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- W2884279983 abstract "Abstract Marine-terminating glaciers and ice streams are important controls of ice sheet mass balance. However, understanding of their long-term response to external forcing is limited by relatively short observational records of present-day glaciers and sparse geologic evidence for paleo-glaciers. Here we use a high-resolution ice sheet model with an accurate representation of grounding line dynamics to study the deglaciation of the marine-based south-western Norwegian sector of the Scandinavian Ice Sheet and its sensitivity to ocean and atmosphere forcing. We find that the regional response to a uniform climate change is highly dependent on the local bedrock topography, consistent with ice sheet reconstructions. Our simulations suggest that ocean warming is able to trigger initial retreat in several fjords, but is not sufficient to explain retreat everywhere. Widespread retreat requires additional ice thinning driven by surface melt. Once retreat is triggered, the underlying bedrock topography and fjord width control the rate and extent of retreat, while multi-millennial changes over the course of deglaciation are modulated by surface melt. We suggest that fjord geometry, ice-ocean interactions and grounding line dynamics are vital controls of decadal-to centennial scale ice sheet mass loss. However, we postulate that atmospheric changes are the most important drivers of widespread ice sheet demise, and will likely trump oceanic influence on future ice sheet mass loss and resulting sea level rise over centennial and longer time scales." @default.
- W2884279983 created "2018-08-03" @default.
- W2884279983 creator A5029245501 @default.
- W2884279983 creator A5044444236 @default.
- W2884279983 creator A5045132387 @default.
- W2884279983 creator A5053014625 @default.
- W2884279983 creator A5091477268 @default.
- W2884279983 date "2018-09-01" @default.
- W2884279983 modified "2023-09-24" @default.
- W2884279983 title "Atmosphere-driven ice sheet mass loss paced by topography: Insights from modelling the south-western Scandinavian Ice Sheet" @default.
- W2884279983 cites W1537957428 @default.
- W2884279983 cites W1608543510 @default.
- W2884279983 cites W1626399112 @default.
- W2884279983 cites W1733916393 @default.
- W2884279983 cites W1766836583 @default.
- W2884279983 cites W1808380395 @default.
- W2884279983 cites W1923053496 @default.
- W2884279983 cites W1925984258 @default.
- W2884279983 cites W1931729083 @default.
- W2884279983 cites W1947695452 @default.
- W2884279983 cites W1957873071 @default.
- W2884279983 cites W1964253382 @default.
- W2884279983 cites W1967557711 @default.
- W2884279983 cites W1970388843 @default.
- W2884279983 cites W1970564495 @default.
- W2884279983 cites W1970866483 @default.
- W2884279983 cites W1971799755 @default.
- W2884279983 cites W1975806685 @default.
- W2884279983 cites W1975921484 @default.
- W2884279983 cites W1983844230 @default.
- W2884279983 cites W1984069597 @default.
- W2884279983 cites W2001136877 @default.
- W2884279983 cites W2003371436 @default.
- W2884279983 cites W2009811105 @default.
- W2884279983 cites W2010594743 @default.
- W2884279983 cites W2010917045 @default.
- W2884279983 cites W2015465891 @default.
- W2884279983 cites W2021805059 @default.
- W2884279983 cites W2024500585 @default.
- W2884279983 cites W2030857646 @default.
- W2884279983 cites W2031700439 @default.
- W2884279983 cites W2033125815 @default.
- W2884279983 cites W2034101498 @default.
- W2884279983 cites W2034693675 @default.
- W2884279983 cites W2037757927 @default.
- W2884279983 cites W2043143266 @default.
- W2884279983 cites W2043976103 @default.
- W2884279983 cites W2049855731 @default.
- W2884279983 cites W2051675253 @default.
- W2884279983 cites W2057598108 @default.
- W2884279983 cites W2060960045 @default.
- W2884279983 cites W2062211802 @default.
- W2884279983 cites W2062672751 @default.
- W2884279983 cites W2068086262 @default.
- W2884279983 cites W2071341963 @default.
- W2884279983 cites W2078542147 @default.
- W2884279983 cites W2082143268 @default.
- W2884279983 cites W2083293775 @default.
- W2884279983 cites W2085216145 @default.
- W2884279983 cites W2086504462 @default.
- W2884279983 cites W2091131302 @default.
- W2884279983 cites W2096056455 @default.
- W2884279983 cites W2101679906 @default.
- W2884279983 cites W2102213705 @default.
- W2884279983 cites W2103951855 @default.
- W2884279983 cites W2109295668 @default.
- W2884279983 cites W2109737016 @default.
- W2884279983 cites W2110611537 @default.
- W2884279983 cites W2118808371 @default.
- W2884279983 cites W2121304076 @default.
- W2884279983 cites W2121325849 @default.
- W2884279983 cites W2123027903 @default.
- W2884279983 cites W2127449685 @default.
- W2884279983 cites W2131847138 @default.
- W2884279983 cites W2132146331 @default.
- W2884279983 cites W2134694696 @default.
- W2884279983 cites W2137816126 @default.
- W2884279983 cites W2143514530 @default.
- W2884279983 cites W2144467914 @default.
- W2884279983 cites W2145016426 @default.
- W2884279983 cites W2145084509 @default.
- W2884279983 cites W2149432002 @default.
- W2884279983 cites W2150022032 @default.
- W2884279983 cites W2150376645 @default.
- W2884279983 cites W2150668626 @default.
- W2884279983 cites W2153259684 @default.
- W2884279983 cites W2154903428 @default.
- W2884279983 cites W2157398194 @default.
- W2884279983 cites W2161566360 @default.
- W2884279983 cites W2168312814 @default.
- W2884279983 cites W2170210609 @default.
- W2884279983 cites W2176369079 @default.
- W2884279983 cites W2214397425 @default.
- W2884279983 cites W2256271227 @default.
- W2884279983 cites W2270437352 @default.
- W2884279983 cites W2281988277 @default.
- W2884279983 cites W2282163239 @default.
- W2884279983 cites W2282352865 @default.