255
Atmospheric
Radiation
frontal cloudy systems has been developed [Nerushev et al., 2013]. Spatial dis‑
tribution of jet flows in the satellite surveillance zones and the intra-annual var‑
iability of their characteristics in the upper troposphere of Northern and Southern
hemispheres was studied by the automated method [Ivangorodsky and Nerushev,
2014]. The cycle of studies on developing methods of satellite diagnosis and
forecasting of summer squalls and thunderstorms has been fulfilled [Bukharov,
2013].
Some studies devoted to the satellite monitoring of the Black Sea oil pollution
[Lavrova and Mityagina, 2013], the total ice concentration [Alekseeva and
Frolov, 2013] and blooms of coc-colithophore E. huxleyi in Arctic waters [Pe‑
trenko et al., 2013] have been also fulfilled.
Joint studies of Water Problems Institute RAS and SRB “Planeta” directed to
using the remote sensing data on surface characteristics
in the simulation of
components of water and heat balances for a river headwater are carried on.
Methods of the AVHRR/NOAA, MODIS/Terra, Aqua, SEVIRI/Meteosat satel‑
lite data processing, which provide the retrieval of vegetation characteristics,
land-surface temperature, and precipitation, have been developed or refined. The
techniques for the assimilation of satellite-based products in the model have been
developed. Some major water regime characteristics have been generated such
as soil water content, evapotranspiration, and others [Startseva et al., 2014]. In
addition the model of the vertical heat-water transfer in the soil-vegetation-at‑
mosphere system (SVAT) utilizing the satellite data on underlying surface and a
number of meteorological characteristics has been improved. Using the SVAT
model, calculations of the water regime of the vast agricultural areas are carried
out [Gelfan et al., 2012].
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