Abstract
Operational forecasts of precipitation amount are produced by a numerical scheme which uses the dew point depression as the moisture parameter. The onset of large scale precipitation occurs gradually when the dew point depression decreases below a threshold value. Small scale precipitation is divided into several meteorological components and each of these is parameterized separately. Improvements were recently obtained by reducing the horizontal grid spacing from 381 km to 190.5 km.
DOI: https://doi.org/10.3402/tellusa.v25i1.9643 | Journal eISSN: 3035-9554
Language: English
Page range: 43 - 57
Submitted on: Jul 7, 1972
Published on: Jan 1, 1973
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1973 David Davies, Marvin P. Olson, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.
