Relationship between the sea ice cover in the retreat and advance seasons in the Antarctic Ocean [PDF]
Sohey Nihashi, Κay I. Ohshima
openalex +1 more source
Abstract Seismic waves preceding the core phase PKIKP, known as PKP precursors, have been used to map small scatterers near the core‐mantle boundary (CMB). However, their low signal‐to‐noise ratio has required manual identification, hindering systematic and comprehensive analysis.
Shang Ma+6 more
wiley +1 more source
Variations of surface air temperature and sea-ice extent in the western Antarctic Peninsula region [PDF]
Raymond C. Smith, Sharon Stammerjohn
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Glacial-ice fragments in Antarctic sea ice [PDF]
David N. Thomas, Christian Haas
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The Reversibility of Antarctic Sea Ice Loss Under CO2 Removal Scenarios
Abstract A pronounced decline in Antarctic sea ice has been observed since 2014, with major changes in the Earth system. This study investigates whether these impacts can be reversed by removing atmospheric greenhouse gases. Using carbon dioxide removal experiments from the Coupled Model Intercomparison Project Phase 6, we identify considerable inter ...
Sirui Li+3 more
wiley +1 more source
Thermal Conductivity of Sea Ice and Antarctic Permafrost [PDF]
Daniel Pringle
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Photosynthetic energy conversion under extreme conditions—I: important role of lipids as structural modulators and energy sink under N-limited growth in Antarctic sea ice diatoms [PDF]
Thomas Möck, Bernd M. A. Kroon
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Controls on Fjord Temperature Throughout Greenland in a Reduced‐Physics Model
Abstract Greenland's fjords modulate exchanges between its outlet glaciers and the open ocean. Subglacial discharge and iceberg melt redistribute heat and salt in the fjord, modifying waters at glacier fronts and impacting glacier melt. Considering observations are sparse and general circulation models are computationally expensive, we use a reduced ...
Martim Mas e Braga+5 more
wiley +1 more source
Mycosporine-Like Amino Acids in Antarctic Sea Ice Algae, and Their Response to UVB Radiation [PDF]
Ken G. Ryan+3 more
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Early Warming Over the Southern Ocean During the Last Deglaciation
Abstract The last deglaciation, ca. 17,000–11,000 years before present (yr BP), marks the most recent period of large‐scale climate reorganization on Earth. However, the timing and spatial patterns of the initial warming preceding these changes remain uncertain.
Peisong Zheng+2 more
wiley +1 more source