Ice-water-air exchanges in the marginal ice zone: Numerical simulations of satellite-sensed surface states
The Arctic surface is undergoing rapid changes due to the warming of the Earth’s atmosphere and oceans, including a reduction in perennial sea ice, creation of leads early in the spring, as well as the expansion of marginal ice zone and its fractured sea ice in late spring and summer. The changing s...
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ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5021177 2023-07-30T04:00:59+02:00 Ice-water-air exchanges in the marginal ice zone: Numerical simulations of satellite-sensed surface states Fogarty, J. Bou-Zeid, E. 2023-07-11 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021177 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-4770 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021177 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-4770 2023-07-09T23:40:20Z The Arctic surface is undergoing rapid changes due to the warming of the Earth’s atmosphere and oceans, including a reduction in perennial sea ice, creation of leads early in the spring, as well as the expansion of marginal ice zone and its fractured sea ice in late spring and summer. The changing surface can lead to modifications in Arctic meteorology, which can also then spread to lower latitudes. This study seeks to understand the role of the surface heterogeneity of ice/water patterns on surface-atmosphere coupling. Remote satellite observations (ice-water interface data, among others) are used as a bottom boundary condition for Large Eddy Simulations (LES) of air flow and associated heat transport to understand the non-linear surface-air exchanges. The strong thermal contrast between warm sea water and cold Arctic air/ice is shown to generate convective plumes and secondary circulations that enhance the transport of heat, humidity, and aerosols. The results suggest that surface heterogeneity of the ice-water-air interface acts as a significant driver of accelerated ice melting in the Arctic spring and summer. The long-term goal is to develop parametrizations for mesoscale and global models and enable them to resolve these microscale processes and feedbacks that are not currently resolved. Conference Object Arctic Sea ice GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Arctic |
institution |
Open Polar |
collection |
GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) |
op_collection_id |
ftgfzpotsdam |
language |
English |
description |
The Arctic surface is undergoing rapid changes due to the warming of the Earth’s atmosphere and oceans, including a reduction in perennial sea ice, creation of leads early in the spring, as well as the expansion of marginal ice zone and its fractured sea ice in late spring and summer. The changing surface can lead to modifications in Arctic meteorology, which can also then spread to lower latitudes. This study seeks to understand the role of the surface heterogeneity of ice/water patterns on surface-atmosphere coupling. Remote satellite observations (ice-water interface data, among others) are used as a bottom boundary condition for Large Eddy Simulations (LES) of air flow and associated heat transport to understand the non-linear surface-air exchanges. The strong thermal contrast between warm sea water and cold Arctic air/ice is shown to generate convective plumes and secondary circulations that enhance the transport of heat, humidity, and aerosols. The results suggest that surface heterogeneity of the ice-water-air interface acts as a significant driver of accelerated ice melting in the Arctic spring and summer. The long-term goal is to develop parametrizations for mesoscale and global models and enable them to resolve these microscale processes and feedbacks that are not currently resolved. |
format |
Conference Object |
author |
Fogarty, J. Bou-Zeid, E. |
spellingShingle |
Fogarty, J. Bou-Zeid, E. Ice-water-air exchanges in the marginal ice zone: Numerical simulations of satellite-sensed surface states |
author_facet |
Fogarty, J. Bou-Zeid, E. |
author_sort |
Fogarty, J. |
title |
Ice-water-air exchanges in the marginal ice zone: Numerical simulations of satellite-sensed surface states |
title_short |
Ice-water-air exchanges in the marginal ice zone: Numerical simulations of satellite-sensed surface states |
title_full |
Ice-water-air exchanges in the marginal ice zone: Numerical simulations of satellite-sensed surface states |
title_fullStr |
Ice-water-air exchanges in the marginal ice zone: Numerical simulations of satellite-sensed surface states |
title_full_unstemmed |
Ice-water-air exchanges in the marginal ice zone: Numerical simulations of satellite-sensed surface states |
title_sort |
ice-water-air exchanges in the marginal ice zone: numerical simulations of satellite-sensed surface states |
publishDate |
2023 |
url |
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021177 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Sea ice |
genre_facet |
Arctic Sea ice |
op_source |
XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-4770 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021177 |
op_doi |
https://doi.org/10.57757/IUGG23-4770 |
_version_ |
1772811698568167424 |