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Record #180903:
- #180903
Main publication details
MARC recordSources of sediment found in sea ice from the western Arctic Ocean: new insights into processes of entrainment and drift patterns / Dennis A. Darby.
| Title: | Sources of sediment found in sea ice from the western Arctic Ocean: new insights into processes of entrainment and drift patterns / Dennis A. Darby. |
| Author(s): | Darby, Dennis A. |
| Date: | 2003. |
| In: | Journal of Geophysical Research. (2003.), Vol. 108(C8) (2003) |
| Abstract: | Reports use of geochemical fingerprint of entrained Fe oxide mineral grains in Arctic Ocean sea ice to determine precise sources of sediment. Drift paths confirmed by this method confirm that North American side of Arctic Ocean is dominated by sea ice floes drifting west with Beaufort Gyre. Postulates Siberian shelf (Laptev Sea) origin for floes containing significant Russian/Banks Island grains. |
| Notes: | Journal of Geophysical Research. Vol. 108(C8) :13.1-13.10 (2003). |
| Keywords: | 550.4 -- Geochemistry. 551.326.7 -- Sea ice. 551.326.14 -- Floating ice, movement. 551.35 -- Marine sediments. 551.46 -- Oceanography, physical. 551.462.32 -- Continental shelves. 551.465 -- Oceanography, dynamics. 551.465.7 -- Oceanography, energy budget. C -- Oceanography, hydrography and hydrology. (*3) -- Arctic regions. (*60) -- Arctic Ocean and adjacent waters. (*628) -- Beaufort Sea. (*684) -- Laptev Sea. |
| SPRI record no.: | 180903 |
LDR 01810naa#a2200000#a#4500 001 SPRI-180903 005 20240416111040.0 007 ta 008 240416s2003####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-180903 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aDarby, Dennis A. 245 10 ‡aSources of sediment found in sea ice from the western Arctic Ocean :‡bnew insights into processes of entrainment and drift patterns /‡cDennis A. Darby. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2003. 300 ## ‡ap. 13.1-13.10 :‡bill., diags., tables, map. 500 ## ‡aJournal of Geophysical Research. Vol. 108(C8) :13.1-13.10 (2003). 520 3# ‡aReports use of geochemical fingerprint of entrained Fe oxide mineral grains in Arctic Ocean sea ice to determine precise sources of sediment. Drift paths confirmed by this method confirm that North American side of Arctic Ocean is dominated by sea ice floes drifting west with Beaufort Gyre. Postulates Siberian shelf (Laptev Sea) origin for floes containing significant Russian/Banks Island grains. 530 ## ‡aAlso issued online ‡uurn:doi:10.1029/2002JC001350‡uhttps://dx.doi.org/10.1029/2002JC001350 650 07 ‡a550.4 -- Geochemistry.‡2udc 650 07 ‡a551.326.7 -- Sea ice.‡2udc 650 07 ‡a551.326.14 -- Floating ice, movement.‡2udc 650 07 ‡a551.35 -- Marine sediments.‡2udc 650 07 ‡a551.46 -- Oceanography, physical.‡2udc 650 07 ‡a551.462.32 -- Continental shelves.‡2udc 650 07 ‡a551.465 -- Oceanography, dynamics.‡2udc 650 07 ‡a551.465.7 -- Oceanography, energy budget.‡2udc 650 07 ‡aC -- Oceanography, hydrography and hydrology.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 651 #7 ‡a(*628) -- Beaufort Sea.‡2udc 651 #7 ‡a(*684) -- Laptev Sea.‡2udc 773 0# ‡7nnas ‡tJournal of Geophysical Research. ‡gVol. 108(C8) (2003) ‡wSPRI-35252 916 ## ‡a2007/11/21 -- JW 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240416 ‡bJW