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• W3004205280 endingPage "102287" @default.
• W3004205280 startingPage "102287" @default.
• W3004205280 abstract "On the Western Antarctic Peninsula (WAP), fjords make up most of the interface between the ocean and the cryosphere, and they are hotspots of biological productivity and biodiversity. Changes in the summer upper ocean (50 m) heat content, H, of a fjord could directly affect primary productivity and melting of icebergs and glacial fronts. Using the adjoint of a high-resolution Regional Ocean Model System model, we quantify the key drivers controlling changes in H to understand the summertime characteristics and potential climatic impacts. Results show that the summertime warming is mainly driven by the surface heat flux, and can be enhanced by inward along-fjord winds or northeastward winds along Gerlache strait. Opposite wind perturbations lead to a reduction of H. We learned that the sensitivity to the along-strait winds relates to the exchange of heat between the fjord and the strait, with the strait being a major heat source for the fjord in the unperturbed conditions. The sensitivity analysis of the most influential regional water masses identifies upper ocean waters from the north (<200 m) as the dominant driver. We also find that two possible consequences of climate change, warming air temperature and increasing meltwater input could have opposing effects on H. The additional meltwater leads to a cooling of the fjord that is mainly caused by a reduced import of heat from the strait. It follows that future increases of meltwater input (e.g. increased runoff) could play a crucial role for the fjord’s upper ocean physics and potentially its ecosystem." @default.
• W3004205280 created "2020-02-07" @default.
• W3004205280 creator A5015262395 @default.
• W3004205280 creator A5067776518 @default.
• W3004205280 creator A5077203379 @default.
• W3004205280 creator A5081257608 @default.
• W3004205280 date "2020-04-01" @default.
• W3004205280 modified "2023-10-04" @default.
• W3004205280 title "Sensitivity of the summer upper ocean heat content in a Western Antarctic Peninsula fjord" @default.
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• W3004205280 cites W1608452541 @default.
• W3004205280 cites W1970296979 @default.
• W3004205280 cites W1975360915 @default.
• W3004205280 cites W1975813086 @default.
• W3004205280 cites W1984884576 @default.
• W3004205280 cites W1991121489 @default.
• W3004205280 cites W1995882247 @default.
• W3004205280 cites W2001610213 @default.
• W3004205280 cites W2002254185 @default.
• W3004205280 cites W2004359105 @default.
• W3004205280 cites W2004623363 @default.
• W3004205280 cites W2008701408 @default.
• W3004205280 cites W2009687546 @default.
• W3004205280 cites W2022899902 @default.
• W3004205280 cites W2027769809 @default.
• W3004205280 cites W2032143893 @default.
• W3004205280 cites W2035707289 @default.
• W3004205280 cites W2042510229 @default.
• W3004205280 cites W2054838530 @default.
• W3004205280 cites W2083029864 @default.
• W3004205280 cites W2083390529 @default.
• W3004205280 cites W2084869045 @default.
• W3004205280 cites W2091671937 @default.
• W3004205280 cites W2095769364 @default.
• W3004205280 cites W2096163705 @default.
• W3004205280 cites W2099814811 @default.
• W3004205280 cites W2100986500 @default.
• W3004205280 cites W2104866858 @default.
• W3004205280 cites W2106526756 @default.
• W3004205280 cites W2108001777 @default.
• W3004205280 cites W2108839864 @default.
• W3004205280 cites W2109203458 @default.
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• W3004205280 cites W2117315558 @default.
• W3004205280 cites W2119822306 @default.
• W3004205280 cites W2121406581 @default.
• W3004205280 cites W2122119574 @default.
• W3004205280 cites W2124473308 @default.
• W3004205280 cites W2125664757 @default.
• W3004205280 cites W2126179800 @default.
• W3004205280 cites W2131191693 @default.
• W3004205280 cites W2131872197 @default.
• W3004205280 cites W2134522878 @default.
• W3004205280 cites W2134788165 @default.
• W3004205280 cites W2145895595 @default.
• W3004205280 cites W2147547928 @default.
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• W3004205280 cites W2158924093 @default.
• W3004205280 cites W2164131390 @default.
• W3004205280 cites W2166981921 @default.
• W3004205280 cites W2167058991 @default.
• W3004205280 cites W2170684122 @default.
• W3004205280 cites W2173246082 @default.
• W3004205280 cites W2173502753 @default.
• W3004205280 cites W2174234596 @default.
• W3004205280 cites W2179031310 @default.
• W3004205280 cites W2327626163 @default.
• W3004205280 cites W2336605858 @default.
• W3004205280 cites W2416982532 @default.
• W3004205280 cites W2440054792 @default.
• W3004205280 cites W2463361367 @default.
• W3004205280 cites W2484817568 @default.
• W3004205280 cites W2493642700 @default.
• W3004205280 cites W2531465781 @default.
• W3004205280 cites W2537163483 @default.
• W3004205280 cites W2543905437 @default.
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• W3004205280 doi "https://doi.org/10.1016/j.pocean.2020.102287" @default.
• W3004205280 hasPublicationYear "2020" @default.
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