Patterns of orographic uplift in the Sierra Nevada and their relationship to upper-level atmospheric circulation
We examine monthly and seasonal patterns of precipitation across various elevations of the eastern Central Valley of California and the Sierra Nevada. A measure of the strength of the orographic effect called the “precipitation ratio” is calculated, and we separate months into four groups based on being wet or dry and having low or high precipitation ratios. Using monthly maps of mean 700-mb height anomalies, we describe the northern hemisphere mid-tropospheric circulation patterns associated with each of the four groups. Wet months are associated with negative height anomalies over the eastern Pacific, as expected. However, the orientation of the trough is different for years with high and low precipitation ratios. Wet months with high ratios typically have circulation patterns factoring a west-southwest to east-northeast storm track from around the Hawaiian Islands to the Pacific Northwest of the United States. Wet months with low precipitation ratios are associated with a trough centered near the Aleutians and a northwest to southeast storm track. Dry months are marked by anticyclones in the Pacific, but this feature is more localized to the eastern Pacific for months with low precipitation ratios than for those with high ratios. Using precipitation gauge and snow course data from the American River and Truckee-Tahoe basins, we determined that the strength of the orographic effect on a seasonal basis is spatially coherent at low and high elevations and on opposite sides of the Sierra Nevada crestline.
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Format: | conference_item biblioteca |
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1993-03
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Subjects: | Atmospheric Sciences, PACLIM, |
Online Access: | http://hdl.handle.net/1834/30338 |
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dig-aquadocs-1834-303382021-06-25T03:06:55Z Patterns of orographic uplift in the Sierra Nevada and their relationship to upper-level atmospheric circulation Aguado, Edward Cayan, Dan Reece, Brian Riddle, Larry Atmospheric Sciences PACLIM We examine monthly and seasonal patterns of precipitation across various elevations of the eastern Central Valley of California and the Sierra Nevada. A measure of the strength of the orographic effect called the “precipitation ratio” is calculated, and we separate months into four groups based on being wet or dry and having low or high precipitation ratios. Using monthly maps of mean 700-mb height anomalies, we describe the northern hemisphere mid-tropospheric circulation patterns associated with each of the four groups. Wet months are associated with negative height anomalies over the eastern Pacific, as expected. However, the orientation of the trough is different for years with high and low precipitation ratios. Wet months with high ratios typically have circulation patterns factoring a west-southwest to east-northeast storm track from around the Hawaiian Islands to the Pacific Northwest of the United States. Wet months with low precipitation ratios are associated with a trough centered near the Aleutians and a northwest to southeast storm track. Dry months are marked by anticyclones in the Pacific, but this feature is more localized to the eastern Pacific for months with low precipitation ratios than for those with high ratios. Using precipitation gauge and snow course data from the American River and Truckee-Tahoe basins, we determined that the strength of the orographic effect on a seasonal basis is spatially coherent at low and high elevations and on opposite sides of the Sierra Nevada crestline. 2021-06-24T16:50:21Z 2021-06-24T16:50:21Z 1993-03 conference_item http://hdl.handle.net/1834/30338 en application/pdf application/pdf 153-163 http://aquaticcommons.org/id/eprint/14471 8 2014-02-14 01:28:56 14471 |
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Atmospheric Sciences PACLIM Atmospheric Sciences PACLIM Aguado, Edward Cayan, Dan Reece, Brian Riddle, Larry Patterns of orographic uplift in the Sierra Nevada and their relationship to upper-level atmospheric circulation |
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We examine monthly and seasonal patterns of precipitation across various elevations of the eastern Central Valley of California and the Sierra Nevada. A measure of the strength of the orographic effect called the “precipitation ratio” is calculated, and we separate months into four groups based on being wet or dry and having low or high precipitation ratios. Using monthly maps of mean 700-mb height anomalies, we describe the northern hemisphere mid-tropospheric circulation patterns associated with each of the four groups. Wet months are associated with negative height anomalies over the eastern Pacific, as expected. However, the orientation of the trough is different for years with high and low precipitation ratios. Wet months with high ratios typically have circulation patterns factoring a west-southwest to east-northeast storm track from around the Hawaiian Islands to the Pacific Northwest of the United States. Wet months with low precipitation ratios are associated with a trough centered near the Aleutians and a northwest to southeast storm track. Dry months are marked by anticyclones in the Pacific, but this feature is more localized to the eastern Pacific for months with low precipitation ratios than for those with high ratios. Using precipitation gauge and snow course data from the American River and Truckee-Tahoe basins, we determined that the strength of the orographic effect on a seasonal basis is spatially coherent at low and high elevations and on opposite sides of the Sierra Nevada crestline. |
format |
conference_item |
topic_facet |
Atmospheric Sciences PACLIM |
author |
Aguado, Edward Cayan, Dan Reece, Brian Riddle, Larry |
author_facet |
Aguado, Edward Cayan, Dan Reece, Brian Riddle, Larry |
author_sort |
Aguado, Edward |
title |
Patterns of orographic uplift in the Sierra Nevada and their relationship to upper-level atmospheric circulation |
title_short |
Patterns of orographic uplift in the Sierra Nevada and their relationship to upper-level atmospheric circulation |
title_full |
Patterns of orographic uplift in the Sierra Nevada and their relationship to upper-level atmospheric circulation |
title_fullStr |
Patterns of orographic uplift in the Sierra Nevada and their relationship to upper-level atmospheric circulation |
title_full_unstemmed |
Patterns of orographic uplift in the Sierra Nevada and their relationship to upper-level atmospheric circulation |
title_sort |
patterns of orographic uplift in the sierra nevada and their relationship to upper-level atmospheric circulation |
publishDate |
1993-03 |
url |
http://hdl.handle.net/1834/30338 |
work_keys_str_mv |
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1756078680074878976 |