Results 201 to 210 of about 197,433 (331)
Abstract This study revisited 158 documented active subglacial lakes across Antarctica, applying a height‐change anomaly delineation algorithm to CryoSat‐2 and ICESat‐2 satellite altimetry data to assemble a 14.75‐year (2010.5–2025.25) time series of active subglacial lake dynamics.
W. Sauthoff +3 more
wiley +1 more source
Antarctic Sea ice distribution detection based on improved ant colony algorithm [PDF]
Xingdong Wang, Zehao Sun
openalex +1 more source
Glacial Expansion of Deoxygenation in the Arabian Sea
Abstract The mechanisms by which ongoing climate change influences ocean Oxygen Minimum Zones (OMZs) are insufficiently understood, making it essential to examine their long‐term variations under substantial climatic forcing. Here, we present the first planktic foraminifera iodine‐to‐calcium records in two Arabian Sea sediment cores: one located within
Deepak Kumar Rai +6 more
wiley +1 more source
Abstract The ice shelves in the Amundsen Sea are being melted rapidly by warm Circumpolar Deep Water (CDW), causing sea‐level rise. Ice‐shelf melt variability is controlled by the speed of a shelf‐break undercurrent which transports CDW onto the continental shelf. We study decadal variability of the undercurrent and ice‐shelf melting using new regional
Michael Haigh +3 more
wiley +1 more source
Southern Ocean Sulfate Aerosol Sources Quantified From Sulfur Isotopes in Antarctic Ice Cores
Abstract The Southern Ocean has emerged as a key region for constraining aerosol‐climate interactions due to its relatively low anthropogenic influence. Sulfate is an important aerosol over the Southern Ocean, and models suggest dimethyl sulfide (DMS) is the largest source of sulfate during summer.
U. A. Jongebloed +5 more
wiley +1 more source
The Roles of Sea-Ice, Light and Sedimentation in Structuring Shallow Antarctic Benthic Communities
Graeme F. Clark +4 more
openalex +2 more sources
The Zonal Wave‐3 Mode Impacts Antarctic Dense Water Formation
Abstract At the Antarctic margins, dense water masses form as sea ice develops, driving the Antarctic branch of the global meridional overturning circulation. Previous studies found that large‐scale climate modes such as the Southern Annular Mode and El Niño Southern do not fully account for the interannual variability of dense water formation.
M. Auger, P. Spence, A. K. Morrison
wiley +1 more source
Antarctic sea ice multidecadal variability triggered by Southern Annular Mode and deep convection [PDF]
Yushi Morioka +6 more
openalex +1 more source
Abstract Global ocean circulation regulates climate and has undergone significant changes over the Cenozoic. Today, the Atlantic Meridional Overturning Circulation (AMOC) is driven by North Atlantic Deep Water (NADW) formation and Southern Ocean upwelling.
Erwan Pineau +7 more
wiley +1 more source
Future Shoaling of the AMOC and Its Impact on Oceanic Heat Transport to the Subpolar North Atlantic
Abstract The Atlantic Meridional Overturning Circulation (AMOC) carries oceanic heat northward to the subpolar North Atlantic (SPNA), where the surface water cools and sinks to the deep ocean. According to a large‐ensemble simulation under a medium‐to‐high emission scenario, the surface cooling and oceanic heat convergence in the SPNA may decrease to ...
Sang‐Ki Lee +3 more
wiley +1 more source

