Overview of the Arctic Sea state and boundary layer physics program
A large collaborative program has studied the coupled air-ice-ocean-wave processes occurring in the Arctic during the autumn ice advance. The program included a field campaign in the western Arctic during the autumn of 2015, with in situ data collection and both aerial and satellite remote sensing....
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ftunivnewcastnsw:uon:35242 2023-05-15T14:34:36+02:00 Overview of the Arctic Sea state and boundary layer physics program Thomson, Jim Ackley, Stephen Fairall, Chris Guest, Peter Gebhardt, Claus Gemmrich, Johannes Graber, Hans C. Holt, Benjamin Lehner, Susanne Lund, Björn Meylan, Michael H. Maksym, Ted Girard-Ardhuin, Fanny Ardhuin, Fabrice Babanin, Alex Boutin, Guillaume Brozena, John Cheng, Sukun Collins, Clarence Doble, Martin The University of Newcastle. Faculty of Science, School of Mathematical and Physical Sciences 2018 http://hdl.handle.net/1959.13/1403957 eng eng Wiley-Blackwell Journal of Geophysical Research: Oceans Vol. 123, Issue 12, p. 8674-8687 10.1002/2018JC013766 Arctic Sea state boundary layer air-ice-ocean-waves Arctic Sea remote sensing journal article 2018 ftunivnewcastnsw 2019-07-08T22:24:04Z A large collaborative program has studied the coupled air-ice-ocean-wave processes occurring in the Arctic during the autumn ice advance. The program included a field campaign in the western Arctic during the autumn of 2015, with in situ data collection and both aerial and satellite remote sensing. Many of the analyses have focused on using and improving forecast models. Summarizing and synthesizing the results from a series of separate papers, the overall view is of an Arctic shifting to a more seasonal system. The dramatic increase in open water extent and duration in the autumn means that large surface waves and significant surface heat fluxes are now common. When refreezing finally does occur, it is a highly variable process in space and time. Wind and wave events drive episodic advances and retreats of the ice edge, with associated variations in sea ice formation types (e.g., pancakes, nilas). This variability becomes imprinted on the winter ice cover, which in turn affects the melt season the following year. Article in Journal/Newspaper Arctic Sea ice NOVA: The University of Newcastle Research Online (Australia) Arctic |
institution |
Open Polar |
collection |
NOVA: The University of Newcastle Research Online (Australia) |
op_collection_id |
ftunivnewcastnsw |
language |
English |
topic |
Arctic Sea state boundary layer air-ice-ocean-waves Arctic Sea remote sensing |
spellingShingle |
Arctic Sea state boundary layer air-ice-ocean-waves Arctic Sea remote sensing Thomson, Jim Ackley, Stephen Fairall, Chris Guest, Peter Gebhardt, Claus Gemmrich, Johannes Graber, Hans C. Holt, Benjamin Lehner, Susanne Lund, Björn Meylan, Michael H. Maksym, Ted Girard-Ardhuin, Fanny Ardhuin, Fabrice Babanin, Alex Boutin, Guillaume Brozena, John Cheng, Sukun Collins, Clarence Doble, Martin Overview of the Arctic Sea state and boundary layer physics program |
topic_facet |
Arctic Sea state boundary layer air-ice-ocean-waves Arctic Sea remote sensing |
description |
A large collaborative program has studied the coupled air-ice-ocean-wave processes occurring in the Arctic during the autumn ice advance. The program included a field campaign in the western Arctic during the autumn of 2015, with in situ data collection and both aerial and satellite remote sensing. Many of the analyses have focused on using and improving forecast models. Summarizing and synthesizing the results from a series of separate papers, the overall view is of an Arctic shifting to a more seasonal system. The dramatic increase in open water extent and duration in the autumn means that large surface waves and significant surface heat fluxes are now common. When refreezing finally does occur, it is a highly variable process in space and time. Wind and wave events drive episodic advances and retreats of the ice edge, with associated variations in sea ice formation types (e.g., pancakes, nilas). This variability becomes imprinted on the winter ice cover, which in turn affects the melt season the following year. |
author2 |
The University of Newcastle. Faculty of Science, School of Mathematical and Physical Sciences |
format |
Article in Journal/Newspaper |
author |
Thomson, Jim Ackley, Stephen Fairall, Chris Guest, Peter Gebhardt, Claus Gemmrich, Johannes Graber, Hans C. Holt, Benjamin Lehner, Susanne Lund, Björn Meylan, Michael H. Maksym, Ted Girard-Ardhuin, Fanny Ardhuin, Fabrice Babanin, Alex Boutin, Guillaume Brozena, John Cheng, Sukun Collins, Clarence Doble, Martin |
author_facet |
Thomson, Jim Ackley, Stephen Fairall, Chris Guest, Peter Gebhardt, Claus Gemmrich, Johannes Graber, Hans C. Holt, Benjamin Lehner, Susanne Lund, Björn Meylan, Michael H. Maksym, Ted Girard-Ardhuin, Fanny Ardhuin, Fabrice Babanin, Alex Boutin, Guillaume Brozena, John Cheng, Sukun Collins, Clarence Doble, Martin |
author_sort |
Thomson, Jim |
title |
Overview of the Arctic Sea state and boundary layer physics program |
title_short |
Overview of the Arctic Sea state and boundary layer physics program |
title_full |
Overview of the Arctic Sea state and boundary layer physics program |
title_fullStr |
Overview of the Arctic Sea state and boundary layer physics program |
title_full_unstemmed |
Overview of the Arctic Sea state and boundary layer physics program |
title_sort |
overview of the arctic sea state and boundary layer physics program |
publisher |
Wiley-Blackwell |
publishDate |
2018 |
url |
http://hdl.handle.net/1959.13/1403957 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Sea ice |
genre_facet |
Arctic Sea ice |
op_relation |
Journal of Geophysical Research: Oceans Vol. 123, Issue 12, p. 8674-8687 10.1002/2018JC013766 |
_version_ |
1766307610551648256 |