Use of optical and radar remote sensing satellites for identifying and monitoring active/inactive landforms in the driest desert in Saudi Arabia
Section snippets
Background
Earth observations from space using optical, thermal, and radar remote sensing sensors have helped resolve significant geomorphological and geological problems across a range of spatial and temporal scales (Abdelkareem et al., 2018). Active synthetic aperture radar (SAR) satellites that operate continuously in all weather conditions emit and receive electromagnetic (EM) radiation and record backscattered pulses that characterize the geometry of the target (Roth & Elachi, 1975; Schaber et al.,
Study area
The study area is in the eastern part of Saudi Arabia and covers a large area that ends at the Arabian Gulf to the east. One of the driest regions of the Arabian Peninsula, with a mean yearly precipitation of 70 mm (Hoetzl, 1995), the area extends from longitude 42° 32′ 56′′ E and 52° 56′ 29′′ E and latitude 21°25′ 35′′ N and 25° 21′ 22′′ E (Fig. 1). The investigated area belongs to the Arabian Shelf platform, comprising a sedimentary sequence of Paleozoic to Cenozoic rocks dipping NE and E
Data and methods
Electromagnetic radiation, particularly low-frequency microwaves, was used to characterize surface roughness, moisture, structure, and geomorphic features; reveal paleodrainage systems based on near-surface forms and structures; and detect extremely small changes at the land surface. The penetration capability of low-frequency radar was used to image and map hidden features under the dry loose sand of the study area with a high degree of certainty. Rather than optical sensors that have limited
Paleohydrological systems
Investigation and clarification of microwave EM data (i.e., the ALOS/PALSAR, Sentinel-1 and SRTM DEM, and VNIR/SWIR data of Landsat-8, Sentinel-2, and Google Earth images) revealed several past and present geomorphic and structural features in the study area. The SRTM DEM data (Fig. 1c) revealed that the area is characterized by wide variations in topography between 0 and 1453 m above sea level (a.s.l.), and most of the downstream areas are covered by mobile sand dunes. This topographic
Discussion
The analysis and interpretation of a wide array of space-borne remote sensing data provide spatially and temporally repeatable observations and enabled us to identify paleohydrological systems, observe sand dune dynamics and human activity in arid land environments.
In this study, the low-frequency SAR data were used to characterize several buried drainage systems under sand sheets and thick sand dunes (Fig. 3); because the low attenuation (high penetration capability) of the long wavelengths of
Conclusions
Recent advances in Earth observation from space enable the detection of buried features under sand sheets and dunes in a fast and cost-effective manner. Such features are difficult to observe by using other techniques. The processing and interpretation of a wide array of optical and radar remote sensing data including Landsat OLI, SRTM, ALOS/PALSAR, and Sentinel-1/2 revealed surface and near-surface features in the eastern part of Saudi Arabia. We used several approaches incorporating a wide
Declaration of competing interest
The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.
Acknowledgments
The authors wish to express their gratitude to the editor and the reviewers. The authors also would like to extend their sincere appreciation to the Deanship of Scientific Research, King Saud University, for funding this research (RG-1437-012), and RSSU at King Saud University for their technical support.
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