The behavior of vertically integrated boundary-layer winds
Abstract This research provides a study of the behavior of vertically integrated boundary-layer winds (IBLWs). This information should be helpful for both theoretical and practical applications, e.g., boundary-layer parameterization in general circulation models, air pollution models, and low-level...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Cormier, René V. [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
1975 |
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| Schlagwörter: |
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| Anmerkung: |
© D. Reidel Publishing Company 1975 |
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| Übergeordnetes Werk: |
Enthalten in: Boundary layer meteorology - Kluwer Academic Publishers, 1970, 9(1975), 3 vom: Nov., Seite 315-324 |
|---|---|
| Übergeordnetes Werk: |
volume:9 ; year:1975 ; number:3 ; month:11 ; pages:315-324 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF00230773 |
|---|
| Katalog-ID: |
OLC2060920043 |
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| 520 | |a Abstract This research provides a study of the behavior of vertically integrated boundary-layer winds (IBLWs). This information should be helpful for both theoretical and practical applications, e.g., boundary-layer parameterization in general circulation models, air pollution models, and low-level parachuting operations. The study concerned itself with winds integrated up to a height of 300 m in the United States. The only data suitable for studying the behavior of IBLWs for such heights were measurements taken on tall towers. An extensive search indicated that data were readily available from only four towers instrumented to or above 300 m. These were located in rural locations in Texas, Oklahoma, Nevada, and South Carolina. At each location, means and coefficients of variation of IBLWs were computed, plotted as a function of time since sunrise/sunset, and compared. The research shows that IBLWs may differ appreciably in magnitude at different locations; may have considerable universality in behavior, and may also be ‘regionally’ dependent; and that IBLWs have a pronounced diurnal variation linked to sunrise/sunset time. | ||
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10.1007/BF00230773 doi (DE-627)OLC2060920043 (DE-He213)BF00230773-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Cormier, René V. verfasserin aut The behavior of vertically integrated boundary-layer winds 1975 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1975 Abstract This research provides a study of the behavior of vertically integrated boundary-layer winds (IBLWs). This information should be helpful for both theoretical and practical applications, e.g., boundary-layer parameterization in general circulation models, air pollution models, and low-level parachuting operations. The study concerned itself with winds integrated up to a height of 300 m in the United States. The only data suitable for studying the behavior of IBLWs for such heights were measurements taken on tall towers. An extensive search indicated that data were readily available from only four towers instrumented to or above 300 m. These were located in rural locations in Texas, Oklahoma, Nevada, and South Carolina. At each location, means and coefficients of variation of IBLWs were computed, plotted as a function of time since sunrise/sunset, and compared. The research shows that IBLWs may differ appreciably in magnitude at different locations; may have considerable universality in behavior, and may also be ‘regionally’ dependent; and that IBLWs have a pronounced diurnal variation linked to sunrise/sunset time. United States Diurnal Variation Circulation Model General Circulation General Circulation Model Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 9(1975), 3 vom: Nov., Seite 315-324 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:9 year:1975 number:3 month:11 pages:315-324 https://doi.org/10.1007/BF00230773 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_154 GBV_ILN_201 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2012 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4311 AR 9 1975 3 11 315-324 |
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10.1007/BF00230773 doi (DE-627)OLC2060920043 (DE-He213)BF00230773-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Cormier, René V. verfasserin aut The behavior of vertically integrated boundary-layer winds 1975 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1975 Abstract This research provides a study of the behavior of vertically integrated boundary-layer winds (IBLWs). This information should be helpful for both theoretical and practical applications, e.g., boundary-layer parameterization in general circulation models, air pollution models, and low-level parachuting operations. The study concerned itself with winds integrated up to a height of 300 m in the United States. The only data suitable for studying the behavior of IBLWs for such heights were measurements taken on tall towers. An extensive search indicated that data were readily available from only four towers instrumented to or above 300 m. These were located in rural locations in Texas, Oklahoma, Nevada, and South Carolina. At each location, means and coefficients of variation of IBLWs were computed, plotted as a function of time since sunrise/sunset, and compared. The research shows that IBLWs may differ appreciably in magnitude at different locations; may have considerable universality in behavior, and may also be ‘regionally’ dependent; and that IBLWs have a pronounced diurnal variation linked to sunrise/sunset time. United States Diurnal Variation Circulation Model General Circulation General Circulation Model Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 9(1975), 3 vom: Nov., Seite 315-324 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:9 year:1975 number:3 month:11 pages:315-324 https://doi.org/10.1007/BF00230773 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_154 GBV_ILN_201 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2012 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4311 AR 9 1975 3 11 315-324 |
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10.1007/BF00230773 doi (DE-627)OLC2060920043 (DE-He213)BF00230773-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Cormier, René V. verfasserin aut The behavior of vertically integrated boundary-layer winds 1975 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1975 Abstract This research provides a study of the behavior of vertically integrated boundary-layer winds (IBLWs). This information should be helpful for both theoretical and practical applications, e.g., boundary-layer parameterization in general circulation models, air pollution models, and low-level parachuting operations. The study concerned itself with winds integrated up to a height of 300 m in the United States. The only data suitable for studying the behavior of IBLWs for such heights were measurements taken on tall towers. An extensive search indicated that data were readily available from only four towers instrumented to or above 300 m. These were located in rural locations in Texas, Oklahoma, Nevada, and South Carolina. At each location, means and coefficients of variation of IBLWs were computed, plotted as a function of time since sunrise/sunset, and compared. The research shows that IBLWs may differ appreciably in magnitude at different locations; may have considerable universality in behavior, and may also be ‘regionally’ dependent; and that IBLWs have a pronounced diurnal variation linked to sunrise/sunset time. United States Diurnal Variation Circulation Model General Circulation General Circulation Model Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 9(1975), 3 vom: Nov., Seite 315-324 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:9 year:1975 number:3 month:11 pages:315-324 https://doi.org/10.1007/BF00230773 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_154 GBV_ILN_201 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2012 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4311 AR 9 1975 3 11 315-324 |
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10.1007/BF00230773 doi (DE-627)OLC2060920043 (DE-He213)BF00230773-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Cormier, René V. verfasserin aut The behavior of vertically integrated boundary-layer winds 1975 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1975 Abstract This research provides a study of the behavior of vertically integrated boundary-layer winds (IBLWs). This information should be helpful for both theoretical and practical applications, e.g., boundary-layer parameterization in general circulation models, air pollution models, and low-level parachuting operations. The study concerned itself with winds integrated up to a height of 300 m in the United States. The only data suitable for studying the behavior of IBLWs for such heights were measurements taken on tall towers. An extensive search indicated that data were readily available from only four towers instrumented to or above 300 m. These were located in rural locations in Texas, Oklahoma, Nevada, and South Carolina. At each location, means and coefficients of variation of IBLWs were computed, plotted as a function of time since sunrise/sunset, and compared. The research shows that IBLWs may differ appreciably in magnitude at different locations; may have considerable universality in behavior, and may also be ‘regionally’ dependent; and that IBLWs have a pronounced diurnal variation linked to sunrise/sunset time. United States Diurnal Variation Circulation Model General Circulation General Circulation Model Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 9(1975), 3 vom: Nov., Seite 315-324 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:9 year:1975 number:3 month:11 pages:315-324 https://doi.org/10.1007/BF00230773 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_154 GBV_ILN_201 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2012 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4311 AR 9 1975 3 11 315-324 |
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10.1007/BF00230773 doi (DE-627)OLC2060920043 (DE-He213)BF00230773-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Cormier, René V. verfasserin aut The behavior of vertically integrated boundary-layer winds 1975 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1975 Abstract This research provides a study of the behavior of vertically integrated boundary-layer winds (IBLWs). This information should be helpful for both theoretical and practical applications, e.g., boundary-layer parameterization in general circulation models, air pollution models, and low-level parachuting operations. The study concerned itself with winds integrated up to a height of 300 m in the United States. The only data suitable for studying the behavior of IBLWs for such heights were measurements taken on tall towers. An extensive search indicated that data were readily available from only four towers instrumented to or above 300 m. These were located in rural locations in Texas, Oklahoma, Nevada, and South Carolina. At each location, means and coefficients of variation of IBLWs were computed, plotted as a function of time since sunrise/sunset, and compared. The research shows that IBLWs may differ appreciably in magnitude at different locations; may have considerable universality in behavior, and may also be ‘regionally’ dependent; and that IBLWs have a pronounced diurnal variation linked to sunrise/sunset time. United States Diurnal Variation Circulation Model General Circulation General Circulation Model Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 9(1975), 3 vom: Nov., Seite 315-324 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:9 year:1975 number:3 month:11 pages:315-324 https://doi.org/10.1007/BF00230773 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_154 GBV_ILN_201 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2012 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4305 GBV_ILN_4307 GBV_ILN_4311 AR 9 1975 3 11 315-324 |
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The behavior of vertically integrated boundary-layer winds |
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Cormier, René V. |
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Boundary layer meteorology |
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Boundary layer meteorology |
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eng |
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500 - Science |
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1975 |
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315 |
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Cormier, René V. |
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9 |
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Cormier, René V. |
| doi_str_mv |
10.1007/BF00230773 |
| dewey-full |
550 |
| title_sort |
the behavior of vertically integrated boundary-layer winds |
| title_auth |
The behavior of vertically integrated boundary-layer winds |
| abstract |
Abstract This research provides a study of the behavior of vertically integrated boundary-layer winds (IBLWs). This information should be helpful for both theoretical and practical applications, e.g., boundary-layer parameterization in general circulation models, air pollution models, and low-level parachuting operations. The study concerned itself with winds integrated up to a height of 300 m in the United States. The only data suitable for studying the behavior of IBLWs for such heights were measurements taken on tall towers. An extensive search indicated that data were readily available from only four towers instrumented to or above 300 m. These were located in rural locations in Texas, Oklahoma, Nevada, and South Carolina. At each location, means and coefficients of variation of IBLWs were computed, plotted as a function of time since sunrise/sunset, and compared. The research shows that IBLWs may differ appreciably in magnitude at different locations; may have considerable universality in behavior, and may also be ‘regionally’ dependent; and that IBLWs have a pronounced diurnal variation linked to sunrise/sunset time. © D. Reidel Publishing Company 1975 |
| abstractGer |
Abstract This research provides a study of the behavior of vertically integrated boundary-layer winds (IBLWs). This information should be helpful for both theoretical and practical applications, e.g., boundary-layer parameterization in general circulation models, air pollution models, and low-level parachuting operations. The study concerned itself with winds integrated up to a height of 300 m in the United States. The only data suitable for studying the behavior of IBLWs for such heights were measurements taken on tall towers. An extensive search indicated that data were readily available from only four towers instrumented to or above 300 m. These were located in rural locations in Texas, Oklahoma, Nevada, and South Carolina. At each location, means and coefficients of variation of IBLWs were computed, plotted as a function of time since sunrise/sunset, and compared. The research shows that IBLWs may differ appreciably in magnitude at different locations; may have considerable universality in behavior, and may also be ‘regionally’ dependent; and that IBLWs have a pronounced diurnal variation linked to sunrise/sunset time. © D. Reidel Publishing Company 1975 |
| abstract_unstemmed |
Abstract This research provides a study of the behavior of vertically integrated boundary-layer winds (IBLWs). This information should be helpful for both theoretical and practical applications, e.g., boundary-layer parameterization in general circulation models, air pollution models, and low-level parachuting operations. The study concerned itself with winds integrated up to a height of 300 m in the United States. The only data suitable for studying the behavior of IBLWs for such heights were measurements taken on tall towers. An extensive search indicated that data were readily available from only four towers instrumented to or above 300 m. These were located in rural locations in Texas, Oklahoma, Nevada, and South Carolina. At each location, means and coefficients of variation of IBLWs were computed, plotted as a function of time since sunrise/sunset, and compared. The research shows that IBLWs may differ appreciably in magnitude at different locations; may have considerable universality in behavior, and may also be ‘regionally’ dependent; and that IBLWs have a pronounced diurnal variation linked to sunrise/sunset time. © D. Reidel Publishing Company 1975 |
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| title_short |
The behavior of vertically integrated boundary-layer winds |
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