Zobrazeno 1 - 6
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pro vyhledávání: '"Allison Hogikyan"'
El Nino years stand out in the global average temperature time series as record-warm years. The coupled atmosphere-ocean dynamics leading to warming in the climatologically cold equatorial Eastern Pacific are well understood, but cannot be the cause
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6f1d489804668a48e884171d24e050fe
https://doi.org/10.5194/egusphere-egu23-4180
https://doi.org/10.5194/egusphere-egu23-4180
Autor:
Laure Resplandy, Allison Hogikyan, Hermann Werner Bange, Daniele Bianchi, Thomas S Weber, Wei-Jun Cai, Scott C. Doney, Katja Fennel, Marion Gehlen, Judith Hauck, Fabrice Lacroix, Peter Landschützer, Corinne Le Quéré, Jens Daniel Müller, Raymond Gabriel Najjar, Alizée Roobaert, Sarah Berthet, Laurent Bopp, Trang Thi-Tuyet Chau, Minhan Dai, Nicolas Gruber, Tatiana Ilyina, Annette Kock, Manfredi Manizza, Zouhair Lachkar, Goulven Gildas Laruelle, Enhui Liao, Ivan D. Lima, Cara Nissen, Christian Rödenbeck, Roland Séférian, Jörg Schwinger, Katsuya Toyama, Hiroyuki Tsujino, Pierre Regnier
Publikováno v:
ESS Open Archive
The coastal ocean contributes to regulating atmospheric greenhouse gas concentrations by taking up carbon dioxide (CO2) and releasing nitrous oxide (N2O) and methane (CH4). Major advances have improved our understanding of the coastal air-sea exchang
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bc494bc2bbf478b0160791cb0dd57979
https://doi.org/10.22541/essoar.168182303.39621839/v1
https://doi.org/10.22541/essoar.168182303.39621839/v1
The global ocean is losing oxygen due to warming, which is expected to significantly increase production of nitrous oxide, a greenhouse gas, and decrease the habitat of many megafauna. In the subtropical Atlantic Ocean, however, there is an observed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cdfe8059bd35dae28f59113e69aaea5f
https://doi.org/10.21203/rs.3.rs-2413587/v1
https://doi.org/10.21203/rs.3.rs-2413587/v1
Publikováno v:
Journal of Climate. 33:303-315
The ocean surface albedo is responsible for the distribution of solar (shortwave) radiant energy between the atmosphere and ocean and therefore is a key parameter in Earth’s surface energy budget. In situ ocean observations typically do not measure
During El Niño, the upwelling in the eastern equatorial Pacific (EEP) slows, leading to a warm sea surface temperature (SST) anomaly, and the tropical troposphere warms. Only SSTs in regions with atmospheric deep convection, typically the warmest SS
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2383ebe6fe37716b03d0c8d8bf17d75b
https://doi.org/10.5194/egusphere-egu21-3340
https://doi.org/10.5194/egusphere-egu21-3340