Episodic Reversal of Autumn Ice Advance Caused by Release of Ocean Heat in the Beaufort Sea-Reference-Cited by-同舟云学术

Episodic Reversal of Autumn Ice Advance Caused by Release of Ocean Heat in the Beaufort Sea

Published:2018-05 Issue:5 Volume:123 Page:3164-3185
ISSN:2169-9275
Container-title:Journal of Geophysical Research: Oceans
language:en
Short-container-title:J. Geophys. Res. Oceans

Author:

Smith Madison¹^ORCID,Stammerjohn Sharon²^ORCID,Persson Ola³^ORCID,Rainville Luc¹,Liu Guoqiang⁴,Perrie William⁴^ORCID,Robertson Robin⁵^ORCID,Jackson Jennifer⁶^ORCID,Thomson Jim¹^ORCID

Affiliation:

1. Applied Physics LaboratoryUniversity of WashingtonSeattle WA USA

2. Institute of Arctic & Alpine Research, University of ColoradoBoulder CO USA

3. NOAA/ESRL Physical Sciences DivisionBoulder CO USA

4. Bedford Institute of Oceanography, Fisheries & Oceans CanadaDartmouth NS Canada

5. China‐ASEAN College of Marine Sciences, Xiamen University, SepangSelangor Malaysia

6. Hakai Science, Hakai InstituteCalvert Island BC Canada

Funder

Office of Naval Research

Publisher

American Geophysical Union (AGU)

Subject

Earth and Planetary Sciences (miscellaneous),Space and Planetary Science,Geochemistry and Petrology,Geophysics,Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2018JC013764

Reference75 articles.

1. Synoptic Climatology of the Southern Beaufort Sea Troposphere with Comparisons to Surface Winds

2. Fracture of summer perennial sea ice by ocean swell as a result of Arctic storms

3. Implications of fractured Arctic perennial ice cover on thermodynamic and dynamic sea ice processes

4. The parameterization of surface albedo for sea ice and its snow cover

5. Modeling the interplay between sea ice formation and the oceanic mixed layer: Limitations of simple brine rejection parameterizations

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