Soil moisture–temperature relationships: results from two field experiments
Article first published online: 7 OCT 2003
Copyright © 2003 John Wiley & Sons, Ltd.
Volume 17, Issue 15, pages 3041–3057, 30 October 2003
How to Cite
Lakshmi, V., Jackson, T. J. and Zehrfuhs, D. (2003), Soil moisture–temperature relationships: results from two field experiments. Hydrol. Process., 17: 3041–3057. doi: 10.1002/hyp.1275
- Issue published online: 7 OCT 2003
- Article first published online: 7 OCT 2003
- Manuscript Accepted: 8 JAN 2003
- Manuscript Received: 7 DEC 2001
- soil moisture;
- surface temperature;
- field experiments
This paper analyses data from two field experiments in Chickasha, Oklahoma, and Tifton, Georgia, carried out in July 1999 and June 2000 respectively. The observations on soil moisture at two depths, viz. 0–2·5 and 0–5·0 cm, surface temperature, and temperatures at 1, 5 and 10 cm depths are analysed. The relationship between the soil moisture and the temperature variability in time is examined as a function of vegetation type and location. Results from these experiments show that, during drydown, surface temperature shows an increase that corresponds to a decrease in the soil moisture. Linear models for prediction of soil moisture (at both depths) using surface temperature observations are examined. Copyright © 2003 John Wiley & Sons, Ltd.