Abstract

ABSTRACTAral Sea has gone through a drastic shrinkage during the past century, from more than 68,000 km2 in 1960s to less than 10,000 km2 in 2015. The desiccation was highly severe in 2009 and 2014 due to the west basin changed to an exposed bottom for several months. Then dust storms, fishery recession and degraded plant communities followed, causing tremendous environmental problems and economic deteriorations. In this paper, high frequency water extents of Aral Sea during 2000–2015 were delineated by MODIS images. Water level changes of the lake were analyzed according to a water level database, which was derived on TOPEX/Poseidon, Jason-1, Jason-2, ENVISAT and SARAL altimeter data. Water volume changes during the same period were determined by a combination of lake surface extents and the corresponding water level data. The largest area of Aral Sea was 30,256.46 km2 in May 2000, and the smallest was 6926.04 km2 in November 2014. Water storage declination for the whole lake was up to 74km3 and water level dropped from 43.42 m to 39.73 m during 2000–2015. In a whole, west and east basins of the lake presented declination trends (−191.73 km2/yr and −1089.48 km2/yr), while the north basin showed a little increase with the rate of 38.18 km2/yr. For the three basins (north, west and east), corresponding level tendencies were 0.15 m/yr, −0.5 m/yr, −0.38 m/yr, and volume variations were 0.29 km3/yr, −1.36 km3/yr, −3.25 km3/yr, respectively.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.