[HTML][HTML] Revisiting circulation and water masses over the East Antarctic margin (80–150° E)
Full-depth hydrographic sections of the BROKE experiment in 1996 (across the Antarctic
margin from 80 to 150° E; Bindoff et al., 2000) were revisited for the first time during the …
margin from 80 to 150° E; Bindoff et al., 2000) were revisited for the first time during the …
Modeling ocean circulation and ice shelf melt in the Bellingshausen Sea
S Hyogo, Y Nakayama… - Journal of Geophysical …, 2024 - Wiley Online Library
The ice shelves in the Bellingshausen Sea are melting and thinning rapidly due to modified
Circumpolar Deep Water (mCDW) intrusions carrying heat toward ice‐shelf cavities …
Circumpolar Deep Water (mCDW) intrusions carrying heat toward ice‐shelf cavities …
Descriptions and patterns in opportunistic marine debris collected near Palmer Station, Antarctica
Observations of marine debris in Antarctica have been increasing; however, impacts,
distributions, sources, and transport pathways of debris remain poorly understood. Here, we …
distributions, sources, and transport pathways of debris remain poorly understood. Here, we …
Reduced Deep Convection and Bottom Water Formation Due To Antarctic Meltwater in a Multi‐Model Ensemble
The additional water from the Antarctic ice sheet and ice shelves due to climate‐induced
melt can impact ocean circulation and global climate. However, the major processes driving …
melt can impact ocean circulation and global climate. However, the major processes driving …
Decoupling of the Surface and Bottom‐Intensified Antarctic Slope Current in Regions of Dense Shelf Water Export
Abstract The Antarctic Slope Current is guided by the topographic gradient of the Antarctic
continental slope and creates a dynamical barrier between the continental shelf and the …
continental slope and creates a dynamical barrier between the continental shelf and the …
Sources and pathways of glacial meltwater in the Bellingshausen Sea, Antarctica
Meltwater content and pathways determine the impact of Antarctica's melting ice shelves on
ocean circulation and climate. Using ocean glider observations, we quantify meltwater …
ocean circulation and climate. Using ocean glider observations, we quantify meltwater …
Ice-shelf freshwater triggers for the Filchner–Ronne Ice Shelf melt tip** point in a global ocean–sea-ice model
MJ Hoffman, C Branecky Begeman… - The …, 2024 - tc.copernicus.org
Some ocean modeling studies have identified a potential tip** point from a low to a high
basal melt regime beneath the Filchner–Ronne Ice Shelf (FRIS), Antarctica, with significant …
basal melt regime beneath the Filchner–Ronne Ice Shelf (FRIS), Antarctica, with significant …
Floating debris and organisms can raft to Antarctic coasts from all major Southern Hemisphere landmasses
Antarctica's unique marine ecosystems are threatened by the arrival of non‐native marine
species on rafting ocean objects. The harsh environmental conditions in Antarctica prevent …
species on rafting ocean objects. The harsh environmental conditions in Antarctica prevent …
Sensitivity of Antarctic shelf waters and abyssal overturning to local winds
Winds around the Antarctic continental margin are known to exert a strong control on the
local ocean stratification and circulation. However, past work has largely focused on the …
local ocean stratification and circulation. However, past work has largely focused on the …
An Amundsen Sea source of decadal temperature changes on the Antarctic continental shelf
Mass loss from the Antarctic Ice Sheet is dominated by basal melting–induced warm ocean
water. Ice-sheet mass loss and thinning of buttressing ice shelves occur primarily in the …
water. Ice-sheet mass loss and thinning of buttressing ice shelves occur primarily in the …