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Snow cloud distribution in the lower atmosphere was observed using two optical lidars (ceilometer) set up at the distance of 3.1 km. Visualization was constructed from two time series data measured by each lidar. The instruments additionally included weather station, to measure wind speed and direction, and snowfall gauge, to calculate precipitation rate. Combination of all these instruments with...
Snow cloud distribution in the lower atmosphere was observed using two optical lidars (ceilometer) set up at the distance of 3.1 km. Visual display was constructed from two time series data measured by each lidar. The instruments additionally included weather station, to measure wind speed and direction, and snowfall gauge, to calculate precipitation rate. All the data were displayed on the same coordinate...
Water vapor distribution in the lower atmosphere was observed using two optical lidars (ceilometer) set up at the distance of 3.1 km. Range height indicator (RHI) display was constructed from two time series data measured by each lidar. The instruments were also included small vertical radar and snowfall gauge. All the data were displayed on the same coordinate system to compare the profiles with...
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