Zobrazeno 1 - 10
of 260
pro vyhledávání: '"Ocean Heat Uptake"'
Publikováno v:
Advances in Climate Change Research, Vol 14, Iss 4, Pp 546-559 (2023)
The diversity of surface-flux perturbations, especially for heat-flux perturbations, notably leads to uncertainties surrounding the responses of ocean climate under global warming scenarios projected by climate/Earth system models. However, when impo
Externí odkaz:
https://doaj.org/article/91120c45b45f47c38bfe14bd8988b458
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 23, Pp n/a-n/a (2023)
Abstract Greenhouse gases and aerosols play a major role in controlling global climate change. Greenhouse gases drive a radiative imbalance which warms the ocean, while aerosols cool the ocean. Since 1980, the effective radiation felt by the planet d
Externí odkaz:
https://doaj.org/article/0bd65a609680493e81f1e568936f6939
Autor:
Gaopeng Xu, Ping Chang, Justin Small, Gokhan Danabasoglu, Stephen Yeager, Sanjiv Ramachandran, Qiuying Zhang
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 21, Pp n/a-n/a (2023)
Abstract Ocean warming is a key factor impacting future changes in climate. Here we investigate vertical structure changes in globally averaged ocean heat content (OHC) in high‐ (HR) and low‐resolution (LR) future climate simulations with the Com
Externí odkaz:
https://doaj.org/article/6ce289ec25bd471287280adef0ff9670
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 22, Pp n/a-n/a (2023)
Abstract The Ocean Heat Uptake Efficiency (OHUE) quantifies the ocean's ability to mitigate surface warming through deep heat sequestration. Despite its importance, the main controls on OHUE, and on its two‐fold spread across contemporary climate m
Externí odkaz:
https://doaj.org/article/de302d901c72485fa627dedfffa7a356
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 18, Pp n/a-n/a (2023)
Abstract The impacts of stratospheric ozone recovery on Southern Ocean surface and interior temperature, heat content, heat uptake, and heat transport are investigated by contrasting two ensemble chemistry‐climate model simulations in 2005–2099:
Externí odkaz:
https://doaj.org/article/65e975a306c44b48a8191c84cce79403
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 8, Pp n/a-n/a (2023)
Abstract Seismically generated sound waves that propagate through the ocean are used to infer temperature anomalies and their vertical structure in the deep East Indian Ocean. These T waves are generated by earthquakes off Sumatra and received by hyd
Externí odkaz:
https://doaj.org/article/0f6c332483e248b1be9f6af1878febce
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 4, Pp n/a-n/a (2023)
Abstract Ocean heat uptake (OHU) plays an important role in determining the rate of surface warming under CO2 forcing. We examined the transient response to CO2 forcing in a set of 30 climate models from Coupled Model Intercomparison Project Phase 6
Externí odkaz:
https://doaj.org/article/9056e1f1bdb44f0cb72e8ff3156f4aef
Akademický článek
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Akademický článek
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K zobrazení výsledku je třeba se přihlásit.
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Autor:
Sergei A. Soldatenko, Robert A. Colman
Publikováno v:
Tellus: Series A, Dynamic Meteorology and Oceanography, Vol 74, Iss 1 (2022)
Climate models used in theoretical studies and the long-term projections of climate change should be able to reproduce essential features of the Earth’s climate system including natural global scale variability on timescales from years to decades.
Externí odkaz:
https://doaj.org/article/8bb03b2ba3dc4075a9c878ea0fc65dd7