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Record #110177:
Evidence for stability enhancement of sea ice in the Greenland and Labrador seas / R.F. Marsden, Lawrence A. Mysak, R.A. Myers.
Title: | Evidence for stability enhancement of sea ice in the Greenland and Labrador seas / R.F. Marsden, Lawrence A. Mysak, R.A. Myers. |
Author(s): | Marsden, R. F. Mysak, Lawrence A. Myers, R. A. |
Date: | 1991. |
In: | Journal of Geophysical Research. (1991.), Vol. 96(C3) (1991) |
Abstract: | Summer salinities from three locations bordering Greenland and Iceland are examined and compared with colocated sea-ice concentrations. For period 1953-80, it is shown that lag correlations between surface salinity and sea-ice anomalies has common structure where salinity anomalies lead sea-ice anomalies. Correlation structure can be reproduced by simple statistical feedback model using nonstationary negative feedback coefficient to account for salinity forcing of ice anomalies. Data presented are all consistent with concept of stability enhancement of sea-ice formation. |
Notes: | Journal of Geophysical Research. Vol. 96(C3) :4783-4789 (1991). |
Keywords: | 551.326.7 -- Sea ice. 54 -- Chemistry. 551.326.2 -- Floating ice, formation and decay. 551.326 -- Floating ice. E6 -- Glaciology: floating ice. (*60) -- Arctic Ocean and adjacent waters. (*617) -- Greenland Sea and Fram Strait. (*616) -- Iceland waters. |
SPRI record no.: | 110177 |
LDR 01640naa#a2200000#a#4500 001 SPRI-110177 005 20230529041218.0 007 ta 008 230529s1991####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-110177 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aMarsden, R. F. 245 10 ‡aEvidence for stability enhancement of sea ice in the Greenland and Labrador seas /‡cR.F. Marsden, Lawrence A. Mysak, R.A. Myers. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1991. 300 ## ‡ap. 4783-4789 :‡bdiags., tables, map. 500 ## ‡aJournal of Geophysical Research. Vol. 96(C3) :4783-4789 (1991). 520 3# ‡aSummer salinities from three locations bordering Greenland and Iceland are examined and compared with colocated sea-ice concentrations. For period 1953-80, it is shown that lag correlations between surface salinity and sea-ice anomalies has common structure where salinity anomalies lead sea-ice anomalies. Correlation structure can be reproduced by simple statistical feedback model using nonstationary negative feedback coefficient to account for salinity forcing of ice anomalies. Data presented are all consistent with concept of stability enhancement of sea-ice formation. 650 07 ‡a551.326.7 -- Sea ice.‡2udc 650 07 ‡a54 -- Chemistry.‡2udc 650 07 ‡a551.326.2 -- Floating ice, formation and decay.‡2udc 650 07 ‡a551.326 -- Floating ice.‡2udc 650 07 ‡aE6 -- Glaciology: floating ice.‡2local 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 651 #7 ‡a(*617) -- Greenland Sea and Fram Strait.‡2udc 651 #7 ‡a(*616) -- Iceland waters.‡2udc 700 1# ‡aMysak, Lawrence A. 700 1# ‡aMyers, R. A. 773 0# ‡7nnas ‡tJournal of Geophysical Research. ‡gVol. 96(C3) (1991) ‡wSPRI-35252 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230529