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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

MARCXML

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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# ‡a20240419