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Seasonal variability of the Caspian Sea three-dimensional circulation, sea level and air-sea interaction

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Academic year: 2017

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Table 1. Monthly mean heat flux components (W/m 2 ) at the sea surface. Q s = incoming solar radiation, Q b = (long wave) thermal radiation, Q s + Q b = total radiative heat flux, H = sensible heat flux, LE = latent heat flux, Q = total heat flux.
Table 2. Water budget of the Caspian Sea. Water fluxes are given in cm/yr, expressed in units of mean sea level change.
Fig. 1. Scheme of the Caspian Sea sea currents (Lednev, 1943).
Fig. 2. Caspian mean sea level during the 1961–1996 period.
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