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contributor authorStephens, Britton B.
contributor authorLong, Matthew C.
contributor authorKeeling, Ralph F.
contributor authorKort, Eric A.
contributor authorSweeney, Colm
contributor authorApel, Eric C.
contributor authorAtlas, Elliot L.
contributor authorBeaton, Stuart
contributor authorBent, Jonathan D.
contributor authorBlake, Nicola J.
contributor authorBresch, James F.
contributor authorCasey, Joanna
contributor authorDaube, Bruce C.
contributor authorDiao, Minghui
contributor authorDiaz, Ernesto
contributor authorDierssen, Heidi
contributor authorDonets, Valeria
contributor authorGao, Bo-Cai
contributor authorGierach, Michelle
contributor authorGreen, Robert
contributor authorHaag, Justin
contributor authorHayman, Matthew
contributor authorHills, Alan J.
contributor authorHoecker-Martínez, Martín S.
contributor authorHonomichl, Shawn B.
contributor authorHornbrook, Rebecca S.
contributor authorJensen, Jorgen B.
contributor authorLi, Rong-Rong
contributor authorMcCubbin, Ian
contributor authorMcKain, Kathryn
contributor authorMorgan, Eric J.
contributor authorNolte, Scott
contributor authorPowers, Jordan G.
contributor authorRainwater, Bryan
contributor authorRandolph, Kaylan
contributor authorReeves, Mike
contributor authorSchauffler, Sue M.
contributor authorSmith, Katherine
contributor authorSmith, Mackenzie
contributor authorStith, Jeff
contributor authorStossmeister, Gregory
contributor authorToohey, Darin W.
contributor authorWatt, Andrew S.
date accessioned2019-09-19T10:06:23Z
date available2019-09-19T10:06:23Z
date copyright7/19/2017 12:00:00 AM
date issued2017
identifier otherbams-d-16-0206.1.pdf
identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4261594
description abstractAbstractThe Southern Ocean plays a critical role in the global climate system by mediating atmosphere?ocean partitioning of heat and carbon dioxide. However, Earth system models are demonstrably deficient in the Southern Ocean, leading to large uncertainties in future air?sea CO2 flux projections under climate warming and incomplete interpretations of natural variability on interannual to geologic time scales. Here, we describe a recent aircraft observational campaign, the O2/N2 Ratio and CO2 Airborne Southern Ocean (ORCAS) study, which collected measurements over the Southern Ocean during January and February 2016. The primary research objective of the ORCAS campaign was to improve observational constraints on the seasonal exchange of atmospheric carbon dioxide and oxygen with the Southern Ocean. The campaign also included measurements of anthropogenic and marine biogenic reactive gases; high-resolution, hyperspectral ocean color imaging of the ocean surface; and microphysical data relevant for understanding and modeling cloud processes. In each of these components of the ORCAS project, the campaign has significantly expanded the amount of observational data available for this remote region. Ongoing research based on these observations will contribute to advancing our understanding of this climatically important system across a range of topics including carbon cycling, atmospheric chemistry and transport, and cloud physics. This article presents an overview of the scientific and methodological aspects of the ORCAS project and highlights early findings.
publisherAmerican Meteorological Society
titleThe O2/N2 Ratio and CO2 Airborne Southern Ocean Study
typeJournal Paper
journal volume99
journal issue2
journal titleBulletin of the American Meteorological Society
identifier doi10.1175/BAMS-D-16-0206.1
journal fristpage381
journal lastpage402
treeBulletin of the American Meteorological Society:;2017:;volume 099:;issue 002
contenttypeFulltext


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