Results 251 to 260 of about 2,868,735 (385)
Decoupled Antarctic and Subarctic export productivity under intensified Southern Hemisphere westerlies during the last interglacial. [PDF]
Lu L +10 more
europepmc +1 more source
Short-term temporal variability in offshore benthic biodiversity across hydrographic regions at a sub-Antarctic archipelago [PDF]
Eleonora Puccinelli +4 more
openalex +1 more source
Abstract The standing meanders of the Antarctic Circumpolar Current are key sites of mixing and meridional transport in the Southern Ocean, but their long‐term variability and trends remain poorly understood. Here, we investigate the Pacific‐Antarctic Ridge meander using satellite altimetry data from 1993 to 2023.
Xinlong Liu, Chengcheng Yang, Yanyu Chen
wiley +1 more source
Cool libraries in a melting world : Proceedings of the 23rd Polar Libraries Colloquy 2010, June 13-18, 2010, Bremerhaven, Germany [PDF]
Brannemann, Marcel, Carle, Daria O.
core +1 more source
Abstract Primitive asteroids and carbonaceous chondrites (CCs) record the history of processes in the early solar system. Visible and shortwave infrared (VSWIR) spectroscopy of primitive asteroids and bulk‐powdered CCs has identified shared spectral features suggestive of shared parent body origins.
S. A. Parra +2 more
wiley +1 more source
Turbulent isopycnal mixing dominates thermohaline transformations of intermediate ocean waters. [PDF]
Sévellec F, Kolodziejczyk N, Portela E.
europepmc +1 more source
Abstract Terrestrial water storage (TWS) plays an important role in describing the Earth system, as water availability is decisive for ecosystems and human development. Since 2002, the Gravity Recovery and Climate Experiment (GRACE) and its Follow‐On (GRACE‐FO) mission have measured TWS anomalies with unprecedented accuracy, enabling a leap in ...
Luis Q. Gentner +5 more
wiley +1 more source
Abstract Dense shelf water (DSW) formed on Antarctica's continental shelves is a significant precursor for Antarctic Bottom Water (AABW), a critical component of global overturning circulation. We hypothesize that DSW cascades off the central Ross Sea shelf generated density currents that entrained sediment as they flowed down Hillary Canyon, resulting
Natalia Varela +6 more
wiley +1 more source

