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Record #112507:
- #112507
Main publication details
MARC recordTextural characteristics of sea ice and the major mechanisms of ice growth in the Weddell Sea / Manfred A. Lange, Hajo Eicken.
| Title: | Textural characteristics of sea ice and the major mechanisms of ice growth in the Weddell Sea / Manfred A. Lange, Hajo Eicken. |
| Author(s): | Lange, Manfred A. Eicken, Hajo. |
| Date: | 1991. |
| In: | Annals of Glaciology. (1991.), Vol. 15 (1991) |
| Abstract: | Finds that Antarctic sea ice of all ages is dominated by granular ice of frazil origin, in contrast to Arctic ice, which consists predominantly of columnar ice of congelation origin. Large fraction of granular ice in first-year sea ice is result of dominant ice-formation process in advancing ice edge (pancake cycle). Dominance of granular over columnar ice in second- or multiyear ice is due to large degree of deformational activity in Southern Ocean. |
| Notes: | Annals of Glaciology. Vol. 15 :210-215 (1991). |
| Keywords: | 551.32 -- Glaciology. 551.326 -- Floating ice. 551.326.7 -- Sea ice. 551.326.3 -- Floating ice, structure and surface features. 551.326.2 -- Floating ice, formation and decay. 548 -- Crystallography. 536.421.4 -- Freezing. E6 -- Glaciology: floating ice. (*80) -- Southern Ocean. |
| SPRI record no.: | 112507 |
LDR 01498naa#a2200000#a#4500 001 SPRI-112507 005 20231208161426.0 007 ta 008 231208s1991####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-112507 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aLange, Manfred A. 245 10 ‡aTextural characteristics of sea ice and the major mechanisms of ice growth in the Weddell Sea /‡cManfred A. Lange, Hajo Eicken. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1991. 300 ## ‡ap. 210-215 :‡bdiags., tables, map. 500 ## ‡aAnnals of Glaciology. Vol. 15 :210-215 (1991). 520 3# ‡aFinds that Antarctic sea ice of all ages is dominated by granular ice of frazil origin, in contrast to Arctic ice, which consists predominantly of columnar ice of congelation origin. Large fraction of granular ice in first-year sea ice is result of dominant ice-formation process in advancing ice edge (pancake cycle). Dominance of granular over columnar ice in second- or multiyear ice is due to large degree of deformational activity in Southern Ocean. 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 ‡a551.326.2 -- Floating ice, formation and decay.‡2udc 650 07 ‡a548 -- Crystallography.‡2udc 650 07 ‡a536.421.4 -- Freezing.‡2udc 650 07 ‡aE6 -- Glaciology: floating ice.‡2local 651 #7 ‡a(*80) -- Southern Ocean.‡2udc 700 1# ‡aEicken, Hajo. 773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 15 (1991) ‡wSPRI-60773 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231208