Results 151 to 160 of about 3,752 (268)
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
Cosmological analogies for geophysical flows, Lagrangians, and new analogue gravity systems. [PDF]
Faraoni V, Jose S.
europepmc +1 more source
REPORT OF THE GLACIOLOGICAL SURVEY 2017
BARONI C., BONDESAN A., CARTURAN L. & CHIARLE M., Relazioni della campagna glaciologica 2017. (IT ISSN 0391-9838, 2018).Vengono presentate le relazioni annuali relative alle vari-zioni frontali dei ghiacciai italiani rilevati nel corso della campagna glaciologica 2017 da circa 200 operatori volonta-ri che operano nei tre settori alpini (Piemontese ...
Baroni C+3 more
openaire +3 more sources
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
ABSTRACT High‐resolution remote sensing, magnetometry, and trench stratigraphy identify a significant flood event at Lagash (modern Tell al‐Hiba) during the late Early Dynastic period (ca. 2400–2350 BC). Satellite imagery and magnetometry reveal a 90‐meter‐wide meander belt—3–15 times broader than documented canals—adjacent to primary temple districts.
Reed Goodman+8 more
wiley +1 more source
Svalbard's 2024 record summer: An early view of Arctic glacier meltdown? [PDF]
Schuler TV+6 more
europepmc +1 more source
Abstract Accurately predicting Greenland's ice mass loss is crucial for understanding future sea level rise. Approximately 50% of the mass loss results from iceberg calving at the ice‐ocean interface. Ice mélange, a jammed, buoyant granular material that extends for 10 km or more in Greenland's largest fjords, can inhibit iceberg calving and discharge ...
Kavinda Nissanka+7 more
wiley +1 more source