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Record #93724:
- #93724
Main publication details
MARC recordCoastal ice dynamics / William M. Sackinger.
| Title: | Coastal ice dynamics / William M. Sackinger. |
| Author(s): | Sackinger, William M. |
| Date: | 1988. |
| Publisher: | New York: American Society of Civil Engineers |
| In: | Arctic coastal processes and slope protection design : a state of the practice report prepared by the Technical Council on Cold Regions Engineering of the American Society of Engineers. (1988.), |
| Abstract: | Dominant force affecting ice motion is from tidal current, but in coastal regions of low tidal excursions, wind forces often play major role. Ice edge can retreat seaward, even in winter when driven by offshore winds. Moving pack ice will experience complex internal stresses and fracture patterns due to local nonuniformity of water drag and Coriolis effects. |
| Notes: | In: Arctic coastal processes and slope protection design : a state of the practice report prepared by the Technical Council on Cold Regions Engineering of the American Society of Engineers / Andrie T. Chen, Craig B. Leidersdorf, eds. |
| Keywords: | 551.32 -- Glaciology. 551.326 -- Floating ice. 551.326.14 -- Floating ice, movement. E6 -- Glaciology: floating ice. (*60) -- Arctic Ocean and adjacent waters. |
| SPRI record no.: | 93724 |
LDR 01661naa#a2200000#a#4500 001 SPRI-93724 005 20231203165108.0 007 ta 008 231203s1988####nyuab##|#####|0||#0#eng#d 035 ## ‡aSPRI-93724 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aSackinger, William M. 245 10 ‡aCoastal ice dynamics /‡cWilliam M. Sackinger. 260 ## ‡aNew York :‡bAmerican Society of Civil Engineers,‡c1988. 300 ## ‡ap. 63-84 :‡bill., diags., tables, maps. 490 0# ‡aTechnical Council on Cold Regions Engineering Monograph 500 ## ‡aIn: Arctic coastal processes and slope protection design : a state of the practice report prepared by the Technical Council on Cold Regions Engineering of the American Society of Engineers / Andrie T. Chen, Craig B. Leidersdorf, eds. 520 3# ‡aDominant force affecting ice motion is from tidal current, but in coastal regions of low tidal excursions, wind forces often play major role. Ice edge can retreat seaward, even in winter when driven by offshore winds. Moving pack ice will experience complex internal stresses and fracture patterns due to local nonuniformity of water drag and Coriolis effects. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.326 -- Floating ice.‡2udc 650 07 ‡a551.326.14 -- Floating ice, movement.‡2udc 650 07 ‡aE6 -- Glaciology: floating ice.‡2local 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 773 0# ‡7nnam ‡aAndrie T. Chen, Craig B. Leidersdorf, eds. ‡tArctic coastal processes and slope protection design : a state of the practice report prepared by the Technical Council on Cold Regions Engineering of the American Society of Engineers. ‡dNew York : American Society of Civil Engineers, 1988. ‡wSPRI-93803 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231203