The potential of remotely sensed thermal infrared data to infer surface soil moisture and evaporation

Water Resources Research

Volumn 16, Issue 4, 1980, Pages 787-795

  Price, John C ^a  

^a NONE

Author keywords

[No Author keywords available]

Indexed keywords

DIURNAL HEAT CAPACITY;

EVAPORATION; HYDROLOGY - MATHEMATICAL MODELS; WATER RESOURCES - RESEARCH;

SOILS;

EID: 0019229290     PISSN: 00431397     EISSN: 19447973     Source Type: Journal    
DOI: 10.1029/WR016i004p00787     Document Type: Article

References (22)

1. Notes on radiation in the atmosphere
2. Flux profile relationships in the atmospheric surface layer
3. On the detection of shallow aquifers using thermal infrared imagery
4. Detection of soil moisture by remote surveillance
5. The utility of surface temperature measurements for the remote sensing of surface soil water status
6. Compensating for environmental variability in the thermal inertia approach to remote sensing of soil moisture
7. An equation for potential evaporation from soil, water, and crop surfaces adaptable to use by remote sensing
8. Surface albedo and desertification
9. Calculation of evaporation rates during the transition from energy‐limiting to soil‐limiting phases using albedo data
10. Thermal inertia mapping: A new geologic mapping tool
11. Thermal inertia mapping from satellites—Discrimination of geologic units in Oman
12. The thermal inertia approach to mapping soil moisture and geology
13. Thermal inertia mapping: A new view of the earth
14. Sensitivity of diurnal temperature range to changes in physical parameters
15. Geologic applications of thermal infrared imagery
16. Remote sensing in evapotranspiration research on the Great Plains