FN Archimer Export Format
PT J
TI Emerging trends in the sea state of the Beaufort and Chukchi seas
BT 
AF THOMSON, Jim
   FAN, Yalin
   STAMMERJOHN, Sharon
   STOPA, Justin
   ROGERS, W. Erick
   GIRARD-ARDHUIN, Fanny
   ARDHUIN, Fabrice
   SHEN, Hayley
   PERRIE, Will
   SHEN, Hui
   ACKLEY, Steve
   BABANIN, Alex
   LIU, Qingxiang
   GUEST, Peter
   MAKSYM, Ted
   WADHAMS, Peter
   FAIRALL, Chris
   PERSSON, Ola
   DOBLE, Martin
   GRABER, Hans
   LUND, Bjoern
   SQUIRE, Vernon
   GEMMRICH, Johannes
   LEHNER, Susanne
   HOLT, Benjamin
   MEYLAN, Mike
   BROZENA, John
   BIDLOT, Jean-Raymond
AS 1:1;2:2;3:3;4:4;5:2;6:27;7:4;8:5;9:6,7;10:6,7;11:8;12:9,10;13:10,11;14:12;15:13;16:14;17:15,16;18:15,16;19:17;20:18;21:19;22:20;23:21;24:22;25:23;26:24;27:25;28:26;
FF 1:;2:;3:;4:PDG-ODE-LOPS-SIAM;5:;6:PDG-ODE-LOPS-SIAM;7:;8:;9:;10:;11:;12:;13:;14:;15:;16:;17:;18:;19:;20:;21:;22:;23:;24:;25:;26:;27:;28:;
C1 Univ Washington, Appl Phys Lab, Seattle, WA 98105 USA.
   Naval Res Lab, Div Oceanog, Stennis Space Ctr, MS USA.
   Univ Colorado, Inst Arctic & Alpine Res, Boulder, CO 80309 USA.
   Univ Brest, CNRS, IFREMER, IRD,LOPS,IUEM, F-29280 Brest, France.
   Clarkson Univ, Dept Civil & Environm Engn, Potsdam, NY USA.
   Fisheries & Oceans Canada, Dartmouth, NS, Canada.
   Bedford Inst Oceanog, Dartmouth, NS, Canada.
   UTSA, Snow & Ice Geophys Lab, San Antonio, TX USA.
   Univ Melbourne, Dept Infrastruct Engn, Melbourne, Vic, Australia.
   Swinburne Univ Technol, Fac Sci Engn & Technol, Melbourne, Vic, Australia.
   Ocean Univ China, Qingdao Collaborat Innovat Ctr Marine Sci & Techn, Phys Oceanog Lab, Qingdao, Peoples R China.
   Naval Postgrad Sch, Dept Meteorol, Monterey, CA USA.
   Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA.
   Univ Cambridge, Cambridge, England.
   Univ Colorado, CIRES, Boulder, CO 80309 USA.
   NOAA, Div Phys Sci, Boulder, CO USA.
   Polar Sci Ltd, Buckingham, England.
   Univ Miami, Ctr Southeastern Trop Adv Remote Sensing, Coral Gables, FL 33124 USA.
   Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Coral Gables, FL 33124 USA.
   Univ Otago, Dept Math & Stat, Dunedin, New Zealand.
   Univ Victoria, Victoria, BC, Canada.
   German Aerosp Ctr DLR, Cologne, Germany.
   CALTECH, Jet Prop Lab, Pasadena, CA 91125 USA.
   Univ Newcastle, Sch Math & Phys Sci, Callaghan, NSW 2308, Australia.
   Naval Res Lab, Marine Geosci Div, Code 7420, Washington, DC 20375 USA.
   European Ctr Medium Range Weather Forecasts, Redding, England.
C2 UNIV WASHINGTON, USA
   NAVAL RES LAB, USA
   UNIV COLORADO, USA
   CNRS, FRANCE
   CLARKSON UNIV, USA
   MPO, CANADA
   BEDFORD INST OCEANOG, CANADA
   UTSA, USA
   UNIV MELBOURNE, AUSTRALIA
   UNIV TECHNOL SWINBURNE, AUSTRALIA
   UNIV OCEAN CHINA, CHINA
   NAVAL POSTGRAD SCH, USA
   WHOI, USA
   UNIV CAMBRIDGE, UK
   UNIV COLORADO, USA
   NOAA, USA
   POLAR SCI LTD, UK
   UNIV MIAMI, USA
   UNIV MIAMI, USA
   UNIV OTAGO, NEW ZEALAND
   UNIV VICTORIA, CANADA
   GERMAN AEROSP CTR DLR, GERMANY
   CALTECH, USA
   UNIV NEWCASTLE, AUSTRALIA
   NAVAL RES LAB, USA
   ECMWF, UK
   IFREMER, FRANCE
SI BREST
SE PDG-ODE-LOPS-SIAM
UM LOPS
IN WOS Ifremer jusqu'en 2018
   copubli-france
   copubli-europe
   copubli-univ-france
   copubli-int-hors-europe
   copubli-sud
IF 3.341
TC 77
UR https://archimer.ifremer.fr/doc/00345/45590/45202.pdf
LA English
DT Article
DE ;Sea ice;Arctic Ocean;Ocean surface waves
AB The sea state of the Beaufort and Chukchi seas is controlled by the wind forcing and the amount of ice-free water available to generate surface waves. Clear trends in the annual duration of the open water season and in the extent of the seasonal sea ice minimum suggest that the sea state should be increasing, independent of changes in the wind forcing. Wave model hindcasts from four selected years spanning recent conditions are consistent with this expectation. In particular, larger waves are more common in years with less summer sea ice and/or a longer open water season, and peak wave periods are generally longer. The increase in wave energy may affect both the coastal zones and the remaining summer ice pack, as well as delay the autumn ice-edge advance. However, trends in the amount of wave energy impinging on the ice-edge are inconclusive, and the associated processes, especially in the autumn period of new ice formation, have yet to be well-described by in situ observations. There is an implicit trend and evidence for increasing wave energy along the coast of northern Alaska, and this coastal signal is corroborated by satellite altimeter estimates of wave energy.
PY 2016
PD SEP
SO Ocean Modelling
SN 1463-5003
PU Elsevier Sci Ltd
VL 105
UT 000386771800001
BP 1
EP 12
DI 10.1016/j.ocemod.2016.02.009
ID 45590
ER

EF