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- W3198793422 endingPage "1073" @default.
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- W3198793422 abstract "Abstract Southern Ocean sea ice can exhibit widespread flooding and subsequent snow-ice formation, due to relatively thick snow covers compared to the total ice thickness. Considerable subkilometer scale variability in snow and ice thickness causes poorly constrained uncertainties in determining the amount of flooding that occurs. Using datasets of snow depth and ice thickness acquired in the Weddell Sea during austral winter 2013 (AWECS campaign) from three floes, we demonstrate large spatial variability of a factor 10 and 5 for snow and combined snow and ice thickness, respectively. The temporal evolution after the floe visit was recorded by automatic weather station and ice mass balance buoys. Using a physics-based, multi-layer snow/sea ice model in a one-dimensional and distributed mode to simulate the thermodynamic processes, we show that the distributed simulations, modeling flooding across the entire heterogeneous floe, produced vastly different amounts of flooding than one-dimensional single point simulations. Three times the flooding is produced in the one-dimensional simulation for the buoy location than distributed (floe-averaged) simulations. The latter is in close agreement with buoy observations. The results suggest that using point observations or one-dimensional simulations to extrapolate processes on the floe-scale can overestimate the amount of flooding and snow-ice formation." @default.
- W3198793422 created "2021-09-13" @default.
- W3198793422 creator A5014068121 @default.
- W3198793422 creator A5022986839 @default.
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- W3198793422 creator A5056043256 @default.
- W3198793422 creator A5067109418 @default.
- W3198793422 creator A5078444388 @default.
- W3198793422 date "2021-08-26" @default.
- W3198793422 modified "2023-10-01" @default.
- W3198793422 title "Spatially distributed simulations of the effect of snow on mass balance and flooding of Antarctic sea ice" @default.
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