Sea ice velocity in the Fram Strait monitored by moored instruments
(2003) In Geophysical Research Letters 30(19). Abstract
The Fram Strait Sea ice velocity was measured by means of a new method using moored Doppler Current Meters in the period 19962000. Almost 3 years of ice velocity observations near 79°N 5°W are analyzed. The average southward ice velocity was 0.16 m/s. The correlation between the ice velocity and the crossstrait sea level pressure (SLP) difference was R = 0.76 for daily means and R = 0.79 for monthly means. The same crossstrait SLP difference exhibits a positive trend since 1950 of 10% of the mean per decade. By a simple linear model we compute mean sea ice area flux to 850 000 km^{2}/year for the period 19502000. Ice thickness, monitored by means of Upward Looking Sonars since 1990, is also discussed. The combined data gave... (More)
The Fram Strait Sea ice velocity was measured by means of a new method using moored Doppler Current Meters in the period 19962000. Almost 3 years of ice velocity observations near 79°N 5°W are analyzed. The average southward ice velocity was 0.16 m/s. The correlation between the ice velocity and the crossstrait sea level pressure (SLP) difference was R = 0.76 for daily means and R = 0.79 for monthly means. The same crossstrait SLP difference exhibits a positive trend since 1950 of 10% of the mean per decade. By a simple linear model we compute mean sea ice area flux to 850 000 km^{2}/year for the period 19502000. Ice thickness, monitored by means of Upward Looking Sonars since 1990, is also discussed. The combined data gave a monthly ice volume flux of 200 km^{3} during the last decade with no significant trend.
(Less)
 author
 Widell, K. ^{LU} ; Østerhus, S. and Gammelsrød, T.
 publishing date
 20031001
 type
 Contribution to journal
 publication status
 published
 subject
 in
 Geophysical Research Letters
 volume
 30
 issue
 19
 publisher
 American Geophysical Union
 external identifiers

 scopus:17744421225
 ISSN
 00948276
 language
 English
 LU publication?
 no
 id
 eb53e435bf6446a9882b9026dc68bafe
 date added to LUP
 20170614 16:45:42
 date last changed
 20180529 12:26:44
@article{eb53e435bf6446a9882b9026dc68bafe, abstract = {<p>The Fram Strait Sea ice velocity was measured by means of a new method using moored Doppler Current Meters in the period 19962000. Almost 3 years of ice velocity observations near 79°N 5°W are analyzed. The average southward ice velocity was 0.16 m/s. The correlation between the ice velocity and the crossstrait sea level pressure (SLP) difference was R = 0.76 for daily means and R = 0.79 for monthly means. The same crossstrait SLP difference exhibits a positive trend since 1950 of 10% of the mean per decade. By a simple linear model we compute mean sea ice area flux to 850 000 km<sup>2</sup>/year for the period 19502000. Ice thickness, monitored by means of Upward Looking Sonars since 1990, is also discussed. The combined data gave a monthly ice volume flux of 200 km<sup>3</sup> during the last decade with no significant trend.</p>}, author = {Widell, K. and Østerhus, S. and Gammelsrød, T.}, issn = {00948276}, language = {eng}, month = {10}, number = {19}, publisher = {American Geophysical Union}, series = {Geophysical Research Letters}, title = {Sea ice velocity in the Fram Strait monitored by moored instruments}, volume = {30}, year = {2003}, }