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Record #110279:

Changes in ice-cover thickness and lake level of Lake Hoare, Antarctica: implications for climatic change / R.A. Wharton, C.P. McKay, Gary D. Clow, D.T. Andersen.

Title: Changes in ice-cover thickness and lake level of Lake Hoare, Antarctica: implications for climatic change / R.A. Wharton, C.P. McKay, Gary D. Clow, D.T. Andersen.
Author(s): Wharton, R. A.
McKay, C. P.
Clow, Gary D.
Andersen, D. T.
Date: 1991.
In: Eos : transactions, American Geophysical Union. (1991.), Vol. 72(17 (Supplement)) (1991)
Abstract: Presents results from 10 a of measurements made at this lake in south Victoria Land. Ice has been thinning at rate of >20 cm a⁻¹ for past decade, but seems to have stabilized recently at thickness of 3.3 m. Evidence suggests that peak summer temperatures have been <0°C for progressively longer period each year since 1972. Most plausible climate change capable of explaining thinning of ice is change in mean annual temperature of 2°C. Also considers changes in mechanism of mass loss from surface.
Notes:

Eos : transactions, American Geophysical Union. Vol. 72(17 (Supplement)) :109 (1991).

American Geophysical Union-Mineralogical Society of America 1991 Spring Meeting. Abstract volume.

Keywords: 551.32 -- Glaciology.
551.326.85 -- Lake ice.
551.326 -- Floating ice.
551.583 -- Climatic changes.
551.58 -- Climatology.
E6 -- Glaciology: floating ice.
(*7) -- Antarctic regions.
(*762.4) -- Scott Coast.
SPRI record no.: 110279

MARCXML

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035 ## ‡aSPRI-110279
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245 00 ‡aChanges in ice-cover thickness and lake level of Lake Hoare, Antarctica :‡bimplications for climatic change /‡cR.A. Wharton, C.P. McKay, Gary D. Clow, D.T. Andersen.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1991.
300 ## ‡ap. 109.
500 ## ‡aEos : transactions, American Geophysical Union. Vol. 72(17 (Supplement)) :109 (1991).
500 ## ‡aAmerican Geophysical Union-Mineralogical Society of America 1991 Spring Meeting. Abstract volume.
520 3# ‡aPresents results from 10 a of measurements made at this lake in south Victoria Land. Ice has been thinning at rate of >20 cm a⁻¹ for past decade, but seems to have stabilized recently at thickness of 3.3 m. Evidence suggests that peak summer temperatures have been <0°C for progressively longer period each year since 1972. Most plausible climate change capable of explaining thinning of ice is change in mean annual temperature of 2°C. Also considers changes in mechanism of mass loss from surface.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.326.85 -- Lake ice.‡2udc
650 07 ‡a551.326 -- Floating ice.‡2udc
650 07 ‡a551.583 -- Climatic changes.‡2udc
650 07 ‡a551.58 -- Climatology.‡2udc
650 07 ‡aE6 -- Glaciology: floating ice.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*762.4) -- Scott Coast.‡2udc
700 1# ‡aWharton, R. A.
700 1# ‡aMcKay, C. P.
700 1# ‡aClow, Gary D.
700 1# ‡aAndersen, D. T.
773 0# ‡7nnas ‡tEos : transactions, American Geophysical Union. ‡gVol. 72(17 (Supplement)) (1991) ‡wSPRI-1028
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20230326