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. (Balanis 6.43) You can confim tat AF = e j kd cosθ + e j kd cosθ N = cos kd cosθ gives te same esult as (6-59) and (6-6), fo a binomial aay wit te coefficients cosen as in section 6.8.. Tis single expession

Retrieval of three-dimensional distribution of rainfall parameters for rain attenuation correction using multi-parameter radar

Retieval of thee-dimensional distibution of ainfall paametes fo ain attenuation coection using multi-paamete ada Dong-Soon Kim 1, Dong-In Lee 1, Masayuki Maki 2 and Ji-Young Gu 1 1 Depatment of Envionmental

Water flows through the voids in a soil which are interconnected. This flow may be called seepage, since the velocities are very small.

Wate movement Wate flows though the voids in a soil which ae inteconnected. This flow may be called seepage, since the velocities ae vey small. Wate flows fom a highe enegy to a lowe enegy and behaves