SSSAJ Grow Your Career with SSSA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


This Article
Right arrow Figures Only
Right arrow Full Text Free
Right arrow Full Text (PDF) Free
Right arrow An erratum has been published
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via ISI Web of Science (16)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Decker, K. L. M.
Right arrow Articles by Scherbatskoy, T.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Decker, K. L. M.
Right arrow Articles by Scherbatskoy, T.
Agricola
Right arrow Articles by Decker, K. L. M.
Right arrow Articles by Scherbatskoy, T.
Related Collections
Right arrow Soil Thermal Properties
Right arrow Frozen Soils
Right arrow Forest Soils
Soil Science Society of America Journal 67:1234-1242 (2003)
© 2003 Soil Science Society of America

DIVISION S-7—FOREST & RANGE SOILS & SOIL & PLANT ANALYSIS

Snow Removal and Ambient Air Temperature Effects on Forest Soil Temperatures in Northern Vermont

K. L. M. Decker*,a,b, D. Wanga, C. Waitea and T. Scherbatskoya

a School of Natural Resources, George D. Aiken Center, Univ. of Vermont, Burlington, VT 05401
b Ecosystem Science and Technology Branch, NASA-Ames Research Center, M/S 242-4, Moffett Field, CA 94035

* Corresponding author (kdecker{at}mail.arc.nasa.gov)

We measured deciduous forest soil temperatures under control (unmanipulated) and snow-free (where snow is manually removed) conditions for four winters (at three soil depths) to determine effects of a snow cover reduction such as may occur as a result of climate change on Vermont forest soils. The four winters we studied were characterized as: ‘cold and snowy’, ‘warm with low snow’, ‘cold with low snow’, and ‘cool with low snow’. Snow-free soils were colder than controls at 5- and 15-cm depth for all years, and at all depths in the two cold winters. Soil thermal variability generally decreased with both increased snow cover and soil depth. The effect of snow cover on soil freeze-thaw events was highly dependent on both the depth of snow and the soil temperature. Snow kept the soil warm and reduced soil temperature variability, but often this caused soil to remain near 0°C, resulting in more freeze–thaw events under snow at one or more soil depths. During the ‘cold snowy’ winter, soils under snow had daily averages consistently >0°C, whereas snow-free soil temperatures commonly dropped below -3°C. During the ‘warm’ year, temperatures of soil under snow were often lower than those of snow-free soils. The warmer winter resulted in less snow cover to insulate soil from freezing in the biologically active top 30 cm. The possible consequences of increased soil freezing include more root mortality and nutrient loss, which would potentially alter ecosystem dynamics, decrease productivity of some tree species, and increase sugar maple (Acer saccharum Marshall) mortality in northern hardwood forests.

Abbreviations: IPCC, Intergovernmental Panel on Climate Change




This article has been cited by other articles:


Home page
Plant Cell PhysiolHome page
H. Inada, M. Nagao, S. Fujikawa, and K. Arakawa
Influence of Simulated Acid Snow Stress on Leaf Tissue of Wintering Herbaceous Plants
Plant Cell Physiol., April 1, 2006; 47(4): 504 - 512.
[Abstract] [Full Text] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2003 by the Soil Science Society of America.