TY - JOUR
T1 - Determining Bathymetry of Shallow and Ephemeral Desert Lakes Using Satellite Imagery and Altimetry
AU - Armon, M.
AU - Dente, E.
AU - Shmilovitz, Y.
AU - Mushkin, A.
AU - Cohen, T. J.
AU - Morin, E.
AU - Enzel, Y.
N1 - Publisher Copyright:
©2020. American Geophysical Union. All Rights Reserved.
PY - 2020/4/16
Y1 - 2020/4/16
N2 - Water volume estimates of shallow desert lakes are the basis for water balance calculations, important both for water resource management and paleohydrology/climatology. Water volumes are typically inferred from bathymetry mapping; however, being shallow, ephemeral, and remote, bathymetric surveys are scarce in such lakes. We propose a new, remote-sensing-based, method to derive the bathymetry of such lakes using the relation between water occurrence, during >30 year of optical satellite data, and accurate elevation measurements from the new Ice, Cloud, and Land Elevation Satellite-2 (ICESat-2). We demonstrate our method at three locations where we map bathymetries with ~0.3 m error. This method complements other remotely sensed, bathymetry-mapping methods as it can be applied to: (a) complex lake systems with subbasins, (b) remote lakes with no in-situ records, and (c) flooded lakes. The proposed method can be easily implemented in other shallow lakes as it builds on publically accessible global data sets.
AB - Water volume estimates of shallow desert lakes are the basis for water balance calculations, important both for water resource management and paleohydrology/climatology. Water volumes are typically inferred from bathymetry mapping; however, being shallow, ephemeral, and remote, bathymetric surveys are scarce in such lakes. We propose a new, remote-sensing-based, method to derive the bathymetry of such lakes using the relation between water occurrence, during >30 year of optical satellite data, and accurate elevation measurements from the new Ice, Cloud, and Land Elevation Satellite-2 (ICESat-2). We demonstrate our method at three locations where we map bathymetries with ~0.3 m error. This method complements other remotely sensed, bathymetry-mapping methods as it can be applied to: (a) complex lake systems with subbasins, (b) remote lakes with no in-situ records, and (c) flooded lakes. The proposed method can be easily implemented in other shallow lakes as it builds on publically accessible global data sets.
KW - Desert hydrology
KW - Ephemeral desert lakes
KW - ICESat-2 altimetry
KW - Lake Eyre
KW - Lake bathymetry
KW - remote sensing bathymetry
UR - http://www.scopus.com/inward/record.url?scp=85083517417&partnerID=8YFLogxK
U2 - 10.1029/2020GL087367
DO - 10.1029/2020GL087367
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AN - SCOPUS:85083517417
SN - 0094-8276
VL - 47
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 7
M1 - e2020GL087367
ER -