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Record #103828:
Quantitative approximation of mountain glacial climates / William W. Locke.
Title: | Quantitative approximation of mountain glacial climates / William W. Locke. |
Author(s): | Locke, William W. |
Date: | 1990. |
In: | Annals of Glaciology. (1990.), Vol. 14 (1990) |
Abstract: | Winter precipitation at equilibrium line altitude of wide selection of modern mountain glaciers is well explained by multiple regression using summer temperature and logarithm of continentality (distance from moisture source) as independent variables. Continentality serves as proxy for inland decreases in energy input through longwave radiation and condensation and increasing energy losses through evaporation and sublimation. Winter precipitation in presently inaccessible areas and former precipitation across broad regions can thus be estimated accurately from two simple variables. |
Notes: | Annals of Glaciology. Vol. 14 :164-167 (1990). |
Keywords: | 551.582 -- Climatology of particular places. 551.588.5 -- Climate, relationship with ice. E10 -- Glaciology: snow and avalanches. |
SPRI record no.: | 103828 |
LDR 01318naa#a2200000#a#4500 001 SPRI-103828 005 20230927114314.0 007 ta 008 230927s1990####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-103828 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aLocke, William W. 245 10 ‡aQuantitative approximation of mountain glacial climates /‡cWilliam W. Locke. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1990. 300 ## ‡ap. 164-167 :‡bdiag., tables. 500 ## ‡aAnnals of Glaciology. Vol. 14 :164-167 (1990). 520 3# ‡aWinter precipitation at equilibrium line altitude of wide selection of modern mountain glaciers is well explained by multiple regression using summer temperature and logarithm of continentality (distance from moisture source) as independent variables. Continentality serves as proxy for inland decreases in energy input through longwave radiation and condensation and increasing energy losses through evaporation and sublimation. Winter precipitation in presently inaccessible areas and former precipitation across broad regions can thus be estimated accurately from two simple variables. 650 07 ‡a551.582 -- Climatology of particular places.‡2udc 650 07 ‡a551.588.5 -- Climate, relationship with ice.‡2udc 650 07 ‡aE10 -- Glaciology: snow and avalanches.‡2local 773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 14 (1990) ‡wSPRI-60773 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230927