FIELD: physics.
SUBSTANCE: anomalies of the water weight equivalent are received based on the gravity data of the satellite measurements GRACE (Gravity Recovery and Climate Experiment). The average number of solid precipitation is calculated based on the anomalies of the water weight equivalent, considering the terrain. The map-charts of the solid precipitation spatial distribution are created in view of the terrain. The map-charts of the solid precipitation spatial distribution are detailed by using the reduction factors.
EFFECT: increasing the spatial resolution of the map-charts.
2 dwg
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