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Record #86462:
Seasonal variations of sea ice motion in the Canada Basin and their implications / Alfred S. McLaren, Mark C. Serreze, Roger G. Barry.
Title: | Seasonal variations of sea ice motion in the Canada Basin and their implications / Alfred S. McLaren, Mark C. Serreze, Roger G. Barry. |
Author(s): | McLaren, Alfred S. Serreze, Mark C. Barry, Roger G. |
Date: | 1987. |
In: | Eos : transactions, American Geophysical Union. (1987.), Vol. 68(44) (1987) |
Abstract: | Abstract of paper to be presented at Fall Meeting of the American Geophysical Union. Analysis of data revealed recurring tendency for reversal of mean clockwise Beaufort Gyre during late summer each year. This previously unidentified, recurrent reversal of ice motion was determined to be in response to seasonal change in atmospheric forcing when anticyclonic regime, which dominates area from October to early summer, is replaced by low-pressure systems. |
Notes: | Eos : transactions, American Geophysical Union. Vol. 68(44) :1228 (1987). |
Keywords: | 551.326.14 -- Floating ice, movement. 551.32 -- Glaciology. 551.326 -- Floating ice. 551.326.12 -- Floating ice, distribution, seasonal. 551.515.7 -- Anticyclones. E6 -- Glaciology: floating ice. (*60) -- Arctic Ocean and adjacent waters. (*601) -- Arctic basin. |
SPRI record no.: | 86462 |
LDR 01534naa#a2200000#a#4500 001 SPRI-86462 005 20240329110121.0 007 ta 008 240329s1987####xx####|##|###|0||#0|eng#d 035 ## ‡aSPRI-86462 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aMcLaren, Alfred S. 245 10 ‡aSeasonal variations of sea ice motion in the Canada Basin and their implications /‡cAlfred S. McLaren, Mark C. Serreze, Roger G. Barry. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1987. 300 ## ‡ap. 1228. 500 ## ‡aEos : transactions, American Geophysical Union. Vol. 68(44) :1228 (1987). 520 3# ‡aAbstract of paper to be presented at Fall Meeting of the American Geophysical Union. Analysis of data revealed recurring tendency for reversal of mean clockwise Beaufort Gyre during late summer each year. This previously unidentified, recurrent reversal of ice motion was determined to be in response to seasonal change in atmospheric forcing when anticyclonic regime, which dominates area from October to early summer, is replaced by low-pressure systems. 650 07 ‡a551.326.14 -- Floating ice, movement.‡2udc 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.326 -- Floating ice.‡2udc 650 07 ‡a551.326.12 -- Floating ice, distribution, seasonal.‡2udc 650 07 ‡a551.515.7 -- Anticyclones.‡2udc 650 07 ‡aE6 -- Glaciology: floating ice.‡2local 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 651 #7 ‡a(*601) -- Arctic basin.‡2udc 700 1# ‡aSerreze, Mark C. 700 1# ‡aBarry, Roger G. 773 0# ‡7nnas ‡tEos : transactions, American Geophysical Union. ‡gVol. 68(44) (1987) ‡wSPRI-1028 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240329