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Record #110828:
- #110828
Main publication details
MARC recordObservations of short-period ice floe accelerations during leg II of the Polarbjørn drift / Seelye Martin, Robert Drucker.
| Title: | Observations of short-period ice floe accelerations during leg II of the Polarbjørn drift / Seelye Martin, Robert Drucker. |
| Author(s): | Martin, Seelye. Drucker, Robert. |
| Date: | 1991. |
| In: | Journal of Geophysical Research. (1991.), Vol. 96(C6) (1991) |
| Abstract: | Describes participation in winter drift phase of Coordinated Eastern Arctic Experiment (CEAREX) during October-December 1988, when ship was frozen into sea ice north and east of Svalbard. Measurements of ice accelerations associated with deformation and breakup showed transition in ice surrounding ship from large floes (1 to 10 km) to small, broken floes (10 to 100 m) between days 310 and 329. Deformation and fracture generated significant accelerations which were associated with ice shear, ridging, and ice-floe collisions. |
| Notes: | Journal of Geophysical Research. Vol. 96(C6) :10, 567-10, 580 (1991). |
| Keywords: | 551.32 -- Glaciology. 551.326 -- Floating ice. 551.326.7 -- Sea ice. 551.326.14 -- Floating ice, movement. 551.326.2 -- Floating ice, formation and decay. E6 -- Glaciology: floating ice. |
| SPRI record no.: | 110828 |
LDR 01481naa#a2200000#a#4500 001 SPRI-110828 005 20230329230653.0 007 ta 008 230329s1991####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-110828 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aMartin, Seelye. 245 10 ‡aObservations of short-period ice floe accelerations during leg II of the Polarbjørn drift /‡cSeelye Martin, Robert Drucker. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1991. 300 ## ‡ap. 10, 567-10, 580 :‡bdiags., table, maps. 500 ## ‡aJournal of Geophysical Research. Vol. 96(C6) :10, 567-10, 580 (1991). 520 3# ‡aDescribes participation in winter drift phase of Coordinated Eastern Arctic Experiment (CEAREX) during October-December 1988, when ship was frozen into sea ice north and east of Svalbard. Measurements of ice accelerations associated with deformation and breakup showed transition in ice surrounding ship from large floes (1 to 10 km) to small, broken floes (10 to 100 m) between days 310 and 329. Deformation and fracture generated significant accelerations which were associated with ice shear, ridging, and ice-floe collisions. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.326 -- Floating ice.‡2udc 650 07 ‡a551.326.7 -- Sea ice.‡2udc 650 07 ‡a551.326.14 -- Floating ice, movement.‡2udc 650 07 ‡a551.326.2 -- Floating ice, formation and decay.‡2udc 650 07 ‡aE6 -- Glaciology: floating ice.‡2local 700 1# ‡aDrucker, Robert. 773 0# ‡7nnas ‡tJournal of Geophysical Research. ‡gVol. 96(C6) (1991) ‡wSPRI-35252 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230329