlo, Peylin, Philippe, Chevallier, Frédéric, Aalto, Tuula, Andrew, Robbie M., and Bastviken, David
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ATMOSPHERIC methane ,BIOMASS burning ,PARIS Agreement (2016) ,EMISSION inventories ,GOVERNMENT policy on climate change ,METHANE ,SOIL mineralogy - Abstract
Monitoring the spatial distribution and trends in surface greenhouse gas (GHG) fluxes, as well as flux attribution to natural and anthropogenic processes, is essential to track progress under the Paris Agreement and to inform its Global Stocktake. This study updates earlier syntheses (Petrescu et al., 2020, 2021, 2023) and provides a consolidated synthesis of CH
4 emissions using bottom-up (BU) and top-down (TD) approaches for the European Union (EU) and seven additional countries with large anthropogenic and/or natural emissions (USA, Brazil, China, India, Indonesia, Russia, and the Democratic Republic of Congo (DR Congo)). The work utilizes updated National GHG Inventories (NGHGIs) reported by Annex I Parties under the United Nations Framework Convention on Climate Change (UNFCCC) in 2023 and the latest available Biennial Update Reports (BURs) reported by non-Annex I Parties. The NGHGIs are considered in an integrated analysis that also relies on independent flux estimates from global inventory datasets, process-based models, inverse modeling and, when available, respective uncertainties. Whenever possible, it extends the period to 2021. Comparing NGHGIs with other approaches reveals that differences in the emission sources that are included in the estimate is a key source of divergence between approaches. A key system boundary difference is whether both anthropogenic and natural fluxes are included and, if they are, how fluxes belonging to these two sources are grouped/partitioned. Additionally, the natural fluxes are sensitive to the prior geospatial distribution of emissions in atmospheric inversions. Over the studied period, the total CH4 emissions in the EU, USA, and Russia show a steady decreasing trend since 1990, while for the non-EU emitters analyzed in this study, Brazil, China, India, Indonesia, and DR Congo, CH4 emissions have generally increased. In the EU, the anthropogenic BU approaches are reporting relatively similar mean emissions over 2015 to 2020 of 18.5 ± 2.7 Tg CH4 yr-1 for EDGAR v7.0, 16 Tg CH4 yr-1 for GAINS and 19 Tg CH4 yr-1 for FAOSTAT, with the NGHGI estimates of 15 ± 1.8 Tg CH4 yr-1 . Inversions give higher emission estimates as they include natural emissions. Over the same period, the three high-resolution regional inversions report a mean emission of 21 (19-25) Tg CH4 yr-1 , while the mean of six coarser-resolution global inversions results in emission estimates of 24 (23-25) Tg CH4 yr-1 . The magnitude of BU natural emissions (peatland and mineral soils, lakes and reservoirs, geological and biomass burning) accounts for 6.6 Tg CH4 yr-1 (Petrescu et al., 2023a) and explains the differences between the TD inversions and the BU estimates of anthropogenic emissions (including NGHGIs). For the other Annex I Parties in this study (USA and Russia), over 2015 to 2020, the mean of the four anthropogenic BU approaches reports 18.5 (13-27.9) Tg CH4 yr-1 for Russia and 29.1 (23.5- Tg CH4 yr-1 for the USA, against total TD mean estimates of 37 (30-43) Tg CH4 yr-1 and 43.4 (42-48) Tg CH4 yr-1 , respectively. The averaged BU and TD natural emissions account for 16.2 Tg CH4 yr-1 for Russia and 14.6 Tg CH4 yr-1 for the USA, partly explaining the gap between the BU anthropogenic and total TD emissions. For the non-Annex I Parties, anthropogenic CH4 estimates from UNFCCC BURs show large differences with the other global inventory-based estimates and even more with atmospheric-based ones. This poses an important potential challenge to monitoring the progress of the global CH4 pledge and the Global Stocktake, not only from the availability of data but also its accuracy. By systematically comparing the BU with TD methods, this study provides recommendations for more robust comparisons of available data sources and hopes to steadily engage more Parties in using observational methods to complement their UNFCCC inventories, as well as considering their natural emissions. With anticipated improvements in atmospheric modeling and observations, as well as modeling of natural fluxes, future development needs to resolve knowledge gaps in both BU and TD approaches and to better quantify remaining uncertainty. Consequently, TD methods may emerge as a powerful tool for verifying emission inventories for CH4 , and other GHGs and informing international climate policy. The referenced datasets related to figures are available at https://doi.org/10.5281/zenodo.10276087 (Petrescu et al., 2023b). [ABSTRACT FROM AUTHOR]- Published
- 2024
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21. Geophysical and Geochemical Exploration of the Pockmark Field in the Gulf of Patras: New Insights on Formation, Growth and Activity
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Christodoulou, Dimitris, primary, Papatheodorou, George, additional, Geraga, Maria, additional, Etiope, Giuseppe, additional, Giannopoulos, Nikos, additional, Kokkalas, Sotiris, additional, Dimas, Xenophon, additional, Fakiris, Elias, additional, Sergiou, Spyros, additional, Georgiou, Nikos, additional, Sokos, Efthimios, additional, and Ferentinos, George, additional
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- 2023
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22. Hydrocarbon seeps in Romania: Gas origin and release to the atmosphere
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Baciu, Calin, Ionescu, Artur, and Etiope, Giuseppe
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- 2018
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23. Seeps in the Ancient World: Myths, Religions, and Social Development
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Etiope, Giuseppe and Etiope, Giuseppe
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- 2015
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24. Gas Seepage and Past Climate Change
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Etiope, Giuseppe and Etiope, Giuseppe
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- 2015
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25. Gas Migration Mechanisms
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Etiope, Giuseppe and Etiope, Giuseppe
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- 2015
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26. Seepage in Field Geology and Petroleum Exploration
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Etiope, Giuseppe and Etiope, Giuseppe
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- 2015
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27. Environmental Impact of Gas Seepage
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Etiope, Giuseppe and Etiope, Giuseppe
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- 2015
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28. Seepage in Serpentinised Peridotites and on Mars
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Etiope, Giuseppe and Etiope, Giuseppe
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- 2015
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29. Detecting and Measuring Gas Seepage
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Etiope, Giuseppe and Etiope, Giuseppe
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- 2015
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30. Gas Seepage Classification and Global Distribution
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Etiope, Giuseppe and Etiope, Giuseppe
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- 2015
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31. Introduction
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Etiope, Giuseppe and Etiope, Giuseppe
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- 2015
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32. Independent confirmation of a methane spike on Mars and a source region east of Gale Crater
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Giuranna, Marco, Viscardy, Sébastien, Daerden, Frank, Neary, Lori, Etiope, Giuseppe, Oehler, Dorothy, Formisano, Vittorio, Aronica, Alessandro, Wolkenberg, Paulina, Aoki, Shohei, Cardesín-Moinelo, Alejandro, Marín-Yaseli de la Parra, Julia, Merritt, Donald, and Amoroso, Marilena
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- 2019
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33. Using global isotopic data to constrain the role of shale gas production in recent increases in atmospheric methane
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Milkov, Alexei V., Schwietzke, Stefan, Allen, Grant, Sherwood, Owen A., and Etiope, Giuseppe
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- 2020
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34. Mud volcanism: An updated review
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Mazzini, Adriano and Etiope, Giuseppe
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- 2017
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35. Water-rock Interaction Ascribed to Hyperalkaline Mineral Waters in the Cabeço de Vide Serpentinized Ultramafic Intrusive Massif (Central Portugal)
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Marques, José M., Neves, Maria O., Miller, Ana Z., Rocha, Carla, Vance, Steve, Christensen, Lance, Etiope, Giuseppe, Carreira, Paula M., and Suzuki, Shino
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- 2017
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36. Abiotic Methane in Continental Serpentinization Sites: An Overview
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Etiope, Giuseppe
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- 2017
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37. Influence of tectonics on global scale distribution of geological methane emissions
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Ciotoli, Giancarlo, Procesi, Monia, Etiope, Giuseppe, Fracassi, Umberto, and Ventura, Guido
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- 2020
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38. The consolidated European synthesis of CH4 and N2O emissions for the European Union and United Kingdom: 1990–2019
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Petrescu, Ana Maria Roxana, primary, Qiu, Chunjing, additional, McGrath, Matthew J., additional, Peylin, Philippe, additional, Peters, Glen P., additional, Ciais, Philippe, additional, Thompson, Rona L., additional, Tsuruta, Aki, additional, Brunner, Dominik, additional, Kuhnert, Matthias, additional, Matthews, Bradley, additional, Palmer, Paul I., additional, Tarasova, Oksana, additional, Regnier, Pierre, additional, Lauerwald, Ronny, additional, Bastviken, David, additional, Höglund-Isaksson, Lena, additional, Winiwarter, Wilfried, additional, Etiope, Giuseppe, additional, Aalto, Tuula, additional, Balsamo, Gianpaolo, additional, Bastrikov, Vladislav, additional, Berchet, Antoine, additional, Brockmann, Patrick, additional, Ciotoli, Giancarlo, additional, Conchedda, Giulia, additional, Crippa, Monica, additional, Dentener, Frank, additional, Groot Zwaaftink, Christine D., additional, Guizzardi, Diego, additional, Günther, Dirk, additional, Haussaire, Jean-Matthieu, additional, Houweling, Sander, additional, Janssens-Maenhout, Greet, additional, Kouyate, Massaer, additional, Leip, Adrian, additional, Leppänen, Antti, additional, Lugato, Emanuele, additional, Maisonnier, Manon, additional, Manning, Alistair J., additional, Markkanen, Tiina, additional, McNorton, Joe, additional, Muntean, Marilena, additional, Oreggioni, Gabriel D., additional, Patra, Prabir K., additional, Perugini, Lucia, additional, Pison, Isabelle, additional, Raivonen, Maarit T., additional, Saunois, Marielle, additional, Segers, Arjo J., additional, Smith, Pete, additional, Solazzo, Efisio, additional, Tian, Hanqin, additional, Tubiello, Francesco N., additional, Vesala, Timo, additional, van der Werf, Guido R., additional, Wilson, Chris, additional, and Zaehle, Sönke, additional
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- 2023
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39. Methane emissions from abandoned hydrocarbon wells in Italy: inventory, measurement techniques and the role of mega-emitters
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Procesi, Monia, primary, Etiope, Giuseppe, additional, Ciotoli, Giancarlo, additional, and Moroni, Monica, additional
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- 2023
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40. An overview of sedimentary volcanism on Mars
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Brož, Petr, primary, Oehler, Dorothy, additional, Mazzini, Adriano, additional, Hauber, Ernst, additional, Komatsu, Goro, additional, Etiope, Giuseppe, additional, and Cuřín, Vojtěch, additional
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- 2023
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41. The consolidated European synthesis of CH4 and N2O emissions for EU27 and UK: 1990–2019
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Petrescu, Ana-Maria-Roxana, Qiu, Chunjing, McGrath, M.J., Peylin, Philippe, P. Peters, Glen, Ciais, P., Thompson, Rona L., Tsuruta, Aki, Brunner, Dominik, Kuhnert, Matthias, Matthews, Bradley, Palmer, Paul I., Tarasova, Oksana, Regnier, Pierre, Lauerwald, Ronny, Bastviken, David, Höglund-Isaksson, Lena, Winiwarter, Wilfried, Etiope, Giuseppe, Aalto, Tuula, Balsamo, Gianpaolo, Bastrikov, Vladislav, Berchet, Antoine, Brockmann, Patrick, Ciotoli, Giancarlo, Conchedda, Giulia, Crippa, Monica, Dentener, Frank J., Groot Zwaaftink, Christine D., Guizzardi, Diego, Günther, Dirk, Haussaire, Jean-Matthieu, Houweling, Sander, Janssens-Maenhout, Greet, Kouyate, Massaer, Leip, Adrian, Leppänen, Antti, Lugato, Emanuele, Maisonnier, Manon, Manning, Alistair J., Markkanen, Tiina, McNorton, Joe, Muntean, Marilena, Oreggioni, Gabriel D., Patra, Prabir K., Perugini, Lucia, Pison, Isabelle, Raivonen, Maarit T., Saunois, Marielle, Segers, Arjo, Smith, Pete, Solazzo, Efisio, Tian, Hanqin, N. Tubiello, Francesco, Vesala, Timo, van der Werf, Guido, Wilson, Chris, and Zaehle, Sönke
- Abstract
Knowledge of the spatial distribution of the fluxes of greenhouse gases (GHGs) and their temporal variability as well as flux attribution to natural and anthropogenic processes is essential to monitoring the progress in mitigating anthropogenic emissions under the Paris Agreement and to inform its global stocktake. This study provides a consolidated synthesis of CH4 and N2O emissions using bottom-up (BU) and top-down (TD) approaches for the European Union and UK (EU27 + UK) and updates earlier syntheses (Petrescu et al., 2020, 2021). The work integrates updated emission inventory data, process-based model results, data-driven sector model results and inverse modeling estimates, and it extends the previous period of 1990–2017 to 2019. BU and TD products are compared with European national greenhouse gas inventories (NGHGIs) reported by parties under the United Nations Framework Convention on Climate Change (UNFCCC) in 2021. Uncertainties in NGHGIs, as reported to the UNFCCC by the EU and its member states, are also included in the synthesis. Variations in estimates produced with other methods, such as atmospheric inversion models (TD) or spatially disaggregated inventory datasets (BU), arise from diverse sources including within-model uncertainty related to parameterization as well as structural differences between models. By comparing NGHGIs with other approaches, the activities included are a key source of bias between estimates, e.g., anthropogenic and natural fluxes, which in atmospheric inversions are sensitive to the prior geospatial distribution of emissions. For CH4 emissions, over the updated 2015–2019 period, which covers a sufficiently robust number of overlapping estimates, and most importantly the NGHGIs, the anthropogenic BU approaches are directly comparable, accounting for mean emissions of 20.5 Tg CH4 yr−1 (EDGARv6.0, last year 2018) and 18.4 Tg CH4 yr−1 (GAINS, last year 2015), close to the NGHGI estimates of 17.5±2.1 Tg CH4 yr−1. TD inversion estimates give higher emission estimates, as they also detect natural emissions. Over the same period, high-resolution regional TD inversions report a mean emission of 34 Tg CH4 yr−1. Coarser-resolution global-scale TD inversions result in emission estimates of 23 and 24 Tg CH4 yr−1 inferred from GOSAT and surface (SURF) network atmospheric measurements, respectively. The magnitude of natural peatland and mineral soil emissions from the JSBACH–HIMMELI model, natural rivers, lake and reservoir emissions, geological sources, and biomass burning together could account for the gap between NGHGI and inversions and account for 8 Tg CH4 yr−1. For N2O emissions, over the 2015–2019 period, both BU products (EDGARv6.0 and GAINS) report a mean value of anthropogenic emissions of 0.9 Tg N2O yr−1, close to the NGHGI data (0.8±55 % Tg N2O yr−1). Over the same period, the mean of TD global and regional inversions was 1.4 Tg N2O yr−1 (excluding TOMCAT, which reported no data). The TD and BU comparison method defined in this study can be operationalized for future annual updates for the calculation of CH4 and N2O budgets at the national and EU27 + UK scales. Future comparability will be enhanced with further steps involving analysis at finer temporal resolutions and estimation of emissions over intra-annual timescales, which is of great importance for CH4 and N2O, and may help identify sector contributions to divergence between prior and posterior estimates at the annual and/or inter-annual scale. Even if currently comparison between CH4 and N2O inversion estimates and NGHGIs is highly uncertain because of the large spread in the inversion results, TD inversions inferred from atmospheric observations represent the most independent data against which inventory totals can be compared. With anticipated improvements in atmospheric modeling and observations, as well as modeling of natural fluxes, TD inversions may arguably emerge as the most powerful tool for verifying emission inventories for CH4, N2O and other GHGs. The referenced datasets related to figures are visualized at https://doi.org/10.5281/zenodo.7553800 (Petrescu et al., 2023).
- Published
- 2023
42. The consolidated European synthesis of CH4 and N2O emissions for EU27 and UK: 1990-2019
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Petrescu, Ana Maria Roxana, Qiu, Chunjing, McGrath, Matthew J., Peylin, Philippe, Peters, Glen P., Ciais, Philippe, Thompson, Rona L., Tsuruta, Aki, Brunner, Dominik, Kuhnert, Matthias, Matthews, Bradley, Palmer, Paul I., Tarasova, Oksana, Regnier, Pierre, Lauerwald, Ronny, Bastviken, David, Höglund-Isaksson, Lena, Winiwarter, Wilfried, Etiope, Giuseppe, Aalto, Tuula, Balsamo, Gianpaolo, Bastrikov, Vladislav, Berchet, Antoine, Brockmann, Patrick, Ciotoli, Giancarlo, Conchedda, Giulia, Crippa, Monica, Dentener, Frank, Groot Zwaaftink, Christine D., Guizzardi, Diego, Günther, Dirk, Haussaire, Jean-Matthieu, Houweling, Sander, Janssens-Maenhout, Greet, Kouyate, Massaer, Leip, Adrian, Leppänen, Antti, Lugato, Emanuele, Maisonnier, Manon, Markkanen, Tiina, McNorton, Joe, Muntean, Marilena, Oreggioni, Gabriel D., Patra, Prabir K., Perugini, Lucia, Pison, Isabelle, Raivonen, Maarit T., Saunois, Marielle, Smith, Pete, Solazzo, Efisio, Tian, Hanqin, Tubiello, Francesco N., Vesala, Timo, Wilson, Chris, Zaehle, Sönke, Segers, Arjo J., and Manning, Alistair J.
- Subjects
methane, nitrous oxide, european synthesis, bottom-up estimates, inversions - Abstract
This repository contains the data files used for figures, and five updated figuresfrom essd-2022-287 Title: The consolidated European synthesis of CH4 and N2O emissions for EU27 and UK: 1990-2019 Author(s): Ana Maria Roxana Petrescu, Chunjing Qiu, Matthew J. McGrath, Philippe Peylin, Glen P. Peters, Philippe Ciais, Rona L. Thompson, Aki Tsuruta, Dominik Brunner, Matthias Kuhnert, Bradley Matthews, Paul I. Palmer, Oksana Tarasova, Pierre Regnier, Ronny Lauerwald, David Bastviken, Lena Höglund-Isaksson, Wilfried Winiwarter, Giuseppe Etiope, Tuula Aalto, Gianpaolo Balsamo, Vladislav Bastrikov, Antoine Berchet, Patrick Brockmann, Giancarlo Ciotoli, Giulia Conchedda, Monica Crippa, Frank Dentener, Christine D. Groot Zwaaftink, Diego Guizzardi, Dirk Günther, Jean-Matthieu Haussaire, Sander Houweling, Greet Janssens-Maenhout, Massaer Kouyate, Adrian Leip, Antti Leppänen, Emanuele Lugato, Manon Maisonnier, Alistair J. Manning, Tiina Markkanen, Joe McNorton, Marilena Muntean, Gabriel D. Oreggioni, Prabir K. Patra, Lucia Perugini, Isabelle Pison, Maarit T. Raivonen, Marielle Saunois, Arjo J. Segers, Pete Smith, Efisio Solazzo, Hanqin Tian, Francesco N. Tubiello, Timo Vesala, Chris W ilson, and Sönke Zaehle MS type: Review article The data and the DOI numberrefers to the updated version which include the two review comments
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- 2023
43. An overview of sedimentary volcanism on Mars.
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Brož, Petr, Oehler, Dorothy, Mazzini, Adriano, Hauber, Ernst, Komatsu, Goro, Etiope, Giuseppe, and Cuřín, Vojtěch
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MARS (Planet) ,MARTIAN atmosphere ,VOLCANISM ,PLANETARY surfaces ,EARTH (Planet) ,OPEN-ended questions - Abstract
Extensive fields of sub-kilometre- to kilometre-scale mounds, cones, domes, shields, and flow-like edifices cover large parts of the martian lowlands. These features have been compared to structures on Earth produced by sedimentary volcanism – a process that involves subsurface sediment/fluid mobilisation and commonly releases methane to the atmosphere. It was proposed that such processes might help to explain the presence of methane in the martian atmosphere and may also have produced habitable, subsurface settings of potential astrobiological relevance. However, it remains unclear if sedimentary volcanism on Earth and Mars share genetic similarities and hence if methane or other gases were released on Mars during this process. The aim of this review is to summarise the current knowledge about mud-volcano-like structures on Mars, address the critical aspects of this process, identify key open questions, and point to areas where further research is needed to understand this phenomenon and its importance for the Red Planet's geological evolution. We show here that after several decades of exploration, the amount of evidence supporting martian sedimentary volcanism has increased significantly, but as the critical ground truth is still lacking, alternative explanations cannot be ruled out. We also highlight that the lower gravity and temperatures on Mars compared to Earth control the dynamics of clastic eruptions and surface emplacement mechanisms and the resulting morphologies of erupted material. This implies that shapes and triggering mechanisms of mud-volcano-like structures may be different from those observed on Earth. Therefore, comparative studies should be done with caution. To provide a better understanding of the significance of these abundant features on Mars, we argue for follow-up studies targeting putative sedimentary volcanic features identified on the planet's surface and, if possible, for in situ investigations by landed missions such as that by the Zhurong rover. [ABSTRACT FROM AUTHOR]
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- 2023
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44. Massive release of natural hydrogen from a geological seep (Chimaera, Turkey): Gas advection as a proxy of subsurface gas migration and pressurised accumulations
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Etiope, Giuseppe, primary
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- 2022
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45. Upward revision of global fossil fuel methane emissions based on isotope database
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Schwietzke, Stefan, Sherwood, Owen A., Bruhwiler, Lori M. P., Miller, John B., Etiope, Giuseppe, Dlugokencky, Edward J., Michel, Sylvia Englund, Arling, Victoria A., Vaughn, Bruce H., White, James W. C., and Tans, Pieter P.
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Fossil fuels -- Chemical properties -- Environmental aspects ,Emissions (Pollution) -- Research ,Methane -- Chemical properties -- Environmental aspects ,Environmental research ,Environmental issues ,Science and technology ,Zoology and wildlife conservation - Abstract
Author(s): Stefan Schwietzke (corresponding author) [1, 2]; Owen A. Sherwood [3]; Lori M. P. Bruhwiler [2]; John B. Miller [1, 2]; Giuseppe Etiope [4, 5]; Edward J. Dlugokencky [2]; Sylvia [...]
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- 2016
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46. The consolidated European synthesis of CH4 and N2O emissions for EU27 and UK: 1990-2020
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Petrescu, Ana Maria Roxana, Qiu, Chunjing, McGrath, Matthew J., Peylin, Philippe, Peters, Glen P., Ciais, Philippe, Thompson, Rona L., Tsuruta, Aki, Brunner, Dominik, Kuhnert, Matthias, Matthews, Bradley, Palmer, Paul I., Tarasova, Oksana, Regnier, Pierre, Lauerwald, Ronny, Bastviken, David, Höglund-Isaksson, Lena, Winiwarter, Wilfried, Etiope, Giuseppe, Aalto, Tuula, Balsamo, Gianpaolo, Bastrikov, Vladislav, Berchet, Antoine, Brockmann, Patrick, Ciotoli, Giancarlo, Conchedda, Giulia, Crippa, Monica, Dentener, Frank, Groot Zwaaftink, Christine D., Guizzardi, Diego, Günther, Dirk, Haussaire, Jean-Matthieu, Houweling, Sander, Janssens-Maenhout, Greet, Kouyate, Massaer, Leip, Adrian, Leppänen, Antti, Lugato, Emanuele, Maisonnier, Manon, Markkanen, Tiina, McNorton, Joe, Muntean, Marilena, Oreggioni, Gabriel D., Patra, Prabir K., Perugini, Lucia, Pison, Isabelle, Raivonen, Maarit T., Saunois, Marielle, Smith, Pete, Solazzo, Efisio, Tian, Hanqin, Tubiello, Francesco N., Vesala, Timo, Wilson, Chris, Zaehle, Sönke, Segers, Arjo J., and Manning, Alistair J.
- Subjects
methane, nitrous oxide, european synthesis, bottom-up estimates, inversions - Abstract
This repository contains the data files used for the figures in essd-2022-287 Title: The consolidated European synthesis of CH4 and N2O emissions for EU27 and UK: 1990-2020 Author(s): Ana Maria Roxana Petrescu, Chunjing Qiu, Matthew J. McGrath, Philippe Peylin, Glen P. Peters, Philippe Ciais, Rona L. Thompson, Aki Tsuruta, Dominik Brunner, Matthias Kuhnert, Bradley Matthews, Paul I. Palmer, Oksana Tarasova, Pierre Regnier, Ronny Lauerwald, David Bastviken, Lena Höglund-Isaksson, Wilfried Winiwarter, Giuseppe Etiope, Tuula Aalto, Gianpaolo Balsamo, Vladislav Bastrikov, Antoine Berchet, Patrick Brockmann, Giancarlo Ciotoli, Giulia Conchedda, Monica Crippa, Frank Dentener, Christine D. Groot Zwaaftink, Diego Guizzardi, Dirk Günther, Jean-Matthieu Haussaire, Sander Houweling, Greet Janssens-Maenhout, Massaer Kouyate, Adrian Leip, Antti Leppänen, Emanuele Lugato, Manon Maisonnier, Alistair J. Manning, Tiina Markkanen, Joe McNorton, Marilena Muntean, Gabriel D. Oreggioni, Prabir K. Patra, Lucia Perugini, Isabelle Pison, Maarit T. Raivonen, Marielle Saunois, Arjo J. Segers, Pete Smith, Efisio Solazzo, Hanqin Tian, Francesco N. Tubiello, Timo Vesala, Chris W ilson, and Sönke Zaehle MS type: Review article The data and the DOI number are subject to future updates and only refers to this initial, first submission, version of the paper.
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- 2022
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47. Supplementary material to "The consolidated European synthesis of CH4 and N2O emissions for EU27 and UK: 1990–2020"
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Petrescu, Ana Maria Roxana, primary, Qiu, Chunjing, additional, McGrath, Matthew J., additional, Peylin, Philippe, additional, Peters, Glen P., additional, Ciais, Philippe, additional, Thompson, Rona L., additional, Tsuruta, Aki, additional, Brunner, Dominik, additional, Kuhnert, Matthias, additional, Matthews, Bradley, additional, Palmer, Paul I., additional, Tarasova, Oksana, additional, Regnier, Pierre, additional, Lauerwald, Ronny, additional, Bastviken, David, additional, Höglund-Isaksson, Lena, additional, Winiwarter, Wilfried, additional, Etiope, Giuseppe, additional, Aalto, Tuula, additional, Balsamo, Gianpaolo, additional, Bastrikov, Vladislav, additional, Berchet, Antoine, additional, Brockmann, Patrick, additional, Ciotoli, Giancarlo, additional, Conchedda, Giulia, additional, Crippa, Monica, additional, Dentener, Frank, additional, Groot Zwaaftink, Christine D., additional, Guizzardi, Diego, additional, Günther, Dirk, additional, Haussaire, Jean-Matthieu, additional, Houweling, Sander, additional, Janssens-Maenhout, Greet, additional, Kouyate, Massaer, additional, Leip, Adrian, additional, Leppänen, Antti, additional, Lugato, Emanuele, additional, Maisonnier, Manon, additional, Manning, Alistair J., additional, Markkanen, Tiina, additional, McNorton, Joe, additional, Muntean, Marilena, additional, Oreggioni, Gabriel D., additional, Patra, Prabir K., additional, Perugini, Lucia, additional, Pison, Isabelle, additional, Raivonen, Maarit T., additional, Saunois, Marielle, additional, Segers, Arjo J., additional, Smith, Pete, additional, Solazzo, Efisio, additional, Tian, Hanqin, additional, Tubiello, Francesco N., additional, Vesala, Timo, additional, Wilson, Chris, additional, and Zaehle, Sönke, additional
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- 2022
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48. The consolidated European synthesis of CH4 and N2O emissions for EU27 and UK: 1990–2020
- Author
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Petrescu, Ana Maria Roxana, primary, Qiu, Chunjing, additional, McGrath, Matthew J., additional, Peylin, Philippe, additional, Peters, Glen P., additional, Ciais, Philippe, additional, Thompson, Rona L., additional, Tsuruta, Aki, additional, Brunner, Dominik, additional, Kuhnert, Matthias, additional, Matthews, Bradley, additional, Palmer, Paul I., additional, Tarasova, Oksana, additional, Regnier, Pierre, additional, Lauerwald, Ronny, additional, Bastviken, David, additional, Höglund-Isaksson, Lena, additional, Winiwarter, Wilfried, additional, Etiope, Giuseppe, additional, Aalto, Tuula, additional, Balsamo, Gianpaolo, additional, Bastrikov, Vladislav, additional, Berchet, Antoine, additional, Brockmann, Patrick, additional, Ciotoli, Giancarlo, additional, Conchedda, Giulia, additional, Crippa, Monica, additional, Dentener, Frank, additional, Groot Zwaaftink, Christine D., additional, Guizzardi, Diego, additional, Günther, Dirk, additional, Haussaire, Jean-Matthieu, additional, Houweling, Sander, additional, Janssens-Maenhout, Greet, additional, Kouyate, Massaer, additional, Leip, Adrian, additional, Leppänen, Antti, additional, Lugato, Emanuele, additional, Maisonnier, Manon, additional, Manning, Alistair J., additional, Markkanen, Tiina, additional, McNorton, Joe, additional, Muntean, Marilena, additional, Oreggioni, Gabriel D., additional, Patra, Prabir K., additional, Perugini, Lucia, additional, Pison, Isabelle, additional, Raivonen, Maarit T., additional, Saunois, Marielle, additional, Segers, Arjo J., additional, Smith, Pete, additional, Solazzo, Efisio, additional, Tian, Hanqin, additional, Tubiello, Francesco N., additional, Vesala, Timo, additional, Wilson, Chris, additional, and Zaehle, Sönke, additional
- Published
- 2022
- Full Text
- View/download PDF
49. Microbial vs abiotic origin of methane in continental serpentinized ultramafic rocks: A critical review and the need of a holistic approach
- Author
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Etiope, Giuseppe, primary and Oze, Christopher, additional
- Published
- 2022
- Full Text
- View/download PDF
50. Natural Gas
- Author
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Etiope, Giuseppe, primary
- Published
- 2017
- Full Text
- View/download PDF
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