Atmospheric Propagation and Remote Sensing

Atmospheric Propagation and Remote Sensing

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... intense insolation, resulted in the development of afternoon and evening thunderstorms over the northern and central parts of ... Delta-T fluctuated between a€”1 and a€”2 AdF (1500-1800 MST), then decreased in magnitude, crossing through 0 AdF at ... delta-T experienced wide fluctuations, on the order of 4 to 5 AdF. The afternoon optical turbulence time series displayed ... During this period, CD2 decreased from about 5 x 10~aquot; maquot;273 (1500 MST) to about 9 x 10aquot; 14 m_2/3 (1700 MST).

Title:Atmospheric Propagation and Remote Sensing
Publisher:Society of Photo Optical - 1993

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