Are Warm Ocean Currents Melting the Ice in Antarctica?
نویسندگان
چکیده
منابع مشابه
Response of Southern Ocean circulation to global warming may enhance basal ice shelf melting around Antarctica
We investigate the large-scale oceanic features determining the future ice shelf–ocean interaction by analyzing global warming experiments in a coarse resolution climate model with a comprehensive ocean component. Heat and freshwater fluxes from basal ice shelf melting (ISM) are parameterized following Beckmann and Goosse [Ocean Model 5(2):157–170, 2003]. Melting sensitivities to the oceanic te...
متن کاملRapid submarine ice melting in the grounding zones of ice shelves in West Antarctica
Enhanced submarine ice-shelf melting strongly controls ice loss in the Amundsen Sea embayment (ASE) of West Antarctica, but its magnitude is not well known in the critical grounding zones of the ASE's major glaciers. Here we directly quantify bottom ice losses along tens of kilometres with airborne radar sounding of the Dotson and Crosson ice shelves, which buttress the rapidly changing Smith, ...
متن کاملOcean mixing beneath Pine Island Glacier ice shelf, West Antarctica
Ice shelves around Antarctica are vulnerable to an increase in ocean-driven melting, with the melt rate depending on ocean temperature and the strength of flow inside the ice-shelf cavities. We present measurements of velocity, temperature, salinity, turbulent kinetic energy dissipation rate, and thermal variance dissipation rate beneath Pine Island Glacier ice shelf, West Antarctica. These mea...
متن کاملOcean freshening, sea level rising, sea ice melting
[1] Estimates of 20th Century sea level rise are typically 1.5 to 2 mm/y, with a steric contribution of (0.5 ± 0.2) mm/y. Estimates of the eustatic contribution vary widely between 1.1 and +1.3 mm/y. We attempt an independent estimate of eustatic sea level rise based on the measured freshening of the global ocean, and with attention to the contribution from melting of sea ice (which affects fre...
متن کاملWarm ocean is eroding West Antarctic Ice Sheet
[1] Satellite radar measurements show that ice shelves in Pine Island Bay have thinned by up to 5.5 m yr 1 over the past decade. The pattern of shelf thinning mirrors that of their grounded tributaries the Pine Island, Thwaites and Smith glaciers and ocean currents on average 0.5 C warmer than freezing appear to be the source. The synchronised imbalance of the inland glaciers is the result of r...
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ژورنال
عنوان ژورنال: Frontiers for Young Minds
سال: 2020
ISSN: 2296-6846
DOI: 10.3389/frym.2020.00124