Lake Volume Monitoring from Space

Мониторинг объёма озёр из космоса
J.-F. Crétaux, Rodrigo Abarca-del-Río, Muriel Bergé‐Nguyen, A. Arsen, Vanessa Drolon, Guillaume Clos, Philippe Maisongrande
2016-02-07

SAR interferometryTibetan Plateaulake water storageremote sensingsatellite altimetry
Lakes are integrators of environmental change occurring at both the regional and global scale. They present a wide range of behavior on a variety of timescales (cyclic and secular) depending on their morphology and climate conditions. Lakes play a crucial role in retaining and stocking water, and because of the significant global environmental changes occurring at several anthropocentric levels, the necessity to monitor all morphodynamic characteristics [e.g., water level, surface (water contour) and volume] has increased substantially. Satellite altimetry and imagery are now widely used together to calculate lake and reservoir water storage changes worldwide. However, strategies and algorithms to calculate these characteristics are not straightforward, and specific approaches need to be developed. We present a review of some of these methodologies by using lakes over the Tibetan Plateau to illustrate some critical aspects and issues (technical and scientific) linked to the observation of climate change impact on surface waters from remote sensing data. Many authors have measured water variation using the limited remote sensing measurements available over short time periods, even though the time series are probably too short to directly link these results with climate change. Indeed, there are many processes and factors, like the influence of lake morphology, that are beyond observation and are still uncertain. The time response for lakes to reach a new state of equilibrium is a key aspect that is often neglected in current literature. Observations over a long period of time, including maintaining a constellation of comprehensive and complementary satellite missions with service continuity over decades, are therefore necessary especially when the ground gauge network is too limited. In addition, the design of future satellite missions with new instrumental concepts (e.g., SAR, SARin, Ka band altimetry, Ka interferometry) will also be suitable for complete monitoring of continental waters.
1
Calculating lake morphodynamic characteristics from remote sensing requires lake-specific strategies and algorithms because morphology and climate conditions produce diverse temporal behaviors.
2
Decades-long continuity of complementary satellite missions is necessary for reliable lake monitoring, particularly where ground-gauge networks are sparse; future SAR, SARin, and Ka-band instruments could improve completeness.
3
Lake response times for reaching a new equilibrium are frequently neglected but are essential for interpreting environmental-change impacts on surface waters.
4
Satellite altimetry and imagery can be combined to estimate global lake and reservoir water-storage changes, including water level, surface area, and volume.
5
Short remote-sensing time series are generally insufficient to attribute observed lake-water variations directly to climate change, with morphology and other unobserved processes introducing uncertainty.

Lakes and reservoirs, with emphasis on surface waters over the Tibetan Plateau

Remote-sensing monitoring of lake morphodynamic characteristics—water level, surface area/contour, volume, and storage changes—and their response to climate change over long timescales

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Publication Date
2016-02-07
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J.-F. Crétaux
Rodrigo Abarca-del-Río
Muriel Bergé‐Nguyen
A. Arsen
Vanessa Drolon
Guillaume Clos
Philippe Maisongrande
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