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Record #97710:
Relations between top and bottom ice topography using a scanning sonar / Ånund Sigurd Johnsen.
Title: | Relations between top and bottom ice topography using a scanning sonar / Ånund Sigurd Johnsen. |
Author(s): | Johnsen, Ånund Sigurd. |
Date: | 1989. |
Publisher: | Luleå: Tekniska Högskolan i Luleå |
In: | POAC 89 : the 10th International Conference on Port and Ocean Engineering under Arctic Conditions. June 12-16 1989, Luleå, Sweden [Vols. 1 & 2]. (1989.), Vol.1. |
Abstract: | Ten ice floes in Barents Sea were mapped. All were in marginal ice zone <90 km from ice edge. Correlation between freeboard and ice thickness was studied. Previous observations of level ice yielded correlation coefficients of 0.8. Present measurements gave values of 0.7 for multiyear, partly deformed ice and 0.5 for first-year, very deformed ice. Differences may be due to effects of thermodynamic processes, isostatic relaxation and deformation processes. |
Notes: | In: POAC 89 : the 10th International Conference on Port and Ocean Engineering under Arctic Conditions. June 12-16 1989, Luleå, Sweden [Vols. 1 & 2]. Vol.1. / Kennet B.E. Axelsson, Lennart Å. Fransson, eds. |
Keywords: | 551.32 -- Glaciology. 551.326 -- Floating ice. 551.326.3 -- Floating ice, structure and surface features. E6 -- Glaciology: floating ice. (*60) -- Arctic Ocean and adjacent waters. (*686) -- Barents Sea. |
SPRI record no.: | 97710 |
LDR 01716naa#a2200000#a#4500 001 SPRI-97710 005 20240419024655.0 007 ta 008 240419s1989####sw#ab##|#####|0||#0#eng#d 035 ## ‡aSPRI-97710 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aJohnsen, Ånund Sigurd. 245 10 ‡aRelations between top and bottom ice topography using a scanning sonar /‡cÅnund Sigurd Johnsen. 260 ## ‡aLuleå :‡bTekniska Högskolan i Luleå,‡c1989. 300 ## ‡ap. 77-86 :‡bdiags., table, map. 500 ## ‡aIn: POAC 89 : the 10th International Conference on Port and Ocean Engineering under Arctic Conditions. June 12-16 1989, Luleå, Sweden [Vols. 1 & 2]. Vol.1. / Kennet B.E. Axelsson, Lennart Å. Fransson, eds. 520 3# ‡aTen ice floes in Barents Sea were mapped. All were in marginal ice zone <90 km from ice edge. Correlation between freeboard and ice thickness was studied. Previous observations of level ice yielded correlation coefficients of 0.8. Present measurements gave values of 0.7 for multiyear, partly deformed ice and 0.5 for first-year, very deformed ice. Differences may be due to effects of thermodynamic processes, isostatic relaxation and deformation processes. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.326 -- Floating ice.‡2udc 650 07 ‡a551.326.3 -- Floating ice, structure and surface features.‡2udc 650 07 ‡aE6 -- Glaciology: floating ice.‡2local 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 651 #7 ‡a(*686) -- Barents Sea.‡2udc 773 0# ‡7nnam ‡aKennet B.E. Axelsson, Lennart Å. Fransson, eds. ‡tPOAC 89 : the 10th International Conference on Port and Ocean Engineering under Arctic Conditions. June 12-16 1989, Luleå, Sweden [Vols. 1 & 2]. ‡dLuleå : Tekniska Högskolan i Luleå, 1989. ‡gVol.1. ‡wSPRI-97704 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240419