Abstract
The most important advantage of using radar for precipitation measurements is the coverage of a large area with high spatial and temporal resolution from a single point and in real time. Furthermore, the three-dimensional picture of the weather situation can be extended over a very large area by compositing data from several radars. However, we have not been able until recently to make measurements over a large area with an accuracy acceptable for hydrological applications.
Cite
CITATION STYLE
Joss, J., Waldvogel, A., & Collier, C. G. (1990). Precipitation Measurement and Hydrology. In Radar in Meteorology (pp. 577–606). American Meteorological Society. https://doi.org/10.1007/978-1-935704-15-7_39
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