Articles | Volume 20, issue 22
https://doi.org/10.5194/acp-20-13929-2020
https://doi.org/10.5194/acp-20-13929-2020
Research article
 | 
19 Nov 2020
Research article |  | 19 Nov 2020

Baffin Bay sea ice extent and synoptic moisture transport drive water vapor isotope (δ18O, δ2H, and deuterium excess) variability in coastal northwest Greenland

Pete D. Akers, Ben G. Kopec, Kyle S. Mattingly, Eric S. Klein, Douglas Causey, and Jeffrey M. Welker

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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Pete D. Akers on behalf of the Authors (23 Aug 2020)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (27 Aug 2020) by Farahnaz Khosrawi
RR by Anonymous Referee #4 (10 Sep 2020)
ED: Publish as is (11 Sep 2020) by Farahnaz Khosrawi
AR by Pete D. Akers on behalf of the Authors (11 Sep 2020)  Manuscript 
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Short summary
Water vapor isotopes recorded for 2 years in coastal northern Greenland largely reflect changes in sea ice cover, with distinct values when Baffin Bay is ice covered in winter vs. open in summer. Resulting changes in moisture transport, surface winds, and air temperature also modify the isotopes. Local glacial ice may thus preserve past changes in the Baffin Bay sea ice extent, and this will help us better understand how the Arctic environment and water cycle responds to global climate change.
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