Scott Polar Research InstituteSPRI library catalogue
Search the catalogue
Browse recordsView a record
Please note: You are viewing the legacy database of the Scott Polar Research Institute Library catalogue. It is no longer being updated, so does not reliably reflect our current library holdings.
Please search for material in iDiscover for up-to-date information about the library collection.
Record #101257:
- #101257
Main publication details
MARC recordSpring melt patterns in the Kara/Barents sea: 1984 / Robert G. Crane, Mark R. Anderson.
| Title: | Spring melt patterns in the Kara/Barents sea: 1984 / Robert G. Crane, Mark R. Anderson. |
| Author(s): | Crane, Robert G. Anderson, Mark R. |
| Date: | 1989. |
| Abstract: | Methodology based on extended principal components analysis is used to categorize spatial and temporal patterns of surface change that occur in seasonal sea-ice zone during spring/early summer. Demonstrated for Kara/Barents seas in spring 1984, using data from Nimbus-7 scanning multichannel microwave radiometer. Shows that conditions in Barents Sea are largely controlled by ice advection, while variance in Kara Sea is dominated by surface melt. |
| Notes: | Offprint: GeoJournal. Vol. 18(1) :25-33. |
| Keywords: | 551.326.7 -- Sea ice. 551.326.2 -- Floating ice, formation and decay. 551.326.12 -- Floating ice, distribution, seasonal. 629.783 -- Satellites. 53.087.23 -- Remote sensing. 551.32 -- Glaciology. E6 -- Glaciology: floating ice. (*60) -- Arctic Ocean and adjacent waters. (*685) -- Kara Sea. (*686) -- Barents Sea. |
| Location(s): | SCO: SPRI-SHF: 551.326.7 |
| SPRI record no.: | 101257 |
LDR 01504nam#a2200000#a#4500 001 SPRI-101257 005 20230929020612.0 007 ta 008 230929s1989####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-101257 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aCrane, Robert G. 245 10 ‡aSpring melt patterns in the Kara/Barents sea :‡b1984 /‡cRobert G. Crane, Mark R. Anderson. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1989. 300 ## ‡ap. 25-33 :‡bdiag., tables, maps. 500 ## ‡aOffprint: GeoJournal. Vol. 18(1) :25-33. 520 3# ‡aMethodology based on extended principal components analysis is used to categorize spatial and temporal patterns of surface change that occur in seasonal sea-ice zone during spring/early summer. Demonstrated for Kara/Barents seas in spring 1984, using data from Nimbus-7 scanning multichannel microwave radiometer. Shows that conditions in Barents Sea are largely controlled by ice advection, while variance in Kara Sea is dominated by surface melt. 650 07 ‡a551.326.7 -- Sea ice.‡2udc 650 07 ‡a551.326.2 -- Floating ice, formation and decay.‡2udc 650 07 ‡a551.326.12 -- Floating ice, distribution, seasonal.‡2udc 650 07 ‡a629.783 -- Satellites.‡2udc 650 07 ‡a53.087.23 -- Remote sensing.‡2udc 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡aE6 -- Glaciology: floating ice.‡2local 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 651 #7 ‡a(*685) -- Kara Sea.‡2udc 651 #7 ‡a(*686) -- Barents Sea.‡2udc 700 1# ‡aAnderson, Mark R. 852 7# ‡2camdept‡bSCO‡cSPRI-SHF‡h551.326.7‡9Create 1 item record‡0Migrate 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230929