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Record #117275:
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MARC recordTheoretical heights of buoyant convection above open leads in the winter Arctic pack ice cover / Mark C. Serreze, James A. Maslanik, Mark C. Rehder, Russell C. Schnell, Jonathan D. Kahl, Edgar L. Andreas.
| Title: | Theoretical heights of buoyant convection above open leads in the winter Arctic pack ice cover / Mark C. Serreze, James A. Maslanik, Mark C. Rehder, Russell C. Schnell, Jonathan D. Kahl, Edgar L. Andreas. |
| Author(s): | Serreze, Mark C. Maslanik, James A. Rehder, Mark C. Schnell, Russell C. Kahl, Jonathan D. Andreas, Edgar L. |
| Date: | 1992. |
| In: | Journal of Geophysical Research. (1992.), Vol. 97(C6) (1992) |
| Abstract: | Plumes of ice crystals and condensate have been observed rising from open leads in Arctic sea ice. Fetch-dependent boundary-layer model is used to examine how predicted height of buoyant convection varies with lead width, vertical temperature structure, winds, cloud cover, and other variables. |
| Notes: | Journal of Geophysical Research. Vol. 97(C6) :9411-9422 (1992). |
| Keywords: | 551.32 -- Glaciology. 551.326 -- Floating ice. 551.326.7 -- Sea ice. 551.326.3 -- Floating ice, structure and surface features. 551.5 -- Meteorology. 551.51 -- Atmosphere. Structure, mechanics and thermodynamics. 519.673 -- Modelling. E6 -- Glaciology: floating ice. (*60) -- Arctic Ocean and adjacent waters. |
| SPRI record no.: | 117275 |
LDR 01591naa#a2200000#a#4500 001 SPRI-117275 005 20240418163031.0 007 ta 008 240418s1992####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-117275 040 ## ‡aUkCU-P‡beng‡eaacr 245 00 ‡aTheoretical heights of buoyant convection above open leads in the winter Arctic pack ice cover /‡cMark C. Serreze, James A. Maslanik, Mark C. Rehder, Russell C. Schnell, Jonathan D. Kahl, Edgar L. Andreas. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1992. 300 ## ‡ap. 9411-9422 :‡bdiags., table, map. 500 ## ‡aJournal of Geophysical Research. Vol. 97(C6) :9411-9422 (1992). 520 3# ‡aPlumes of ice crystals and condensate have been observed rising from open leads in Arctic sea ice. Fetch-dependent boundary-layer model is used to examine how predicted height of buoyant convection varies with lead width, vertical temperature structure, winds, cloud cover, and other variables. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.326 -- Floating ice.‡2udc 650 07 ‡a551.326.7 -- Sea ice.‡2udc 650 07 ‡a551.326.3 -- Floating ice, structure and surface features.‡2udc 650 07 ‡a551.5 -- Meteorology.‡2udc 650 07 ‡a551.51 -- Atmosphere. Structure, mechanics and thermodynamics.‡2udc 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡aE6 -- Glaciology: floating ice.‡2local 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 700 1# ‡aSerreze, Mark C. 700 1# ‡aMaslanik, James A. 700 1# ‡aRehder, Mark C. 700 1# ‡aSchnell, Russell C. 700 1# ‡aKahl, Jonathan D. 700 1# ‡aAndreas, Edgar L. 773 0# ‡7nnas ‡tJournal of Geophysical Research. ‡gVol. 97(C6) (1992) ‡wSPRI-35252 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240418