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Record #185812:
Antarctic glacier thinning, 1992-2003 / Andrew Shepherd, Duncan J. Wingham.
Title: | Antarctic glacier thinning, 1992-2003 / Andrew Shepherd, Duncan J. Wingham. |
Author(s): | Shepherd, Andrew. Wingham, Duncan J. |
Date: | 2008. |
In: | Scottish Geographical Journal. (2008.), Vol. 124(2-3) (2008) |
Abstract: | Analyses elevation changes of entire Antarctic Ice Sheet to determine decadal trends in mass of principal outlet glaciers, and compares pattern of imbalance to characteristics of ice sheet geometry in order to isolate factors common to all currently retreating sectors. Results indicate that only glaciers in both East and West Antarctica seated in submarine basins with no substantial ice shelf barrier are losing mass today. Their susceptibility to changes in climate may mean that they provide substantial contribution to global sea levels over 21st century should ocean warming continue as projected. |
Notes: | Scottish Geographical Journal. Vol. 124(2-3) :154-164 (2008). |
Keywords: | 551.32 -- Glaciology. 551.324 -- Land ice. 551.324.43 -- Land ice, regime and mass balance. 551.324.63 -- Land ice, advance and retreat. 551.461.2 -- Sea level, fluctuations. .000(410) -- British author. E5 -- Glaciology: land ice. (*7) -- Antarctic regions. (*7.3) -- East Antarctica. (*7.7) -- West Antarctica. |
SPRI record no.: | 185812 |
LDR 01813naa#a2200000#a#4500 001 SPRI-185812 005 20230928052255.0 007 ta 008 230928s2008####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-185812 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aShepherd, Andrew. 245 10 ‡aAntarctic glacier thinning, 1992-2003 /‡cAndrew Shepherd, Duncan J. Wingham. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2008. 300 ## ‡ap. 154-164 :‡bill., diags., tables, map. 500 ## ‡aScottish Geographical Journal. Vol. 124(2-3) :154-164 (2008). 520 3# ‡aAnalyses elevation changes of entire Antarctic Ice Sheet to determine decadal trends in mass of principal outlet glaciers, and compares pattern of imbalance to characteristics of ice sheet geometry in order to isolate factors common to all currently retreating sectors. Results indicate that only glaciers in both East and West Antarctica seated in submarine basins with no substantial ice shelf barrier are losing mass today. Their susceptibility to changes in climate may mean that they provide substantial contribution to global sea levels over 21st century should ocean warming continue as projected. 530 ## ‡aAlso issued online ‡uurn:doi:10.1080/14702540802441144‡uhttps://dx.doi.org/10.1080/14702540802441144 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.43 -- Land ice, regime and mass balance.‡2udc 650 07 ‡a551.324.63 -- Land ice, advance and retreat.‡2udc 650 07 ‡a551.461.2 -- Sea level, fluctuations.‡2udc 650 07 ‡a.000(410) -- British author.‡2udc 650 07 ‡aE5 -- Glaciology: land ice.‡2local 651 #7 ‡a(*7) -- Antarctic regions.‡2udc 651 #7 ‡a(*7.3) -- East Antarctica.‡2udc 651 #7 ‡a(*7.7) -- West Antarctica.‡2udc 700 1# ‡aWingham, Duncan J. 773 0# ‡7nnas ‡tScottish Geographical Journal. ‡gVol. 124(2-3) (2008) ‡wSPRI-150833 916 ## ‡aHS 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230928 ‡bHS