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- W2085773619 abstract "Projections of sea level rise due to ice loss from the land to the ocean have been hampered by a lack of understanding of the role the ocean is playing in glacier retreat, including the processes that contribute to the supply of warm water to the ice-ocean interface. Here shipboard, moored, and weather station data collected off Jorge Montt, a rapidly retreating glacier in Patagonia, are analyzed to understand the influence of wind forcing. During summer, synoptic-scale down-fjord wind events enhance an estuarine-like two-layer flow, increasing the inflow of oceanic deep water. During up-fjord wind events, the inflow of deep water is significantly reduced, and a three-layer exchange flow develops. Overall, along-fjord wind forcing is shown to modulate the inflow of warm water to the fjord by a factor of 2.5 The results sug- gest that local, channelized winds can be an important process modulating warm water supply and melting of tidewater glaciers." @default.
- W2085773619 created "2016-06-24" @default.
- W2085773619 creator A5044995325 @default.
- W2085773619 date "2014-06-02" @default.
- W2085773619 modified "2023-10-18" @default.
- W2085773619 title "Wind-driven modulation of warm water supply to a proglacial fjord, Jorge Montt Glacier, Patagonia" @default.
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- W2085773619 doi "https://doi.org/10.1002/2014gl060071" @default.
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