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Precipitation and Streamflow of a Colorado Front Range Watershed (Classic Reprint)



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Precipitation and Streamflow of a Colorado Front Range Watershed (Classic Reprint) by Herbert W Berndt
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Excerpt from Precipitation and Streamflow of a Colorado Front Range Watershed Spring peak ows resulting from snowmelt occur with considerable regularity. Data indicate that these peaks are caused by melting snow on the slopes of the water shed below 8, 300 feet. Snowmelt water from elevations above 8, 300 feet contributes less to peak discharge and more to the characteristically high May ows, which make up approximately 40 percent of the total yield annually. During summer, streamflow is almost entirely from ground-water reserve. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at 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."
Release date Australia
November 17th, 2016
Country of Publication
United States
, black & white illustrations
Forgotten Books
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