FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2280456580> ?p ?o ?g. }

• W2280456580 endingPage "1553" @default.
• W2280456580 startingPage "1531" @default.
• W2280456580 abstract "Abstract The Arctic Ocean is undergoing a period of rapid transition. Freshwater input is projected to increase, and the decline in Arctic sea ice is likely to drive periodic increases in vertical mixing during ice-free periods. Here, a 1D model of the Arctic Ocean is used to explore how these competing processes will affect the stratification, the stability of the cold halocline, and the sea ice cover at the surface. Initially, stronger shear leads to elevated vertical mixing that causes the mixed layer to warm. The change in temperature, however, is too small to affect the sea ice cover. Most importantly, in the Eurasian Basin, the elevated shear also deepens the halocline and strengthens the stratification over the Atlantic Water thermocline, reducing the vertical heat flux. After about a decade this effect dominates, and the mixed layer begins to cool. The sea ice cover can only be significantly affected if the elevated mixing is sufficient to erode the stratification barrier associated with the cold halocline. While freshwater generally dominates in the Canadian Basin (further isolating the mixed layer from the Atlantic Water layer), in the Eurasian Basin elevated shear reduces the strength of the stratification barrier, potentially allowing Atlantic Water heat to be directly entrained into the mixed layer during episodic mixing events. Therefore, although most sea ice retreat to date has occurred in the Canadian Basin, the results here suggest that, in future decades, elevated vertical mixing may play a more significant role in sea ice melt in the Eurasian Basin." @default.
• W2280456580 created "2016-06-24" @default.
• W2280456580 creator A5017417252 @default.
• W2280456580 creator A5017824948 @default.
• W2280456580 creator A5029227690 @default.
• W2280456580 creator A5062744900 @default.
• W2280456580 date "2016-05-01" @default.
• W2280456580 modified "2023-10-17" @default.
• W2280456580 title "Competing Effects of Elevated Vertical Mixing and Increased Freshwater Input on the Stratification and Sea Ice Cover in a Changing Arctic Ocean" @default.
• W2280456580 cites W1507506485 @default.
• W2280456580 cites W1589831712 @default.
• W2280456580 cites W1651849303 @default.
• W2280456580 cites W1867506197 @default.
• W2280456580 cites W1943471202 @default.
• W2280456580 cites W1963549306 @default.
• W2280456580 cites W1963979445 @default.
• W2280456580 cites W1972711250 @default.
• W2280456580 cites W1973926848 @default.
• W2280456580 cites W1974853484 @default.
• W2280456580 cites W1978487473 @default.
• W2280456580 cites W1988330407 @default.
• W2280456580 cites W1990425071 @default.
• W2280456580 cites W1994928074 @default.
• W2280456580 cites W1998203115 @default.
• W2280456580 cites W1998920319 @default.
• W2280456580 cites W1999154090 @default.
• W2280456580 cites W1999238637 @default.
• W2280456580 cites W2000183650 @default.
• W2280456580 cites W2006188529 @default.
• W2280456580 cites W2006554678 @default.
• W2280456580 cites W2007104457 @default.
• W2280456580 cites W2008801446 @default.
• W2280456580 cites W2010181142 @default.
• W2280456580 cites W2012492797 @default.
• W2280456580 cites W2013376676 @default.
• W2280456580 cites W2016507588 @default.
• W2280456580 cites W2017357503 @default.
• W2280456580 cites W2020002089 @default.
• W2280456580 cites W2021826564 @default.
• W2280456580 cites W2023850230 @default.
• W2280456580 cites W2024193973 @default.
• W2280456580 cites W2026795246 @default.
• W2280456580 cites W2028777311 @default.
• W2280456580 cites W2029463771 @default.
• W2280456580 cites W2030537128 @default.
• W2280456580 cites W2031634764 @default.
• W2280456580 cites W2033357735 @default.
• W2280456580 cites W2040712683 @default.
• W2280456580 cites W2042412895 @default.
• W2280456580 cites W2047438989 @default.
• W2280456580 cites W2050117913 @default.
• W2280456580 cites W2051220568 @default.
• W2280456580 cites W2056294409 @default.
• W2280456580 cites W2058037637 @default.
• W2280456580 cites W2060148338 @default.
• W2280456580 cites W2061249168 @default.
• W2280456580 cites W2063539079 @default.
• W2280456580 cites W2064352977 @default.
• W2280456580 cites W2072068698 @default.
• W2280456580 cites W2077241988 @default.
• W2280456580 cites W2079876722 @default.
• W2280456580 cites W2082909450 @default.
• W2280456580 cites W2087076786 @default.
• W2280456580 cites W2093420722 @default.
• W2280456580 cites W2098474668 @default.
• W2280456580 cites W2101047738 @default.
• W2280456580 cites W2103425624 @default.
• W2280456580 cites W2110385320 @default.
• W2280456580 cites W2115023733 @default.
• W2280456580 cites W2116030881 @default.
• W2280456580 cites W2117944840 @default.
• W2280456580 cites W2121719964 @default.
• W2280456580 cites W2125378957 @default.
• W2280456580 cites W2125918809 @default.
• W2280456580 cites W2129559534 @default.
• W2280456580 cites W2132590819 @default.
• W2280456580 cites W2160567237 @default.
• W2280456580 cites W2165463641 @default.
• W2280456580 cites W2168373356 @default.
• W2280456580 cites W4213280129 @default.
• W2280456580 doi "https://doi.org/10.1175/jpo-d-15-0174.1" @default.
• W2280456580 hasPublicationYear "2016" @default.
• W2280456580 type Work @default.
• W2280456580 sameAs 2280456580 @default.
• W2280456580 citedByCount "24" @default.
• W2280456580 countsByYear W22804565802016 @default.
• W2280456580 countsByYear W22804565802017 @default.
• W2280456580 countsByYear W22804565802018 @default.
• W2280456580 countsByYear W22804565802019 @default.
• W2280456580 countsByYear W22804565802020 @default.
• W2280456580 countsByYear W22804565802021 @default.
• W2280456580 countsByYear W22804565802022 @default.
• W2280456580 countsByYear W22804565802023 @default.
• W2280456580 crossrefType "journal-article" @default.
• W2280456580 hasAuthorship W2280456580A5017417252 @default.
• W2280456580 hasAuthorship W2280456580A5017824948 @default.
• W2280456580 hasAuthorship W2280456580A5029227690 @default.
• W2280456580 hasAuthorship W2280456580A5062744900 @default.

• next