SPRI library catalogue
View a record
Please note: You are viewing the legacy database of the Scott Polar Research Institute Library catalogue. It is no longer being updated, so does not reliably reflect our current library holdings.
Please search for material in iDiscover for up-to-date information about the library collection.
Record #103491:
Reversals of Beaufort gyre sea ice circulation and effects on ice concentration in the Canada Basin / Mark C. Serreze, Roger G. Barry, Alfred S. McLaren.
Title: | Reversals of Beaufort gyre sea ice circulation and effects on ice concentration in the Canada Basin / Mark C. Serreze, Roger G. Barry, Alfred S. McLaren. |
Author(s): | Serreze, Mark C. Barry, Roger G. McLaren, Alfred S. |
Date: | 1990. |
In: | CRREL Monograph. (1990.), Vol. 90-1 (1990) |
Abstract: | In response to synoptic-scale wind forcings clockwise circulation breaks down for at least 30 d in late summer to early autumn, and becomes anticlockwise. Reversal is associated with mean ice divergences exceeding 0.5% per day. Open-water areas produced may have climatic and oceanographic implications. |
Notes: | CRREL Monograph. Vol. 90-1 :185-188 (1990). |
Keywords: | 551.32 -- Glaciology. 551.326 -- Floating ice. 551.326.7 -- Sea ice. 551.326.14 -- Floating ice, movement. E6 -- Glaciology: floating ice. (*60) -- Arctic Ocean and adjacent waters. (*62) -- Canadian Arctic waters. (*628) -- Beaufort Sea. |
SPRI record no.: | 103491 |
LDR 01327naa#a2200000#a#4500 001 SPRI-103491 005 20240419095146.0 007 ta 008 240419s1990####xx#b##|##|###|0||#0|eng#d 035 ## ‡aSPRI-103491 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aSerreze, Mark C. 245 10 ‡aReversals of Beaufort gyre sea ice circulation and effects on ice concentration in the Canada Basin /‡cMark C. Serreze, Roger G. Barry, Alfred S. McLaren. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1990. 300 ## ‡ap. 185-188 :‡bmaps. 500 ## ‡aCRREL Monograph. Vol. 90-1 :185-188 (1990). 520 3# ‡aIn response to synoptic-scale wind forcings clockwise circulation breaks down for at least 30 d in late summer to early autumn, and becomes anticlockwise. Reversal is associated with mean ice divergences exceeding 0.5% per day. Open-water areas produced may have climatic and oceanographic implications. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.326 -- Floating ice.‡2udc 650 07 ‡a551.326.7 -- Sea ice.‡2udc 650 07 ‡a551.326.14 -- Floating ice, movement.‡2udc 650 07 ‡aE6 -- Glaciology: floating ice.‡2local 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 651 #7 ‡a(*62) -- Canadian Arctic waters.‡2udc 651 #7 ‡a(*628) -- Beaufort Sea.‡2udc 700 1# ‡aBarry, Roger G. 700 1# ‡aMcLaren, Alfred S. 773 0# ‡7nnas ‡tCRREL Monograph. ‡gVol. 90-1 (1990) ‡wSPRI-64222 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240419