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With greater accumulation of dense ice on the crystal, its fall velocity increases.
This means that coarser sand with larger fall velocity corresponds to quicker sediment response.
Terminal fall velocity of particles with mean diameter of 50 μm is calculated as ~0.1 m/s.
For this reason, a new parameter, named wave erosivity factor, was introduced by considering the fall velocity of grains as a constant in the Ω parameter.
The sediment diffusion is represented by an adaptation time T s, which is a function of the local water depth and the sediment fall velocity w s.
The average vertical structure is studied in terms of drop size distribution (DSD), fall velocity, rain rate, liquid water content and radar reflectivity profile.
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Fall velocities of snow range up to about 2 metres per second (6.5 feet per second).
The typical radii of raindrops resulting from this type of precipitation process range up to several millimetres and have fall velocities of around 3 to 4 metres (10 to 13 feet) per second.
The model was verified using experimental results from droplet fall velocities and loss rates.
The average relative error between the predicted and measured data of fall velocities and loss rates were 1.2%and4.3%3%, respectively.
On the other hand, Suzuki (1983) estimated terminal fall velocities of volcanic particles as a function of mean diameter in the atmosphere.
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