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ISSN 2070-7401 (Print), ISSN 2411-0280 (Online)
Sovremennye problemy distantsionnogo zondirovaniya Zemli iz kosmosa
CURRENT PROBLEMS IN REMOTE SENSING OF THE EARTH FROM SPACE

  

Sovremennye problemy distantsionnogo zondirovaniya Zemli iz kosmosa, 2019, Vol. 16, No. 3, pp. 44-60

The use of satellite data on land surface and meteorological characteristics in modeling the water and heat regimes of large agricultural region

E.L. Muzylev 1 , Z.P. Startseva 1 , A.M. Zeyliger 2 , O.S. Ermolaeva 2 , E.V. Volkova 3 , E.V. Vasilenko 3 , A.I. Osipov 4 
1 Water Problems Institute RAS, Moscow, Russia
2 Russian State Agrarian University ― Moscow Timiryazev Agricultural Academy, Moscow, Russia
3 State Research Center “Planeta”, Moscow, Russia
4 Agrophysical Research Institute, Saint Petersburg, Russia
Accepted: 10.03.2019
DOI: 10.21046/2070-7401-2019-16-3-44-60
Estimates of the water and heat regime characteristics of the part of the Central Black Earth region territory largely occupied by crops are presented for the vegetation seasons 2016–2017. These estimates were obtained using the model of vertical water and heat exchange between land surface and atmosphere LSM (Land Surface Model) utilizing satellite information on the land surface and meteorological conditions. This information was presented by the data of AVHRR/NOAA, MSU MR/“Meteor-M” No. 2, and SEVIRI/Meteosat-10, -11, -8. Among the characteristics calculated using the model are soil water content W, evapotranspiration Ev, vertical heat fluxes, land surface temperature, soil moisture and temperature at different soil depths. In the frame of this approach, the methods to use satellite-derived from Meteosat-11, -8 data estimates of meteorological characteristics (precipitation, vegetation and soil surface temperatures, effective land surface temperature) and vegetation characteristics (vegetation index NDVI, vegetation cover fraction B, leaf area index LAI, etc.) in the model were tested for the territory under study. Values of W and Ev in their dynamics during the vegetation season modeled using different variants of satellite-derived vegetation and meteorological characteristic estimation from measurements of all the above sensors were compared with actual W and Ev values. The estimation errors were within 15 % for W and 25 % for Ev. The possibility to use estimates of soil surface moisture, obtained from the ASCAT/MetOp scatterometer measurements in the microwave range when modeling was shown. Using these estimates, the initial conditions can be selected when calculating soil water content W and evaporation from the soil surface Evg, which is one of the water regime characteristics. The calculated Evg values were used directly to calculate values of W as well as to assign the upper boundary condition for the vertical soil water transfer equation.
Keywords: modeling, satellite data, soil water content, evapotranspiration, water and heat regimes, soil surface moisture, precipitation, land surface temperature, leaf area index, vegetation cover fraction
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