RADIOBRIGHTNESS OF DIURNALLY HEATED, FREEZING SOIL

Freezing and thawing soils exhibit unique radiometric characteristics. To examine these characteristics, diurnal insolation is modeled as one-dimensional heating of a moist soil half-space during a typical fall at a northern Great Plains site (Bismarck, ND). The one-dimensional heat flow equation is nonlinear because both the enthalpy (the change in internal energy with temperature at constant pressure) and the thermal conductivity of freezing soils are nonlinear functions of temperature. The problem is particularly difficult because phase boundaries propagate in time, and because soils, particularly clay-rich soils, freeze over a range of temperatures rather than at 0°C—that is, they possess diffuse phase boundaries. A modified Chernous’ko method was used to integrate the heat flow equation to obtain monthly thermal models during a typical September through December period. Diurnal radiobrightness curves at 10.7, 18, and 37 GHz were computed for each month. The 37-GHz radiobrightness best tracks soil surface temperature; the 10.7–37-GHz spectral gradient of thawed soils is strongly positive; the spectral gradient of frozen soils is slightly negative; and the midnight-to-noon spectral gradient is shifted by approximately + 0.1 K/GHz by diurnal changes in the surface temperature and the thermal gradient. These observations support the use of the scanning multichannel microwave radiometer 37-GHz radiobrightness and its 10.7-37-GHz spectral gradient as discriminants in a frozen soil classifier for high latitude prairie. © 1990 IEEE