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Low-frequency variability enhancement of the midlatitude climate in an eddy-resolving coupled ocean–atmosphere model—part II: ocean mechanisms
This paper investigates the spatial inhomogeneity of the time-averaged, quasigeostrophic, double-gyre circulation response to fixed, realistic,...
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Competing impacts of tropical Pacific and Atlantic on Southern Ocean inter-decadal variability
The observed Southern Ocean sea surface temperature (SST) has experienced prominent inter-decadal variability nearly in phase with the Inter-decadal...
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A pole-to-equator ocean overturning circulation on Enceladus
Enceladus is believed to have a saltwater global ocean, heated at the ocean–core interface and losing heat to the floating ice shell above. This...
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Distribution of Deep-Water Scleractinian Corals in the Indian Ocean and Its Similarities and Differences with the Distribution in the Pacific Ocean
AbstractThe aim of this article is to clarify the particular distribution of deep-water Indian Ocean scleractinian corals with respect to the...
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Weakening of the Atlantic Meridional Overturning Circulation abyssal limb in the North Atlantic
The abyssal limb of the global Meridional Overturning Circulation redistributes heat and carbon as it carries Antarctic Bottom Water from the...
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Ocean Circulation and Air-Sea Interaction in the South China Sea
This book summarizes achievements of the study on circulation and air–sea interaction and development of the ocean observation network in the South...
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Ocean heat uptake and interbasin redistribution driven by anthropogenic aerosols and greenhouse gases
Anthropogenic aerosols and greenhouse gases have played important roles in modulating the storage and distribution of heat in oceans since the...
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Collapse and slow recovery of the Atlantic Meridional Overturning Circulation (AMOC) under abrupt greenhouse gas forcing
Modeling studies which abruptly increase atmospheric CO 2 concentration evidence a rapid reduction or collapse of the Atlantic Meridional Overturning...
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Oxygenated deep waters fed early Atlantic overturning circulation upon Antarctic glaciation
The Atlantic meridional overturning circulation (AMOC) exerts a major control on the global distribution of heat, dissolved oxygen and carbon in the...
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Rainfall variability and its teleconnection with atmospheric circulation anomalies over southern and southeastern region, Ethiopia
Factors related to rainfall variabilities in southern and southeastern Ethiopia have not yet been addressed. The extreme wet and dry events caused by...
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The changes in south Asian summer monsoon circulation during the mid-Piacenzian warm period
The Mid-Piacenzian (MP; approximately 3.3-3.0 Ma) was a relatively warm period in geological time and this past warming climate was in some respects...
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Future changes in South Asian summer monsoon circulation under global warming: role of the Tibetan Plateau latent heating
The South Asian summer monsoon (SASM) is a significant monsoon system that exerts a profound impact on climate and human livelihoods. According to 38...
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Deep learning to estimate ocean subsurface salinity structure in the Indian Ocean using satellite observations
Accurately estimating the ocean subsurface salinity structure (OSSS) is crucial for understanding ocean dynamics and predicting climate variations....
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Downscaling the ocean response to the Madden–Julian Oscillation in the Northwest Atlantic and adjacent shelf seas
Subseasonal-to-seasonal (S2S) prediction is a global effort to forecast the state of the atmosphere and ocean with lead times between two weeks and a...
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Contrasts of bimodal tropical instability waves (TIWs)-induced wind stress perturbations in the Pacific Ocean among observations, ocean models, and coupled climate models
The coupling between wind stress perturbations and sea surface temperature (SST) perturbations induced by tropical instability waves (TIWs) in the...
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Variational Method for Solving the Quasi-Geostrophic Circulation Problem in a Two-Layer Ocean
AbstractA new variational formulation and a method for solving the problem of quasi-geostrophic dynamics in a two-layer periodic channel are...
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Century-scale carbon sequestration flux throughout the ocean by the biological pump
The ocean contains about 40 times more carbon than the atmosphere, storing 38,000 Pg C as dissolved inorganic carbon (DIC) versus 900 Pg C as carbon...
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Persistent warming and anomalous biogeochemical signatures observed in the Northern Tropical Pacific Ocean during 2013–2020
During 2013–2020, the northern tropical Pacific Ocean (NTPO, 5° N–20° N) experienced a persistent surface warming of over 0.5 °C. This warming was...
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General Circulation of the Atmosphere
TheGeneral circulationatmosphere general circulationCirculation ofGeneral circulation models the atmosphere and oceanGeneral circulationOcean is what...
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Numerical simulations of Atlantic meridional overturning circulation (AMOC) from OMIP experiments and its sensitivity to surface forcing
Atlantic meridional overturning circulation (AMOC) plays an important role in transporting heat meridionally in the Earth’s climate system and is...