Abstract
Abstract Observations and measurements of the bright band in radar echoes are presented. It is shown that the theory of coalescence and melting of snowflakes provides an adequate explanation of the phenomenon.
Cite
CITATION STYLE
APA
Austin, P. M., & Bemis, A. C. (1950). A QUANTITATIVE STUDY OF THE “BRIGHT BAND” IN RADAR PRECIPITATION ECHOES. Journal of Meteorology, 7(2), 145–151. https://doi.org/10.1175/1520-0469(1950)007<0145:aqsotb>2.0.co;2
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.
Already have an account? Sign in
Sign up for free