Physics
Scientific paper
Jan 1965
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1965jatp...27...91b&link_type=abstract
Journal of Atmospheric and Terrestrial Physics, vol. 27, no. 1, pp. 91-99
Physics
1
Scientific paper
Records of space charge concentration and potential gradient over a melting snow cover indicate an average concentration of 5500 negative elementary charges/cm3 in the first metre above the ground, with a wind speed of 10 m/sec, and an average of 770 positive/cm3 between 1 and 21 m. The upper positive space charge is accounted for by the blowing of snow on neighbouring high land. The lower negative charge in the air near the ground, persisting in spite of the wind, can be explained if a separation of charge occurs at the surface, the positive charge remaining on the melting snow.
Bent R. B.
Hutchinson C. A. W.
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