Hydroclimatology of the US Intermountain West

The semi-arid US Intermountain West is characterized by complex hydroclimatic variability, influenced both by topography and by atmosphere and ocean processes operating over a large range of time and space scales. Understanding climate–hydrology interactions has become increasingly important as dema...

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Published in:Progress in Physical Geography: Earth and Environment
Main Author: Wise, Erika K.
Format: Article in Journal/Newspaper
Language:English
Published: SAGE Publications 2012
Subjects:
Online Access:http://dx.doi.org/10.1177/0309133312446538
http://journals.sagepub.com/doi/pdf/10.1177/0309133312446538
http://journals.sagepub.com/doi/full-xml/10.1177/0309133312446538
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spelling crsagepubl:10.1177/0309133312446538 2024-06-23T07:45:14+00:00 Hydroclimatology of the US Intermountain West Wise, Erika K. 2012 http://dx.doi.org/10.1177/0309133312446538 http://journals.sagepub.com/doi/pdf/10.1177/0309133312446538 http://journals.sagepub.com/doi/full-xml/10.1177/0309133312446538 en eng SAGE Publications http://journals.sagepub.com/page/policies/text-and-data-mining-license Progress in Physical Geography: Earth and Environment volume 36, issue 4, page 458-479 ISSN 0309-1333 1477-0296 journal-article 2012 crsagepubl https://doi.org/10.1177/0309133312446538 2024-06-11T04:30:49Z The semi-arid US Intermountain West is characterized by complex hydroclimatic variability, influenced both by topography and by atmosphere and ocean processes operating over a large range of time and space scales. Understanding climate–hydrology interactions has become increasingly important as demands on water resources grow from both within and beyond the region, particularly in light of projected climate changes. This paper reviews key atmospheric and oceanic controls that impact the Intermountain West’s water supply, how those controls vary over multiple timescales, the tree-ring record of hydroclimatic variability in the region, projected climate change impacts, and research needs for the future. Water availability in the Intermountain West is largely influenced by interrelated atmospheric features that include the strength and position of the Pacific subtropical high, the intensity and geographic location of the Aleutian low, the latitude of the westerly storm track, and teleconnections such as the Pacific North American pattern and the El Niño−Southern Oscillation system. The tree-ring record of pre-instrumental conditions in the Intermountain West indicates that there have been droughts in the past that were more severe than those experienced in the historical record. Climate model projections of future moisture-related changes, including decreased snowpack and changing seasonality of precipitation, may exacerbate strain on the region’s water supply. Advances in climate modeling and in our understanding of climate variability over multiple time and space scales would improve capacity for water resource management in the Intermountain West. Article in Journal/Newspaper aleutian low SAGE Publications Pacific Progress in Physical Geography: Earth and Environment 36 4 458 479
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description The semi-arid US Intermountain West is characterized by complex hydroclimatic variability, influenced both by topography and by atmosphere and ocean processes operating over a large range of time and space scales. Understanding climate–hydrology interactions has become increasingly important as demands on water resources grow from both within and beyond the region, particularly in light of projected climate changes. This paper reviews key atmospheric and oceanic controls that impact the Intermountain West’s water supply, how those controls vary over multiple timescales, the tree-ring record of hydroclimatic variability in the region, projected climate change impacts, and research needs for the future. Water availability in the Intermountain West is largely influenced by interrelated atmospheric features that include the strength and position of the Pacific subtropical high, the intensity and geographic location of the Aleutian low, the latitude of the westerly storm track, and teleconnections such as the Pacific North American pattern and the El Niño−Southern Oscillation system. The tree-ring record of pre-instrumental conditions in the Intermountain West indicates that there have been droughts in the past that were more severe than those experienced in the historical record. Climate model projections of future moisture-related changes, including decreased snowpack and changing seasonality of precipitation, may exacerbate strain on the region’s water supply. Advances in climate modeling and in our understanding of climate variability over multiple time and space scales would improve capacity for water resource management in the Intermountain West.
format Article in Journal/Newspaper
author Wise, Erika K.
spellingShingle Wise, Erika K.
Hydroclimatology of the US Intermountain West
author_facet Wise, Erika K.
author_sort Wise, Erika K.
title Hydroclimatology of the US Intermountain West
title_short Hydroclimatology of the US Intermountain West
title_full Hydroclimatology of the US Intermountain West
title_fullStr Hydroclimatology of the US Intermountain West
title_full_unstemmed Hydroclimatology of the US Intermountain West
title_sort hydroclimatology of the us intermountain west
publisher SAGE Publications
publishDate 2012
url http://dx.doi.org/10.1177/0309133312446538
http://journals.sagepub.com/doi/pdf/10.1177/0309133312446538
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op_source Progress in Physical Geography: Earth and Environment
volume 36, issue 4, page 458-479
ISSN 0309-1333 1477-0296
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op_doi https://doi.org/10.1177/0309133312446538
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