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Record #112299:
Meteorological triggers for deep convection in the Greenland Sea / P.S. Guest, K.L. Davidson.
Title: | Meteorological triggers for deep convection in the Greenland Sea / P.S. Guest, K.L. Davidson. |
Author(s): | Guest, P. S. Davidson, K. L. |
Date: | 1991. |
Publisher: | Amsterdam: Elsevier |
In: | Deep convection and deep water formation in the oceans. Proceedings of the International Monterey Colloquium on Deep Convection and Deep Water Formation in the Oceans. (1991.), |
Abstract: | Examines types of meteorological phenomena capable of triggering deep convection. In particular, postulates that favourable condition for deep convection within marginal ice zone (MIZ) occurs when direction of cold, strong, off-ice wind is at angle of less than 45° from ice edge, with edge to right looking downwind. |
Notes: | In: Deep convection and deep water formation in the oceans. Proceedings of the International Monterey Colloquium on Deep Convection and Deep Water Formation in the Oceans / P.C. Chu, J.C. Gascard, eds. |
Keywords: | 551.46 -- Oceanography, physical. 551.465 -- Oceanography, dynamics. 551.465.4 -- Oceanography, stratification. 551.465.46 -- Upwelling. 551.5 -- Meteorology. 551.556 -- Wind, effects of. 551.326 -- Floating ice. C -- Oceanography, hydrography and hydrology. (*60) -- Arctic Ocean and adjacent waters. (*61) -- North Atlantic Ocean. (*617) -- Greenland Sea and Fram Strait. |
SPRI record no.: | 112299 |
LDR 01790naa#a2200000#a#4500 001 SPRI-112299 005 20230330021926.0 007 ta 008 230330s1991####ne#ab##|#####|0||#0#eng#d 035 ## ‡aSPRI-112299 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aGuest, P. S. 245 10 ‡aMeteorological triggers for deep convection in the Greenland Sea /‡cP.S. Guest, K.L. Davidson. 260 ## ‡aAmsterdam :‡bElsevier,‡c1991. 300 ## ‡ap. 369-375 :‡bdiag., maps. 500 ## ‡aIn: Deep convection and deep water formation in the oceans. Proceedings of the International Monterey Colloquium on Deep Convection and Deep Water Formation in the Oceans / P.C. Chu, J.C. Gascard, eds. 520 3# ‡aExamines types of meteorological phenomena capable of triggering deep convection. In particular, postulates that favourable condition for deep convection within marginal ice zone (MIZ) occurs when direction of cold, strong, off-ice wind is at angle of less than 45° from ice edge, with edge to right looking downwind. 650 07 ‡a551.46 -- Oceanography, physical.‡2udc 650 07 ‡a551.465 -- Oceanography, dynamics.‡2udc 650 07 ‡a551.465.4 -- Oceanography, stratification.‡2udc 650 07 ‡a551.465.46 -- Upwelling.‡2udc 650 07 ‡a551.5 -- Meteorology.‡2udc 650 07 ‡a551.556 -- Wind, effects of.‡2udc 650 07 ‡a551.326 -- Floating ice.‡2udc 650 07 ‡aC -- Oceanography, hydrography and hydrology.‡2local 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 651 #7 ‡a(*61) -- North Atlantic Ocean.‡2udc 651 #7 ‡a(*617) -- Greenland Sea and Fram Strait.‡2udc 700 1# ‡aDavidson, K. L. 773 0# ‡7nnam ‡aP.C. Chu, J.C. Gascard, eds. ‡tDeep convection and deep water formation in the oceans. Proceedings of the International Monterey Colloquium on Deep Convection and Deep Water Formation in the Oceans. ‡dAmsterdam : Elsevier, 1991. ‡wSPRI-112291 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230330