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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 |
LDR 01644nam#a2200000#a#4500 001 SPRI-115103 005 20240328181054.0 007 ta 008 240328s1991####lu#a###|#####|0||#0#eng#d 035 ## ‡aSPRI-115103 040 ## ‡aUkCU-P‡beng‡eaacr 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 948 3# ‡a20240328