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• W2891699449 abstract "Abstract We estimate the cooling flux from snow melting in the ocean through CloudSat satellite snowfall retrievals and reanalysis data. For snowfall events with less than 0.01 mm/hr, this flux is inconsequential. Melting snow begins to compete with other ocean surface heat fluxes as snowfall rates increase beyond 0.1 mm/hr, and it may often become the dominant heat flux as snowfall rates approach and exceed 1 mm/hr. The largest monthly average values of the melting snow cooling flux occur in winter months, approaching −10 W/m 2 in both hemispheres. To determine the regional influence of melting snow on a seasonal basis, we calculate an impact metric that gauges the cooling flux of melting snow against the net flux in the ocean. This metric can be between 20% and 30% in the Northern Hemisphere during March, April, May; the Southern Ocean during March, April, May and September, October, November; and in high‐latitude polar oceans during sea ice freeze up seasons." @default.
• W2891699449 created "2018-09-27" @default.
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• W2891699449 date "2018-09-27" @default.
• W2891699449 modified "2023-10-10" @default.
• W2891699449 title "The Role of Melting Snow in the Ocean Surface Heat Budget" @default.
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• W2891699449 doi "https://doi.org/10.1029/2018gl079182" @default.
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