FN Archimer Export Format
PT J
TI Overview of the Arctic Sea State and Boundary Layer Physics Program
BT 
AF THOMSON, Jim
   ACKLEY, Stephen
   GIRARD-ARDHUIN, Fanny
   ARDHUIN, Fabrice
   BABANIN, Alex
   BOUTIN, Guillaume
   BROZENA, John
   CHENG, Sukun
   COLLINS, Clarence
   DOBLE, Martin
   FAIRALL, Chris
   GUEST, Peter
   GEBHARDT, Claus
   GEMMRICH, Johannes
   GRABER, Hans C.
   HOLT, Benjamin
   LEHNER, Susanne
   LUND, Bjorn
   MEYLAN, Michael H.
   MAKSYM, Ted
   MONTIEL, Fabien
   PERRIE, Will
   PERSSON, Ola
   RAINVILLE, Luc
   ROGERS, W. Erick
   SHEN, Hui
   SHEN, Hayley
   SQUIRE, Vernon
   STAMMERJOHN, Sharon
   STOPA, Justin
   SMITH, Madison M.
   SUTHERLAND, Peter
   WADHAMS, Peter
AS 1:1;2:2;3:3;4:24;5:4;6:24;7:5;8:6;9:7;10:8;11:9,10;12:11;13:12;14:13;15:14;16:15;17:12;18:14;19:16;20:17;21:18;22:19,20;23:9,10;24:1;25:21;26:19,20;27:6;28:18;29:22;30:3;31:1;32:3;33:23;
FF 1:;2:;3:PDG-ODE-LOPS-SIAM;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;14:;15:;16:;17:;18:;19:;20:;21:;22:;23:;24:;25:;26:;27:;28:;29:;30:PDG-ODE-LOPS-SIAM;31:;32:PDG-ODE-LOPS-SIAM;33:;
C1 Univ Washington, Appl Phys Lab, Seattle, WA 98105 USA.
   UTSA, Snow & Ice Geophys Lab, San Antonio, TX USA.
   Univ Brest, CNRS, IFREMER, IRD,LOPS,IUEM, Brest, France.
   Univ Melbourne, Dept Ocean Engn, Melbourne, Vic, Australia.
   Naval Res Lab, Marine Geosci Div, Washington, DC 20375 USA.
   Clarkson Univ, Dept Civil & Environm Engn, Potsdam, NY USA.
   US Army, Coastal & Hydraul Lab, Engineer Res & Dev Ctr, Duck, NC USA.
   Polar Sci Ltd, Appin, Argyll, Scotland.
   Univ Colorado, CIRES, Boulder, CO 80309 USA.
   NOAA, Phys Sci Div, Boulder, CO USA.
   US Navy, Postgrad Sch, Dept Meteorol, Monterey, CA 93943 USA.
   German Aerosp Ctr DLR, SAR Oceanog, Bremen, Germany.
   Univ Victoria, Phys & Astron, Victoria, BC, Canada.
   Univ Miami, CSTARS, Miami, FL USA.
   CALTECH, Jet Prop Lab, Pasadena, CA USA.
   Univ Newcastle, Sch Math & Phys Sci, Callaghan, NSW, Australia.
   Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA.
   Univ Otago, Dept Math & Stat, Dunedin, New Zealand.
   Fisheries & Oceans Canada, Dartmouth, NS, Canada.
   Bedford Inst Oceanog, Dartmouth, NS, Canada.
   Naval Res Lab, Hancock, MS USA.
   Univ Colorado Boulder, Inst Arctic & Alpine Res, Boulder, CO USA.
   Univ Cambridge, Dept Appl Math & Theoret Phys, Cambridge, England.
C2 UNIV WASHINGTON, USA
   UNIV TEXAS SAN ANTONIO, USA
   IFREMER, FRANCE
   UNIV MELBOURNE, AUSTRALIA
   MARINE GEOSCIENCES DIV, USA
   UNIV CLARKSON, USA
   US ARMY, USA
   POLAR SCI LTD, UK
   UNIV COLORADO, USA
   NOAA, USA
   US NAVY, USA
   DLR, GERMANY
   UNIV VICTORIA, CANADA
   UNIV MIAMI, USA
   CALTECH, USA
   UNIV NEWCASTLE, AUSTRALIA
   WHOI, USA
   UNIV OTAGO, NEW ZEALAND
   MPO, CANADA
   BEDFORD INST OCEANOG, CANADA
   NAVAL RES LAB, USA
   UNIV COLORADO BOULDER, USA
   UNIV CAMBRIDGE, UK
   CNRS, FRANCE
SI BREST
SE PDG-ODE-LOPS-SIAM
UM LOPS
IN WOS Ifremer jusqu'en 2018
   copubli-france
   copubli-europe
   copubli-int-hors-europe
IF 3.235
TC 93
UR https://archimer.ifremer.fr/doc/00437/54837/56313.pdf
   https://archimer.ifremer.fr/doc/00437/54837/61562.bst
   https://archimer.ifremer.fr/doc/00437/54837/61563.cls
   https://archimer.ifremer.fr/doc/00437/54837/61564.bib
   https://archimer.ifremer.fr/doc/00437/54837/61565.bbl
LA English
DT Article
DE ;Arctic;waves;autumn;sea ice;Beaufort;flux
AB 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. 
PY 2018
PD DEC
SO Journal Of Geophysical Research-oceans
SN 2169-9275
PU Amer Geophysical Union
VL 123
IS 12
UT 000456405900001
BP 8674
EP 8687
DI 10.1002/2018JC013766
ID 54837
ER

EF