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Record #112863:
Snow-accumulation variability from seasonal surface observations and firn-core stratigraphy, eastern Wilkes Land, Antarctica / Ian D. Goodwin.
Title: | Snow-accumulation variability from seasonal surface observations and firn-core stratigraphy, eastern Wilkes Land, Antarctica / Ian D. Goodwin. |
Author(s): | Goodwin, Ian D. |
Date: | 1991. |
In: | Journal of Glaciology. (1991.), Vol. 37(127) (1991) |
Abstract: | Annual accumulation records were derived from two firn cores drilled along 2000 m contour, separated by 750 km. Records, spanning 1930-85, show that annual accumulation has increased by 25% from 1960 to 1985, resulting in highest rates in 55-year records. Annual accumulation layers were identified in firn cores using firn-stratigraphic model together with seasonal oxygen-isotope ratios. Suggests that increase is result of changes in general atmospheric circulation pattern, which have produced higher annual frequency of precipitation events. |
Notes: | Journal of Glaciology. Vol. 37(127) :383-387 (1991). |
Keywords: | 551.578.46 -- Snow cover and snow patches. 551.324 -- Land ice. 551.324.24 -- Ice sheets and caps. E10 -- Glaciology: snow and avalanches. (*7) -- Antarctic regions. (*747) -- Wilkes Land. |
SPRI record no.: | 112863 |
LDR 01461naa#a2200000#a#4500 001 SPRI-112863 005 20230320085105.0 007 ta 008 230320s1991####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-112863 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aGoodwin, Ian D. 245 10 ‡aSnow-accumulation variability from seasonal surface observations and firn-core stratigraphy, eastern Wilkes Land, Antarctica /‡cIan D. Goodwin. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1991. 300 ## ‡ap. 383-387 :‡bdiags., tables, maps. 500 ## ‡aJournal of Glaciology. Vol. 37(127) :383-387 (1991). 520 3# ‡aAnnual accumulation records were derived from two firn cores drilled along 2000 m contour, separated by 750 km. Records, spanning 1930-85, show that annual accumulation has increased by 25% from 1960 to 1985, resulting in highest rates in 55-year records. Annual accumulation layers were identified in firn cores using firn-stratigraphic model together with seasonal oxygen-isotope ratios. Suggests that increase is result of changes in general atmospheric circulation pattern, which have produced higher annual frequency of precipitation events. 650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.24 -- Ice sheets and caps.‡2udc 650 07 ‡aE10 -- Glaciology: snow and avalanches.‡2local 651 #7 ‡a(*7) -- Antarctic regions.‡2udc 651 #7 ‡a(*747) -- Wilkes Land.‡2udc 773 0# ‡7nnas ‡tJournal of Glaciology. ‡gVol. 37(127) (1991) ‡wSPRI-20534 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230320