skip to primary navigation skip to content
 

 

You are not currently logged in

SPRI library catalogue

View 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 It is no longer being updated, so does not reliably reflect our current library holdings.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:

Spring 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

MARCXML

LDR 01504nam#a2200000#a#4500
001 SPRI-101257
005 20221006033101.0
007 ta
008 221006s1989####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# ‡a20221006