Results 161 to 170 of about 123,794 (282)

How to Predict the Phase Shift of “Warm Arctic–Cold Eurasia” Pattern Between Early and Late Winter?

Journal of Geophysical Research: Atmospheres, Volume 131, Issue 13, 16 July 2026.
Abstract The “Warm Arctic−Cold Eurasia” (WACE) pattern frequently undergoes distinct phase reversals between early and late winter, posing significant challenges for climate prediction. Current state‐of‐the‐art real‐time prediction models exhibit limited skill in forecasting WACE reversals, and the main reason is poor representation of key atmospheric ...
Zhicong Yin, Tianbao Xu
wiley   +1 more source

Compound drivers of Antarctic sea ice loss and Southern Ocean destratification. [PDF]

Sci Adv
Narayanan A, Ayres H, England MH, Haumann FA, Mazloff MR, Silvano A, Spira T, Zhou S, Naveira Garabato AC.   +8 more
europepmc   +1 more source

A Vast Valley Network Beneath the Greenland Ice Sheet

Geophysical Research Letters, Volume 53, Issue 13, 16 July 2026.
Abstract Mapping subglacial topography along the margin of the Greenland Ice Sheet was revolutionized by reconciling measurements of ice thickness and surface velocity using the principle of mass conservation. Despite evidence that many subglacial valleys resolved by that method extend upstream, it cannot be applied to the ice sheet's slower‐flowing ...
Allison M. Chartrand, Joseph A. MacGregor, Mathieu Morlighem, Olga V. Sergienko, Helen Ockenden, William T. Colgan, Gong Cheng   +6 more
wiley   +1 more source

Recent extremes in Antarctic sea ice extent modulated by ocean heat ventilation. [PDF]

Proc Natl Acad Sci U S A
Wilson EA, Arlen L, Campbell EC.
europepmc   +1 more source

Sea Ice Latent Heat Becomes More Active in the Arctic Sea Ice Energy Budget

Geophysical Research Letters, Volume 53, Issue 13, 16 July 2026.
Abstract Arctic sea ice has experienced rapid decrease in recent decades. The sea ice property changes have altered its thermodynamic processes, enhancing the heat exchange among atmosphere‐ocean‐ice surface. However, heat exchange associated with sea ice phase‐change process, which is defined as sea ice latent heat, have received relatively little ...
Yuang Liu, Lujun Zhang, Guorui Shi, Xi Liang   +3 more
wiley   +1 more source

Weak 21st‐Century AMOC Response to Greenland Meltwater in a Strongly Eddying Ocean Model

Geophysical Research Letters, Volume 53, Issue 13, 16 July 2026.
Abstract Climate models project that the Atlantic Meridional Overturning Circulation (AMOC) will weaken in the 21st century, but the magnitude is highly uncertain. Some of this uncertainty is structural, as most climate models neglect increasing meltwater from the Greenland ice sheet and do not explicitly capture mesoscale ocean eddies.
Oliver Mehling, Henk A. Dijkstra
wiley   +1 more source

Antarctic Sea-Ice

Sharon Stammerjohn, Clare Eayrs, F. Alexander Haumann, Will Hobbs, Marika Holland, Phillip Reid, Lettie A. Roach, Madison Smith   +7 more
openaire   +2 more sources

Comparative genomics of an Antarctic sea-ice diatom (<i>Nitzschia</i> sp.) provides insights into potential polar adaptation. [PDF]

Front Microbiol
Zhai C, Kennedy F, Han M, Yu H, Sun J, Liang Y, Wang M, McMinn A.   +7 more
europepmc   +1 more source

Tidal Mixing on the Antarctic Continental Slope Enhances Ocean Heat Transport With Implications for Sea Ice

Geophysical Research Letters, Volume 53, Issue 13, 16 July 2026.
Abstract Ocean microstructure measurements collected during three austral summers (2023–2025) along the Antarctic continental slope off Dronning Maud Land show enhanced subsurface mixing. Mean turbulent dissipation between 100 and 800 m depth is an order of magnitude higher than in the open ocean, with an extreme event reaching 3×10−6 $3\times 1{0}^{-6}
Johanne Jahnsen Hus, Amelie Meyer, Tore Hattermann, Beatriz Peña‐Molino, Casimir de Lavergne   +4 more
wiley   +1 more source

Tracing the Abyssal Water Pathways in the Indian Ocean

Geophysical Research Letters, Volume 53, Issue 13, 16 July 2026.
Abstract Antarctic‐origin abyssal waters occupy a significant fraction of the global ocean volume and play a key role in deep circulation and ventilation, yet their volume is declining rapidly in a warming climate. Although the Indian Ocean (IO) contains a substantial fraction of these waters, abyssal pathways and upwelling in the basin remain poorly ...
Kaushik Mishra, Bishakhdatta Gayen, Kathryn L. Gunn, P. N. Vinayachandran, Nihar Paul   +4 more
wiley   +1 more source