Publisher's Synopsis
Excerpt from Precipitation Characteristics of Summer Storms at High-Elevation Stations in Utah
This paper presents the results of data analyses for 25 precipitation intensity stations on two study areas in central and north-central Utah located at elevations between 4, 350 and 10, 150 feet m. S. 1. All data were collected during the period May 1 to October 31. Each station has 10 or more years of record; one station has 30 years of record. The'following analyses were made: (1) Record consistency; (2) definition of local precipi tation zones; (3) intensity - duration - frequency characteristics; (4) 24-hour depths; (5) monthly depths and number of storms; (6) storm occurrence by hour of the day; and (7) storm occurrence by storm duration. The precipi tation zone between and feet m. S. L. Is expected to receive the greatest rainfall intensities. There is a trend toward reduced intensities with increasing elevation but the trend is not uniform. However, those pre cipitation zones that receive the most intense rainfall do not coincide with those zones receiving the greatest depth of rainfall. Generally, rainfall depth increases with elevation, but on one study area the zone that received the greatest depth was not the highest elevation zone. A marked difference in the distribution of storm occurrence by hour between the two study areas is attributed to differences in storm type and to differences in the principal source of summer moisture. Average storm length varies inversely with elevation.
About the Publisher
Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.com
This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works.
