Relationships between the Interannual Variability of Antarctic Sea Ice and the Southern Oscillation [PDF]
Ian Simmonds, T. H. Jacka
openalex +1 more source
Application of modern analog technique to marine Antarctic diatoms: Reconstruction of maximum sea‐ice extent at the Last Glacial Maximum [PDF]
Xavier Crosta, J. Pichon, L. H. Burckle
openalex +1 more source
Abstract Stable isotope analysis of animal tissues is a valuable tool for understanding foraging ecology, habitat use, and developmental changes throughout an animal's life. Stable isotope values of whisker segments offer long‐term data on mammalian foraging, as whisker growth incorporates isotopic signals from the diet and reflects dietary shifts ...
Danelle A. Baronia+3 more
wiley +1 more source
East Antarctic sea ice: observations and modelling [PDF]
A. P. Worby, Xingren Wu
openalex +1 more source
Sea level pressure variability in the Amundsen Sea region inferred from a West Antarctic glaciochemical record [PDF]
Using European Center for Medium‐Range Weather Forecasts (ECMWF) numerical operational analyses, sea ice extent records, and station pressure data, we investigate the influence of sea level pressure variability in the Amundsen Sea region on a West ...
Kreutz, Karl J.+5 more
core +3 more sources
Southern elephant seal movements and Antarctic sea ice [PDF]
Horst Bornemann+6 more
openalex +1 more source
Sea-ice proxies in Antarctic ice cores [PDF]
Röthlisberger, R., Abram, N.J.
openaire +2 more sources
Sea ice floe segmentation in close-range optical imagery using active contour and foundation models [PDF]
The size of sea ice floes is a key factor influencing ice coverage, albedo, wave propagation through ice-covered waters, and ocean-atmosphere energy exchanges. Floe size can be observed by processing visual-range imagery from ships, aircraft, or satellites.
arxiv
Antarctic research yields circumpolar sea ice thickness data [PDF]
A. P. Worby, S. F. Ackley
openalex +1 more source
Uncertainty-enabled machine learning for emulation of regional sea-level change caused by the Antarctic Ice Sheet [PDF]
Projecting sea-level change in various climate-change scenarios typically involves running forward simulations of the Earth's gravitational, rotational and deformational (GRD) response to ice mass change, which requires high computational cost and time.
arxiv