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Record #115103:

The role of sea ice in the simulated winter climate / C. Senior.

Title: The role of sea ice in the simulated winter climate / C. Senior.
Author(s): Senior, C.
Date: 1991.
Publisher: Luxembourg: Commission of the European Communities
Abstract: Modelling experiments suggest that removal of Antarctic sea ice produces reduction in surface pressure over area of largest change in sea-ice extent. Thermal forcing due to increase in turbulent heating is likely to be exaggerated in model as constant depth of 2 m is used for all sea-ice points, whereas it is much thinner and contains substantial open water. These factors must be considered in models used to determine effect of sea-ice anomalies.
Notes:

Offprint: Climatic change and impacts: a general introduction. Proceedings of the European School of Climatology and Natural Hazards Course, held in Florence from 11 to 18 September 1988 / R. Fantechi, G. Maracchi, M.E. Almeida-Teixeira, eds.

Keywords: 551.326.7 -- Sea ice.
551.58 -- Climatology.
551.588 -- Climate, effect of man and environment.
551.588.5 -- Climate, relationship with ice.
519.673 -- Modelling.
.000(410) -- British author.
E6 -- Glaciology: floating ice.
(*80) -- Southern Ocean.
(*7) -- Antarctic regions.
Location(s): SCO: SPRI-PAM: 551.588.5
SPRI record no.: 115103

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100 1# ‡aSenior, C.
245 14 ‡aThe role of sea ice in the simulated winter climate /‡cC. Senior.
260 ## ‡aLuxembourg :‡bCommission of the European Communities,‡c1991.
300 ## ‡ap. 445-447 :‡bdiags.
490 0# ‡aEUR 11943 EN
500 ## ‡aOffprint: Climatic change and impacts: a general introduction. Proceedings of the European School of Climatology and Natural Hazards Course, held in Florence from 11 to 18 September 1988 / R. Fantechi, G. Maracchi, M.E. Almeida-Teixeira, eds.
520 3# ‡aModelling experiments suggest that removal of Antarctic sea ice produces reduction in surface pressure over area of largest change in sea-ice extent. Thermal forcing due to increase in turbulent heating is likely to be exaggerated in model as constant depth of 2 m is used for all sea-ice points, whereas it is much thinner and contains substantial open water. These factors must be considered in models used to determine effect of sea-ice anomalies.
650 07 ‡a551.326.7 -- Sea ice.‡2udc
650 07 ‡a551.58 -- Climatology.‡2udc
650 07 ‡a551.588 -- Climate, effect of man and environment.‡2udc
650 07 ‡a551.588.5 -- Climate, relationship with ice.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡a.000(410) -- British author.‡2udc
650 07 ‡aE6 -- Glaciology: floating ice.‡2local
651 #7 ‡a(*80) -- Southern Ocean.‡2udc
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
852 7# ‡2camdept‡bSCO‡cSPRI-PAM‡h551.588.5‡9Create 1 item record‡0Migrate
917 ## ‡aUnenhanced record from Muscat, imported 2019
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