XVI Contents
8.2
8.2.1
8.2.2
8.3
8.3.1
8.3.2
8.3.3
8.304
8.3.5
8.3.6
804
804.1
804.2
8.5
8.6
8.7
8.8
8.9
Evaporation and radiometric variables ................... 160
Potential Evaporation. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 160
Actual Evaporation .................................... 162
Remote Sensing of Land Evaporation: Applications and
Modelling Approaches. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 165
General. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 165
Linear relationships between evaporation and land surface
temperature [1] ....................................... 166
Improved linear relationships [2] ....................... , 167
Relationships between evaporation, surface, temperature
and spectral indices [3] ................................. 168
Soil Vegetation Atmosphere Transfer
(SVAT) models [4] .................................... 169
Integrated SVAT and Planetary Boundary Layer (PBL)
models [5] ........................................... 170
Current trends: improved observations and improved
parameterizations .............. . . . . . . . . . . . . . . . . . . . . . .. 171
Local maximum evaporation
and land surface temperature [6] ........................ 171
Improved observation ofland surface variables [7] ........ 174
Spatial variability ..................................... 177
Accuracy ............................................. 178
Applications. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 179
Current and Future Observations . . . . . . . . . . . . . . . . . . . . . . .. 180
Summary and Conclusions . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 181
Colour Plates of Chaps. 6-8 . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 189
Chapter 9
9.1
9.2
9.3
904
9.5
Chapter 10
10.1
10.2
10.3
lOA
10.5
10.6
10.7
10.8
Soil Moisture . ....................................... 197
Introduction. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 197
General Approach. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 198
Sensor-Target Interactions. . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 202
Hydrologic Examples .................................. 209
Future Microwave Remote Sensing of Soil Moisture ....... 212
Remote Sensing of Surface Water ..................... 217
Introduction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 217
Surface Water Detection . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 218
Lake and Reservoir Area Estimates. . . . . . . . . . . . . . . . . . . . .. 220
Wetlands. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 223
Lake Levels . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 224
River Levels and Flows ................................ 226
Flood Extent. ......................................... 230
Conclusion ........................................... 233
8.2
8.2.1
8.2.2
8.3
8.3.1
8.3.2
8.3.3
8.304
8.3.5
8.3.6
804
804.1
804.2
8.5
8.6
8.7
8.8
8.9
Evaporation and radiometric variables ................... 160
Potential Evaporation. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 160
Actual Evaporation .................................... 162
Remote Sensing of Land Evaporation: Applications and
Modelling Approaches. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 165
General. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 165
Linear relationships between evaporation and land surface
temperature [1] ....................................... 166
Improved linear relationships [2] ....................... , 167
Relationships between evaporation, surface, temperature
and spectral indices [3] ................................. 168
Soil Vegetation Atmosphere Transfer
(SVAT) models [4] .................................... 169
Integrated SVAT and Planetary Boundary Layer (PBL)
models [5] ........................................... 170
Current trends: improved observations and improved
parameterizations .............. . . . . . . . . . . . . . . . . . . . . . .. 171
Local maximum evaporation
and land surface temperature [6] ........................ 171
Improved observation ofland surface variables [7] ........ 174
Spatial variability ..................................... 177
Accuracy ............................................. 178
Applications. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 179
Current and Future Observations . . . . . . . . . . . . . . . . . . . . . . .. 180
Summary and Conclusions . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 181
Colour Plates of Chaps. 6-8 . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 189
Chapter 9
9.1
9.2
9.3
904
9.5
Chapter 10
10.1
10.2
10.3
lOA
10.5
10.6
10.7
10.8
Soil Moisture . ....................................... 197
Introduction. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 197
General Approach. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 198
Sensor-Target Interactions. . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 202
Hydrologic Examples .................................. 209
Future Microwave Remote Sensing of Soil Moisture ....... 212
Remote Sensing of Surface Water ..................... 217
Introduction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 217
Surface Water Detection . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 218
Lake and Reservoir Area Estimates. . . . . . . . . . . . . . . . . . . . .. 220
Wetlands. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 223
Lake Levels . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .. 224
River Levels and Flows ................................ 226
Flood Extent. ......................................... 230
Conclusion ........................................... 233
