Spatial variation of evaporation from an area with dambos is derived from r
emotely sensed Landsat Thematic Mapper (TM) data. The temporal variation of
evaporation during the dry season from the area is used to classify the da
mbos on the basis of the time after the end of the rainy season when the da
mbo begins to evapotranspire at low rates indicating when they begin to dry
out. (C) 2000 Elsevier Science Ltd. All rights reserved.