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Showing posts with label Antarctic Ice Sheet. Show all posts
Showing posts with label Antarctic Ice Sheet. Show all posts

Wednesday, February 8, 2023

Universities of Edinburgh, Cambridge and Washington (January 2023) - Antarctic ice sheet retreat slowed by ocean changes

Title:
Antarctic ice sheet retreat slowed by ocean changes
 
Published:
The University of Edinburgh, 27 January 2023

From the article:
A team of researchers from the Universities of Edinburgh, Cambridge and Washington used satellite imagery and climate and ocean records to obtain the most detailed understanding yet of how the West Antarctic Ice Sheet is responding to climate change.
 

Tuesday, December 22, 2020

Modeling the breakup of tabular icebergs [Scholarly Article - Science Advances, 16 December 2020]

Title:
Modeling the breakup of tabular icebergs
 
Authors:
Mark R. England1&2, Till J.W. Wagner1 & Ian Eisenman2
1. Department of Physics and Physical Oceanography, University of North Carolina Wilmington, Wilmington, NC, USA. 
2. Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA, USA.

Published:
Science Advances, Volume 6, Number 51, eabd1273 (16 December 2020)

Abstract:
Nearly half of the freshwater flux from the Antarctic Ice Sheet into the Southern Ocean occurs in the form of large tabular icebergs that calve off the continent’s ice shelves. However, because of difficulties in adequately simulating their breakup, large Antarctic icebergs to date have either not been represented in models or represented but with no breakup scheme such that they consistently survive too long and travel too far compared with observations. Here, we introduce a representation of iceberg fracturing using a breakup scheme based on the “footloose mechanism.” We optimize the parameters of this breakup scheme by forcing the iceberg model with an ocean state estimate and comparing the modeled iceberg trajectories and areas with the Antarctic Iceberg Tracking Database. We show that including large icebergs and a representation of their breakup substantially affects the iceberg meltwater distribution, with implications for the circulation and stratification of the Southern Ocean.