Atlantic deep water formation occurs primarily in the Iceland Basin and Irminger Sea by local buoyancy forcing
Abstract The Atlantic Meridional Overturning Circulation (AMOC), a key mechanism in the
climate system, delivers warm and salty waters from the subtropical gyre to the subpolar …
climate system, delivers warm and salty waters from the subtropical gyre to the subpolar …
[HTML][HTML] A limited role for unforced internal variability in twentieth-century warming
Aldrin, M., M. Holden, P. Guttorp, R. Skeie, G. Myhre, and T. Berntsen, 2012: Bayesian
estimation of climate sensitivity based on a simple climate model fitted to observations of …
estimation of climate sensitivity based on a simple climate model fitted to observations of …
Sea-ice retreat suggests re-organization of water mass transformation in the Nordic and Barents Seas
Water mass transformation in the Nordic and Barents Seas, triggered by air-sea heat fluxes,
is an integral component of the Atlantic Meridional Overturning Circulation (AMOC). These …
is an integral component of the Atlantic Meridional Overturning Circulation (AMOC). These …
Indian Ocean warming as a driver of the North Atlantic warming hole
S Hu, AV Fedorov - Nature communications, 2020 - nature.com
Over the past century, the subpolar North Atlantic experienced slight cooling or suppressed
warming, relative to the background positive temperature trends, often dubbed the North …
warming, relative to the background positive temperature trends, often dubbed the North …
Century-long cooling trend in subpolar North Atlantic forced by atmosphere: an alternative explanation
A well-known exception to rising sea surface temperatures (SST) across the globe is the
subpolar North Atlantic, where SST has been declining at a rate of 0.39 (±±0.23) K century …
subpolar North Atlantic, where SST has been declining at a rate of 0.39 (±±0.23) K century …
Volume, heat, and freshwater divergences in the subpolar North Atlantic suggest the Nordic Seas as key to the state of the meridional overturning circulation
L Chafik, T Rossby - Geophysical Research Letters, 2019 - Wiley Online Library
The meridional overturning circulation (MOC) decreases rapidly in subpolar and Nordic
regions where the warm upper layer loses its buoyancy due to intense heat loss, sinks, and …
regions where the warm upper layer loses its buoyancy due to intense heat loss, sinks, and …
A hybrid deep learning framework with physical process description for simulation of evapotranspiration
Evapotranspiration (ET) estimation models can be broadly classified as statistical or physical
process based models. However, assuming the limitation of individual approaches, the …
process based models. However, assuming the limitation of individual approaches, the …
A clearer view of Southern Ocean air–sea interaction using surface heat flux asymmetry
SA Josey, JP Grist, JV Mecking… - … Transactions of the …, 2023 - royalsocietypublishing.org
Progress in understanding Southern Ocean heat exchange and wind forcing is discussed
and new results presented. These include a metric of the zonal asymmetry between surface …
and new results presented. These include a metric of the zonal asymmetry between surface …
Role of air–sea fluxes and ocean surface density in the production of deep waters in the eastern subpolar gyre of the North Atlantic
Wintertime convection in the North Atlantic Ocean is a key component of the global climate
as it produces dense waters at high latitudes that flow equatorward as part of the Atlantic …
as it produces dense waters at high latitudes that flow equatorward as part of the Atlantic …
Mechanisms for late 20th and early 21st century decadal AMOC variability
Recent studies using data from the OSNAP observational campaign and from numerical
ocean models suggest that the Iceland Basin and the Irminger Sea may be more significant …
ocean models suggest that the Iceland Basin and the Irminger Sea may be more significant …