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Excerpt from Precipitation and Streamflow of a Colorado Front Range Watershed
Spring peak flows 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 flows, which make up approximately 40 percent of the total yield annually. During summer, streamflow is almost entirely from ground-water reserve.
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Precipitation and Streamflow of a Colorado Front Range Watershed
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Paperback. Zustand: New. Print on Demand. This book delves into the fascinating subject of a Colorado watershed's intricate relationship with precipitation and streamflow, shedding light on how these elements interact and shape the region's water dynamics. The author, an expert in the field, draws upon years of meticulous research and data analysis to provide a comprehensive understanding of the watershed's unique characteristics and behaviors. The book explores the influence of diverse factors such as topography, soil composition, vegetation, and climate on the water cycle, revealing the intricate interplay between these elements and their profound impact on the watershed's hydrology. Through detailed examination of precipitation patterns, streamflow variations, and sediment production, the author unveils the intricate connections between the physical environment and the movement of water. This provides valuable insights into the delicate balance of a watershed's ecosystem, highlighting the importance of preserving and managing these natural resources for future generations. This book is a reproduction of an important historical work, digitally reconstructed using state-of-the-art technology to preserve the original format. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in the book. print-on-demand item. Bestandsnummer des Verkäufers 9781334307324_0
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