FN Archimer Export Format
PT J
TI Wave groups observed in pancake sea ice
BT 
AF Thomson, Jim
   Gemmrich, Johannes
   Rogers, W. Erick
   Collins, Clarence O.
   ARDHUIN, Fabrice
AS 1:1;2:2;3:3;4:4;5:5;
FF 1:;2:;3:;4:;5:;
C1 Applied Physics Laboratory University of Washington Seattle WA, USA
   University of Victoria ,Victoria BC , Canada
   Naval Research Laboratory ,Stennis Space Center MS, USA
   US Army Research and Development Center, Coastal Hydraulics Laboratory Duck NC , USA
   Univ. Brest, CNRS, Ifremer, IRD, Laboratoire d'Oceanographie Physique et Spatiale Brest 29200 ,France
C2 UNIV WASHINGTON, USA
   UNIV VICTORIA, CANADA
   NAVAL RES LAB, USA
   US ARMY, USA
   CNRS, FRANCE
UM LOPS
IN WOS Cotutelle UMR
   copubli-int-hors-europe
IF 3.559
TC 14
UR https://archimer.ifremer.fr/doc/00587/69864/67763.pdf
   https://archimer.ifremer.fr/doc/00587/69864/67766.pdf
LA English
DT Article
AB Ocean surface waves propagating through sea ice are scattered and dissipated. The net attenuation occurs preferentially at the higher frequencies, and thus the spectral bandwidth of a given wave field is reduced, relative to open water. The reduction in bandwidth is associated with an increase in the groupiness of the wave field. Using SWIFT buoy data from the 2015 Arctic Sea State experiment, bandwidth is compared between pancake ice and open water conditions, and the linkage to group envelopes is explored. The enhancement of wave groups in ice is consistent with the simple linear mechanism of superposition of waves with narrowing spectral bandwidth. This is confirmed using synthetic data. Nonlinear mechanisms, which have been shown as significant in other ice types, are not found to be important in this data set. 
PY 2019
PD NOV
SO Journal Of Geophysical Research-oceans
SN 2169-9275
PU American Geophysical Union (AGU)
VL 124
IS 11
UT 000494997000001
BP 7400
EP 7411
DI 10.1029/2019JC015354
ID 69864
ER

EF