Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Matthew P. Couldrey"'
Autor:
Matthew P. Couldrey, Jonathan M. Gregory, Xiao Dong, Oluwayemi Garuba, Helmuth Haak, Aixue Hu, William J. Hurlin, Jiangbo Jin, Johann Jungclaus, Armin Köhl, Hailong Liu, Sayantani Ojha, Oleg A. Saenko, Abhishek Savita, Tatsuo Suzuki, Zipeng Yu, Laure Zanna
Publikováno v:
Climate Dynamics. 60:2003-2039
The effect of anthropogenic climate change in the ocean is challenging to project because atmosphere-ocean general circulation models (AOGCMs) respond differently to forcing. This study focuses on changes in the Atlantic Meridional Overturning Circul
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::57b2864ad99f385b98c60d514b9f3e85
https://doi.org/10.1007/s00382-022-06386-y
https://doi.org/10.1007/s00382-022-06386-y
Autor:
Jonathan M. Gregory, Stephen M. Griffies, Matthew P. Couldrey, Fabio Boeira Dias, Oleg A. Saenko
Publikováno v:
Journal of Climate. 34:2017-2035
Using an ensemble of atmosphere–ocean general circulation models (AOGCMs) in an idealized climate change experiment, this study quantifies the contributions to ocean heat uptake (OHU) from ocean physical parameterizations and resolved dynamical pro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::75b3013dd5af3056972c35f49263a799
https://doi.org/10.1175/jcli-d-20-0652.1
https://doi.org/10.1175/jcli-d-20-0652.1
Autor:
Simon J. Marsland, Catia M. Domingues, Johann H. Jungclaus, A. Todd, Peter Dobrohotoff, Armin Köhl, Stephen M. Griffies, Sayantani Ojha, Abhishek Savita, Laure Zanna, Helmuth Haak, Aixue Hu, Detlef Stammer, Tatsuo Suzuki, Fabio Boeira Dias, Oleg A. Saenko, Andrew Shao, Matthew P. Couldrey, Masayoshi Ishii, Jonathan M. Gregory, Oluwayemi A. Garuba
Publikováno v:
Climate Dynamics
Sea levels of different atmosphere–ocean general circulation models (AOGCMs) respond to climate change forcing in different ways, representing a crucial uncertainty in climate change research. We isolate the role of the ocean dynamics in setting th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::dcfecbd1a60cb55dae91a07905803def
https://centaur.reading.ac.uk/95872/1/382_2020_Article_5471.pdf
https://centaur.reading.ac.uk/95872/1/382_2020_Article_5471.pdf
Thermosteric sea level change, resulting from ocean heat uptake, is a key component of recent and future sea level rise. The various atmosphere-ocean general circulation models (AOGCMs) used to predict future climate produce diverse spatial patterns
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9675067328a3c456623114ecffa19c3c
https://doi.org/10.5194/egusphere-egu2020-18438
https://doi.org/10.5194/egusphere-egu2020-18438
Autor:
Alexander Todd, Laure Zanna, Kewei Lyu, Xuebin Zhang, Riccardo Farneti, Oleg A. Saenko, John A. Church, Duo Yang, Jonathan M. Gregory, Matthew P. Couldrey, René Navarro-Labastida, Quran Wu
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 12, Iss 8, Pp n/a-n/a (2020)
A rise in global mean sea level is a robust feature of projected anthropogenic climate change using state-of-the-art atmosphere-ocean general circulation models (AOGCMs). However, there is considerable disagreement over the more policy-relevant regio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c7e27e126c87b1b90f81b5a44d7849d0
https://doi.org/10.1002/essoar.10501557.1
https://doi.org/10.1002/essoar.10501557.1
The North Atlantic carbon sink is a prominent component of global climate, storing large amounts of atmospheric carbon dioxide (CO2), but this basin’s CO2 uptake variability presents challenges for future climate prediction. A comprehensive mechani
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::80e258d934f9f38164233566008d87d4
https://doi.org/10.5194/bg-2019-16
https://doi.org/10.5194/bg-2019-16
Publikováno v:
Global Biogeochemical Cycles. 30:787-802
The North Atlantic is an important basin for the global ocean's uptake of anthropogenic and natural carbon dioxide (CO2), but the mechanisms controlling this carbon flux are not fully understood. The air-sea flux of CO2, F, is the product of a gas tr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::670b6358f42a52c8f11daf24202fbfad
https://doi.org/10.1002/2015gb005267
https://doi.org/10.1002/2015gb005267
Autor:
Alberto C. Naveira Garabato, Laura Herraiz-Borreguero, Kevin L. Speer, Craig D. Rye, Peter J. Brown, Loïc Jullion, Matthew P. Couldrey, Michael P. Meredith
[1] Four repeat hydrographic sections across the eastern Weddell gyre at 30°E reveal a warming (by ~0.1°C) and lightening (by ~0.02–0.03 kg m−3) of the Antarctic Bottom Water (AABW) entering the gyre from the Indian sector of the Southern Ocean
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::985caa4fd89f4101b3e61ea3c7778489
http://nora.nerc.ac.uk/id/eprint/500831/
http://nora.nerc.ac.uk/id/eprint/500831/
Autor:
Alberto C. Naveira Garabato, Matthew P. Couldrey, Peter J. Brown, Michael P. Meredith, Loïc Jullion
Publikováno v:
Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences. 372:20130041
The densest waters in the Atlantic overturning circulation are sourced at the periphery of Antarctica, especially the Weddell Sea, and flow northward via routes that involve crossing the complex bathymetry of the Scotia Arc. Recent observations of si
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::61e170c4e9cc6a5e60054ebc51ce65e7
https://doi.org/10.1098/rsta.2013.0041
https://doi.org/10.1098/rsta.2013.0041