The effect of decoupled low-level flow on winter orographic clouds in northern Colorado
(eBook)

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Published
Fort Collins, Colo. : Department of Atmospheric Science, Colorado State University, 1989.
Physical Desc
1 online resource (ix, 145 pages) : illustrations, maps.
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Format
eBook
Language
English

Notes

General Note
"May 1989."
Bibliography
Includes bibliographical references (pages 141-145).
Description
The results indicate that the presence of extensive low-level decoupled flow does indeed cause part of the orographic lift of the mountain barrier to be experienced upstream of the barrier. This changes the location of condensate production which in turn shifts precipitation upstream.
Additional Physical Form
Also available in print form.
Funding Information
Sponsored by National Science Foundation, grants,ATM-8109590,,ATM-8704776,,ATM-8813345.
Funding Information
Sponsored by the Colorado Experiment Station.

Citations

APA Citation, 7th Edition (style guide)

Peterson, T. C. (1989). The effect of decoupled low-level flow on winter orographic clouds in northern Colorado . Department of Atmospheric Science, Colorado State University.

Chicago / Turabian - Author Date Citation, 17th Edition (style guide)

Peterson, Thomas C. 1989. The Effect of Decoupled Low-level Flow On Winter Orographic Clouds in Northern Colorado. Department of Atmospheric Science, Colorado State University.

Chicago / Turabian - Humanities (Notes and Bibliography) Citation, 17th Edition (style guide)

Peterson, Thomas C. The Effect of Decoupled Low-level Flow On Winter Orographic Clouds in Northern Colorado Department of Atmospheric Science, Colorado State University, 1989.

MLA Citation, 9th Edition (style guide)

Peterson, Thomas C. The Effect of Decoupled Low-level Flow On Winter Orographic Clouds in Northern Colorado Department of Atmospheric Science, Colorado State University, 1989.

Note! Citations contain only title, author, edition, publisher, and year published. Citations should be used as a guideline and should be double checked for accuracy. Citation formats are based on standards as of August 2021.

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Grouped Work ID
ad3af63b-9591-4268-679e-9eead9bd501f-eng
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Grouped Work IDad3af63b-9591-4268-679e-9eead9bd501f-eng
Full titleeffect of decoupled low level flow on winter orographic clouds in northern colorado
Authorpeterson thomas c
Grouping Categorybook
Last Update2022-06-13 10:33:16AM
Last Indexed2024-03-29 02:20:12AM

Book Cover Information

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First DetectedJul 19, 2011 12:00:00 AM
Last File Modification TimeJul 31, 2021 04:33:43 AM

MARC Record

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520 |a The results indicate that the presence of extensive low-level decoupled flow does indeed cause part of the orographic lift of the mountain barrier to be experienced upstream of the barrier. This changes the location of condensate production which in turn shifts precipitation upstream.
530 |a Also available in print form.
536 |a Sponsored by National Science Foundation, grants|c ATM-8109590,|c ATM-8704776,|c ATM-8813345.
536 |a Sponsored by the Colorado Experiment Station.
650 0|a Orographic clouds.
650 0|a Cloud physics.
7102 |a National Science Foundation (U.S.)
7102 |a Colorado State University.|b Department of Atmospheric Science.
7102 |a Colorado Agricultural Experiment Station.
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