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Record #202176:
A new approach to quantifying soil temperature responses to changing air temperature and snow cover / Michael C. Mackiewicz.
Title: | A new approach to quantifying soil temperature responses to changing air temperature and snow cover / Michael C. Mackiewicz. |
Author(s): | Mackiewicz, Michael C. |
Date: | 2012. |
In: | Polar Science. (2012.), Vol. 6(3-4) (2012) |
Abstract: | Reports use of multiple linear regression (MLR) with dummy predictor variables to quantify degree of dampening between air and shallow soil temperatures in presence and absence of snow cover at four sites in Greenland. Results obtained for sites indicated that, with snow cover, temperature of shallow soils changed by 0.12-0.23°C in response to corresponding 1°C change in air temperature, while, in absence of snow cover, soil temperature changed by 0.22-0.44°C. |
Notes: | Polar Science. Vol. 6(3-4) :226-236 (2012). |
Keywords: | 551.1/.4 -- Geology. 631.436 -- Soils, thermal properties. 551.52 -- Atmospheric radiation and temperature. 551.525 -- Earth temperatures, meteorological aspects. 551.578.46 -- Snow cover and snow patches. 536.5 -- Temperature measurement and control. B -- Geology and soil sciences. (*3) -- Arctic regions. (*38) -- Greenland. |
SPRI record no.: | 202176 |
LDR 01682naa#a2200000#a#4500 001 SPRI-202176 005 20230326041538.0 007 ta 008 230326s2012####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-202176 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aMackiewicz, Michael C. 245 12 ‡aA new approach to quantifying soil temperature responses to changing air temperature and snow cover /‡cMichael C. Mackiewicz. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2012. 300 ## ‡ap. 226-236 :‡bill., diags., tables, map. 500 ## ‡aPolar Science. Vol. 6(3-4) :226-236 (2012). 520 3# ‡aReports use of multiple linear regression (MLR) with dummy predictor variables to quantify degree of dampening between air and shallow soil temperatures in presence and absence of snow cover at four sites in Greenland. Results obtained for sites indicated that, with snow cover, temperature of shallow soils changed by 0.12-0.23°C in response to corresponding 1°C change in air temperature, while, in absence of snow cover, soil temperature changed by 0.22-0.44°C. 530 ## ‡aAlso issued online ‡uurn:doi:10.1016/j.polar.2012.06.003‡uhttps://dx.doi.org/10.1016/j.polar.2012.06.003 650 07 ‡a551.1/.4 -- Geology.‡2udc 650 07 ‡a631.436 -- Soils, thermal properties.‡2udc 650 07 ‡a551.52 -- Atmospheric radiation and temperature.‡2udc 650 07 ‡a551.525 -- Earth temperatures, meteorological aspects.‡2udc 650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc 650 07 ‡a536.5 -- Temperature measurement and control.‡2udc 650 07 ‡aB -- Geology and soil sciences.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*38) -- Greenland.‡2udc 773 0# ‡7nnas ‡tPolar Science. ‡gVol. 6(3-4) (2012) ‡wSPRI-178968 916 ## ‡a2013/01/23 -- JW 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230326 ‡bJW