Melt onset over Arctic sea ice controlled by atmospheric moisture transport

The timing of melt onset affects the surface energy uptake throughout the melt season. Yet the processes triggering melt and causing its large interannual variability are not well understood. Here we show that melt onset over Arctic sea ice is initiated by positive anomalies of water vapor, clouds,...

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Published inGeophysical research letters Vol. 43; no. 12; pp. 6636 - 6642
Main Authors Mortin, Jonas, Svensson, Gunilla, Graversen, Rune G., Kapsch, Marie‐Luise, Stroeve, Julienne C., Boisvert, Linette N.
Format Journal Article
LanguageEnglish
Published Washington John Wiley & Sons, Inc 28.06.2016
Subjects
Air temperature
Annual variations
Anomalies
Arctic regions
Arctic sea ice
Atmospheric moisture
Atmospheric processes
climate variability
Clouds
Downwelling
Energy
Ice
Interannual variability
Long wave radiation
Marine
melt onset
Melting
Melts
polar meteorology
Radiation
remote sensing
Sea ice
Spring
Surface energy
Surface properties
Trends
Uptake
Variability
Water vapor
Water vapour
Arctic region
PN, Arctic
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Summary:The timing of melt onset affects the surface energy uptake throughout the melt season. Yet the processes triggering melt and causing its large interannual variability are not well understood. Here we show that melt onset over Arctic sea ice is initiated by positive anomalies of water vapor, clouds, and air temperatures that increase the downwelling longwave radiation (LWD) to the surface. The earlier melt onset occurs; the stronger are these anomalies. Downwelling shortwave radiation (SWD) is smaller than usual at melt onset, indicating that melt is not triggered by SWD. When melt occurs early, an anomalously opaque atmosphere with positive LWD anomalies preconditions the surface for weeks preceding melt. In contrast, when melt begins late, clearer than usual conditions are evident prior to melt. Hence, atmospheric processes are imperative for melt onset. It is also found that spring LWD increased during recent decades, consistent with trends toward an earlier melt onset. Key Points Humid air masses trigger Arctic sea ice melt by means of longwave radiation Melt preconditioning of the sea ice surface prior to melt onset Trends toward earlier melt onset linked to positive trends of longwave radiation in spring
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ISSN:0094-8276
1944-8007
1944-8007
DOI:10.1002/2016GL069330