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Record #104692:
- #104692
Main publication details
MARC recordOne hundred years of Arctic ice cover variations as simulated by one-dimensional, ice-ocean model / S. Häkkinen, G.L. Mellor.
| Title: | One hundred years of Arctic ice cover variations as simulated by one-dimensional, ice-ocean model / S. Häkkinen, G.L. Mellor. |
| Author(s): | Häkkinen, S. Mellor, G. L. |
| Date: | 1990. |
| In: | Journal of Geophysical Research. (1990.), Vol. 95(C9) (1990) |
| Abstract: | Main aim was to investigate behaviour of ice/upper ocean system on climatic time scales, especially asymmetry of freezing and melting seasons. Coupled model was applied to period 1880-1985, using published surface air-temperature fluctuations. Analysis shows that variability in summer melt determines variability in average ice thickness. Annual oceanic heat flux from deep ocean and maximum freezing rate and associated nearly constant minimum surface salinity flux did not vary significantly interannually. This implies that oceanic influence on Arctic ice mass is minimal for range of atmospheric variables tested. |
| Notes: | Journal of Geophysical Research. Vol. 95(C9) :15, 959-15, 969 (1990). |
| Keywords: | 519.673 -- Modelling. 551.32 -- Glaciology. 551.326 -- Floating ice. 551.326.7 -- Sea ice. 551.326.2 -- Floating ice, formation and decay. E6 -- Glaciology: floating ice. (*60) -- Arctic Ocean and adjacent waters. |
| SPRI record no.: | 104692 |
LDR 01594naa#a2200000#a#4500 001 SPRI-104692 005 20231130040123.0 007 ta 008 231130s1990####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-104692 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aHäkkinen, S. 245 10 ‡aOne hundred years of Arctic ice cover variations as simulated by one-dimensional, ice-ocean model /‡cS. Häkkinen, G.L. Mellor. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1990. 300 ## ‡ap. 15, 959-15, 969 :‡bdiags. 500 ## ‡aJournal of Geophysical Research. Vol. 95(C9) :15, 959-15, 969 (1990). 520 3# ‡aMain aim was to investigate behaviour of ice/upper ocean system on climatic time scales, especially asymmetry of freezing and melting seasons. Coupled model was applied to period 1880-1985, using published surface air-temperature fluctuations. Analysis shows that variability in summer melt determines variability in average ice thickness. Annual oceanic heat flux from deep ocean and maximum freezing rate and associated nearly constant minimum surface salinity flux did not vary significantly interannually. This implies that oceanic influence on Arctic ice mass is minimal for range of atmospheric variables tested. 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.326 -- Floating ice.‡2udc 650 07 ‡a551.326.7 -- Sea ice.‡2udc 650 07 ‡a551.326.2 -- Floating ice, formation and decay.‡2udc 650 07 ‡aE6 -- Glaciology: floating ice.‡2local 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 700 1# ‡aMellor, G. L. 773 0# ‡7nnas ‡tJournal of Geophysical Research. ‡gVol. 95(C9) (1990) ‡wSPRI-35252 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231130