Using Remote Sensing to Map and Monitor
Water Resources in Arid and Semiarid
Regions
Victor Klemas and Aline Pieterse
Contents
1 Introduction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 34
2 Identification and Mapping of Arid and Semiarid Regions . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 35
3 Detecting and Mapping Inland Surface Waters . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 36
4 Detecting Subsurface Waters . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 38
4.1 Determining Soil Moisture . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 38
4.2 Detecting Groundwater . . . . . . . . . . . . . .. . . . . . . . . . . . . . . . . . . . . .. . . . . . . . . . . . . . . . . . . . . . .. . . . . . 41
5 Detecting Freshwater Springs and Biomass . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 44
5.1 Detecting Freshwater Plumes . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 45
5.2 Determining Biomass Production . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 46
5.3 Biomass as a Drought Indicator . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 47
6 Detecting and Mapping Wetlands . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 48
7 Drought Monitoring and Prediction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 51
8 Conclusions . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 52
References . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 54
Abstract Life on Earth depends on water. Yet water resources are severely
stressed by the rapid growth of the human population and activities. In arid
environments the exploration and monitoring of water resources is a prerequisite
for water accessibility and rational use and management. To survey large arid areas
for water, conventional land-based techniques must be complemented by using
satellite and airborne remote sensors. Surface water systems can be mapped using
multispectral and radar sensors; soil moisture in the unsaturated zone can be
remotely sensed with microwave radiometers using indirect indicators, such as
V. Klemas (*)
School of Marine Science and Policy, University of Delaware, Newark, DE, USA
e-mail: klemas@udel.edu
A. Pieterse
Department of Geological Sciences, University of Delaware, Newark, DE, USA
© Springer International Publishing Switzerland 2015
T. Younos, T.E. Parece (eds.), Advances in Watershed Science
and Assessment, The Handbook of Environmental Chemistry 33,
DOI 10.1007/978-3-319-14212-8_2
33
Water Resources in Arid and Semiarid
Regions
Victor Klemas and Aline Pieterse
Contents
1 Introduction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 34
2 Identification and Mapping of Arid and Semiarid Regions . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 35
3 Detecting and Mapping Inland Surface Waters . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 36
4 Detecting Subsurface Waters . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 38
4.1 Determining Soil Moisture . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 38
4.2 Detecting Groundwater . . . . . . . . . . . . . .. . . . . . . . . . . . . . . . . . . . . .. . . . . . . . . . . . . . . . . . . . . . .. . . . . . 41
5 Detecting Freshwater Springs and Biomass . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 44
5.1 Detecting Freshwater Plumes . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 45
5.2 Determining Biomass Production . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 46
5.3 Biomass as a Drought Indicator . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 47
6 Detecting and Mapping Wetlands . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 48
7 Drought Monitoring and Prediction . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 51
8 Conclusions . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 52
References . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 54
Abstract Life on Earth depends on water. Yet water resources are severely
stressed by the rapid growth of the human population and activities. In arid
environments the exploration and monitoring of water resources is a prerequisite
for water accessibility and rational use and management. To survey large arid areas
for water, conventional land-based techniques must be complemented by using
satellite and airborne remote sensors. Surface water systems can be mapped using
multispectral and radar sensors; soil moisture in the unsaturated zone can be
remotely sensed with microwave radiometers using indirect indicators, such as
V. Klemas (*)
School of Marine Science and Policy, University of Delaware, Newark, DE, USA
e-mail: klemas@udel.edu
A. Pieterse
Department of Geological Sciences, University of Delaware, Newark, DE, USA
© Springer International Publishing Switzerland 2015
T. Younos, T.E. Parece (eds.), Advances in Watershed Science
and Assessment, The Handbook of Environmental Chemistry 33,
DOI 10.1007/978-3-319-14212-8_2
33
