Document Type
Article
Publication Date
4-23-2005
Publication Title
Geophysical Research Letters
Volume
32
Abstract
[1] The close relationship between air and ground temperatures has been used to reconstruct paleoclimate conditions from ground temperatures. Unfortunately, the presence of snow decouples air and ground temperatures and obscures their relationship. The objective of this paper is to investigate the role that snowpack conditions play in affecting the relationship between air and soil temperatures. The annual thermal offset between mean annual soil and air temperatures is examined over a 12 year period (1990–2002) at Fargo, ND, using observed soil temperatures along with simulations from a physically based snowpack model. Early season snow cover does not necessarily lead to large thermal offsets. These snowpacks, while low in density, also tended to be shallow and therefore do not provide much thermal insulation. Winter snowpacks explain a greater portion of the annual thermal offset. While denser than fall snowpacks, the extra depth and longer persistence leads to superior insulation of the ground.
Issue
8
DOI
10.1029/2005GL022532
ISSN
1944-8007
Rights
An edited version of this paper was published by AGU. Copyright 2005 American Geophysical Union.
Recommended Citation
Andrew Grundstein, Paul E. Todhunter, and Thomas Mote. "Snowpack control over the thermal offset of air and soil temperatures in eastern North Dakota" (2005). Geography & Geographic Information Science Faculty Publications. 3.
https://commons.und.edu/geo-fac/3