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Record #126355:

Southern Michigan's snow belt: modelled impacts on soil temperatures and freezing / S.A. Isard, R.J. Schaetzl.

Title: Southern Michigan's snow belt: modelled impacts on soil temperatures and freezing / S.A. Isard, R.J. Schaetzl.
Author(s): Isard, S. A.
Schaetzl, R. J.
Date: [1993]
In: Eastern Snow Conference. Proceedings. ([1993]), Vol. 50th Annual Meeting ([1993])
Abstract: Physically based computer model is developed for estimating soil temperatures at depths between 0.05 and 0.5 m in sandy, forested soils, using daily minimum and maximum air temperatures and precipitation as input data. Algorithm is evaluated by comparing its output to 490 soil temperature observations for 1990-93 at stations in southern Michigan. This region was chosen because it experiences subfreezing temperatures and has widely variable differences in snow accumulations, spatially and temporally. Model is used to simulate soil temperatures over 41 years (1951-91) at 14 sites. Simulations show pronounced impact of Great Lakes on soil temperature, primarily through influence on patterns of winter precipitation and air temperatures.
Notes:

Eastern Snow Conference. Proceedings. Vol. 50th Annual Meeting :247-253 ([1993]).

Joint Meeting with 61st Western Snow Conference.

Keywords: 551.578.46 -- Snow cover and snow patches.
551.578.468 -- Snow cover, protection and insulation.
519.673 -- Modelling.
E10 -- Glaciology: snow and avalanches.
(73) -- United States.
(77) -- North central states.
SPRI record no.: 126355

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245 10 ‡aSouthern Michigan's snow belt :‡bmodelled impacts on soil temperatures and freezing /‡cS.A. Isard, R.J. Schaetzl.
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300 ## ‡ap. 247-253 :‡bdiag., tables, map.
500 ## ‡aEastern Snow Conference. Proceedings. Vol. 50th Annual Meeting :247-253 ([1993]).
500 ## ‡aJoint Meeting with 61st Western Snow Conference.
520 3# ‡aPhysically based computer model is developed for estimating soil temperatures at depths between 0.05 and 0.5 m in sandy, forested soils, using daily minimum and maximum air temperatures and precipitation as input data. Algorithm is evaluated by comparing its output to 490 soil temperature observations for 1990-93 at stations in southern Michigan. This region was chosen because it experiences subfreezing temperatures and has widely variable differences in snow accumulations, spatially and temporally. Model is used to simulate soil temperatures over 41 years (1951-91) at 14 sites. Simulations show pronounced impact of Great Lakes on soil temperature, primarily through influence on patterns of winter precipitation and air temperatures.
650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc
650 07 ‡a551.578.468 -- Snow cover, protection and insulation.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡aE10 -- Glaciology: snow and avalanches.‡2local
651 #7 ‡a(73) -- United States.‡2udc
651 #7 ‡a(77) -- North central states.‡2udc
700 1# ‡aSchaetzl, R. J.
773 0# ‡7nnas ‡tEastern Snow Conference. Proceedings. ‡gVol. 50th Annual Meeting ([1993]) ‡wSPRI-23848
917 ## ‡aUnenhanced record from Muscat, imported 2019
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