By Peter O. Zavialov
Read or Download Physical Oceanography of the Dying Aral Sea (Springer Praxis Books Geophysical Sciences) PDF
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Extra resources for Physical Oceanography of the Dying Aral Sea (Springer Praxis Books Geophysical Sciences)
Hereinafter, AD and SD indicate the respective deltas of AmuDarya and Syr-Darya. Redrawn from Bortnik and Chistyaeva (1990). Sec. 1. Monthly mean air temperature ( C) in Aralsk and Muynak (1951±1960) for different months. Hereinafter, I is January, XII is December, etc. Adapted from Bortnik and Chistyaeva (1990). 6 The mean summer temperatures of the air over the Aral Sea are lower than those of the air over the surrounding deserts by up to 5 C. 1. 2 Humidity and precipitation Relative humidity of air in the Aral Sea region in summer is 20±25% higher than that in the surrounding desert areas.
8 ppt. According to Kosarev (1975), seasonal salinity changes in the open sea are smaller. The underlying interannual variability range is normally within 1 ppt, but it can be up to 4 ppt for spring months, which is associated with varying ice conditions and also intensity and timing of maximum ¯uvial discharges in individual years. The maximum seasonal range is observed in the Small Sea where the ice conditions in winter are most severe. In winter and spring, the salinity distribution is rather homogeneous, both horizontally and vertically, because of the winter convective mixing of the basin.
Summertime conditions in the region are typically characterized by clear sky and high air temperature. Lower temperature episodes can be provoked by atmospheric intrusions from the north or north-west. In winter, the region is under the peripheral 20 The immediate past: A summary of the pre-desiccation state [Ch. 2 in¯uence from the Siberian high-pressure system, which often results in clear and dry weather. At the same time, western intrusions can be accompanied by intense precipitation events.