GM001

Institut Teknologi Sepuluh Nopember

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Presentatie

course of the interbasin exchange through the connecting channel.
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94

januari 2023

2022/2023
of agricultural diversions and unsustainable use of water resources in the river basins. This lead to drastic changes of the Aral’s water balance, resulting in rapid shallowing of the lake. In 1989, the northernmost part of the Aral Sea and the main body of the lake separated, forming two individual lakes known as the Small Sea and the Large Sea. In this paper, we focus on the Large Sea only. By now, the lake surface level has dropped by almost 23 meters with respect to the value of 19...
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Presentatie

not only because of the local evaporation, but also because of the assimilation of the saltier eastern basin water in the course o
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65

januari 2023

2021/2022
the interbasin exchange through the connecting channel. The satellite imagery analysis, in particular the Maximum CrossCorrelation method, suggests that the circulation pattern in
emax59
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Presentatie

hydrographic survey
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22

januari 2023

2021/2022
The salinity in the western deep basin of the Aral Sea varied from about 82 psu at the surface to over 94 psu at the bottom. The absolute lake surface level was about 30.5 m. Hence, the observed salinity values were much higher, and the level much lower, than expected according to earlier predictions. The density in the western basin exhibited an extremely strong stratification of 11 kg/m3 per 20 m in the bottom layer. The picnocline was accompanied by a temperature inversion whose mag...
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