The atmospheric boundary layer over a wavy surface
Abstract The wavy area of north-west Bohemia (Czechoslovakia) is simulated by a cylindrical surface model. A curvilinear orthogonal system of coordinates along the model surface is introduced. The hydrodynamical equations of motion are transformed into this system of coordinates. By applying boundar...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Jaňour, Z. [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
1975 |
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| Schlagwörter: |
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| Anmerkung: |
© D. Reidel Publishing Company 1975 |
|---|
| Übergeordnetes Werk: |
Enthalten in: Boundary layer meteorology - Kluwer Academic Publishers, 1970, 9(1975), 1 vom: Aug., Seite 3-10 |
|---|---|
| Übergeordnetes Werk: |
volume:9 ; year:1975 ; number:1 ; month:08 ; pages:3-10 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF00232249 |
|---|
| Katalog-ID: |
OLC2060919894 |
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| 520 | |a Abstract The wavy area of north-west Bohemia (Czechoslovakia) is simulated by a cylindrical surface model. A curvilinear orthogonal system of coordinates along the model surface is introduced. The hydrodynamical equations of motion are transformed into this system of coordinates. By applying boundary-layer assumptions, the equations of motion for the atmospheric boundary layer (ABL) above the model are derived. The equations and boundary conditions show an equivalence of the ABL above the model with that above a flat surface with external pressure gradient. | ||
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10.1007/BF00232249 doi (DE-627)OLC2060919894 (DE-He213)BF00232249-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Jaňour, Z. verfasserin aut The atmospheric boundary layer over a wavy surface 1975 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1975 Abstract The wavy area of north-west Bohemia (Czechoslovakia) is simulated by a cylindrical surface model. A curvilinear orthogonal system of coordinates along the model surface is introduced. The hydrodynamical equations of motion are transformed into this system of coordinates. By applying boundary-layer assumptions, the equations of motion for the atmospheric boundary layer (ABL) above the model are derived. The equations and boundary conditions show an equivalence of the ABL above the model with that above a flat surface with external pressure gradient. Boundary Condition Boundary Layer Pressure Gradient Model Surface Flat Surface Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 9(1975), 1 vom: Aug., Seite 3-10 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:9 year:1975 number:1 month:08 pages:3-10 https://doi.org/10.1007/BF00232249 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 1 08 3-10 |
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10.1007/BF00232249 doi (DE-627)OLC2060919894 (DE-He213)BF00232249-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Jaňour, Z. verfasserin aut The atmospheric boundary layer over a wavy surface 1975 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1975 Abstract The wavy area of north-west Bohemia (Czechoslovakia) is simulated by a cylindrical surface model. A curvilinear orthogonal system of coordinates along the model surface is introduced. The hydrodynamical equations of motion are transformed into this system of coordinates. By applying boundary-layer assumptions, the equations of motion for the atmospheric boundary layer (ABL) above the model are derived. The equations and boundary conditions show an equivalence of the ABL above the model with that above a flat surface with external pressure gradient. Boundary Condition Boundary Layer Pressure Gradient Model Surface Flat Surface Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 9(1975), 1 vom: Aug., Seite 3-10 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:9 year:1975 number:1 month:08 pages:3-10 https://doi.org/10.1007/BF00232249 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 1 08 3-10 |
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10.1007/BF00232249 doi (DE-627)OLC2060919894 (DE-He213)BF00232249-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Jaňour, Z. verfasserin aut The atmospheric boundary layer over a wavy surface 1975 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1975 Abstract The wavy area of north-west Bohemia (Czechoslovakia) is simulated by a cylindrical surface model. A curvilinear orthogonal system of coordinates along the model surface is introduced. The hydrodynamical equations of motion are transformed into this system of coordinates. By applying boundary-layer assumptions, the equations of motion for the atmospheric boundary layer (ABL) above the model are derived. The equations and boundary conditions show an equivalence of the ABL above the model with that above a flat surface with external pressure gradient. Boundary Condition Boundary Layer Pressure Gradient Model Surface Flat Surface Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 9(1975), 1 vom: Aug., Seite 3-10 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:9 year:1975 number:1 month:08 pages:3-10 https://doi.org/10.1007/BF00232249 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 1 08 3-10 |
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10.1007/BF00232249 doi (DE-627)OLC2060919894 (DE-He213)BF00232249-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Jaňour, Z. verfasserin aut The atmospheric boundary layer over a wavy surface 1975 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1975 Abstract The wavy area of north-west Bohemia (Czechoslovakia) is simulated by a cylindrical surface model. A curvilinear orthogonal system of coordinates along the model surface is introduced. The hydrodynamical equations of motion are transformed into this system of coordinates. By applying boundary-layer assumptions, the equations of motion for the atmospheric boundary layer (ABL) above the model are derived. The equations and boundary conditions show an equivalence of the ABL above the model with that above a flat surface with external pressure gradient. Boundary Condition Boundary Layer Pressure Gradient Model Surface Flat Surface Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 9(1975), 1 vom: Aug., Seite 3-10 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:9 year:1975 number:1 month:08 pages:3-10 https://doi.org/10.1007/BF00232249 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 1 08 3-10 |
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10.1007/BF00232249 doi (DE-627)OLC2060919894 (DE-He213)BF00232249-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Jaňour, Z. verfasserin aut The atmospheric boundary layer over a wavy surface 1975 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1975 Abstract The wavy area of north-west Bohemia (Czechoslovakia) is simulated by a cylindrical surface model. A curvilinear orthogonal system of coordinates along the model surface is introduced. The hydrodynamical equations of motion are transformed into this system of coordinates. By applying boundary-layer assumptions, the equations of motion for the atmospheric boundary layer (ABL) above the model are derived. The equations and boundary conditions show an equivalence of the ABL above the model with that above a flat surface with external pressure gradient. Boundary Condition Boundary Layer Pressure Gradient Model Surface Flat Surface Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 9(1975), 1 vom: Aug., Seite 3-10 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:9 year:1975 number:1 month:08 pages:3-10 https://doi.org/10.1007/BF00232249 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 1 08 3-10 |
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Abstract The wavy area of north-west Bohemia (Czechoslovakia) is simulated by a cylindrical surface model. A curvilinear orthogonal system of coordinates along the model surface is introduced. The hydrodynamical equations of motion are transformed into this system of coordinates. By applying boundary-layer assumptions, the equations of motion for the atmospheric boundary layer (ABL) above the model are derived. The equations and boundary conditions show an equivalence of the ABL above the model with that above a flat surface with external pressure gradient. © D. Reidel Publishing Company 1975 |
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Abstract The wavy area of north-west Bohemia (Czechoslovakia) is simulated by a cylindrical surface model. A curvilinear orthogonal system of coordinates along the model surface is introduced. The hydrodynamical equations of motion are transformed into this system of coordinates. By applying boundary-layer assumptions, the equations of motion for the atmospheric boundary layer (ABL) above the model are derived. The equations and boundary conditions show an equivalence of the ABL above the model with that above a flat surface with external pressure gradient. © D. Reidel Publishing Company 1975 |
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Abstract The wavy area of north-west Bohemia (Czechoslovakia) is simulated by a cylindrical surface model. A curvilinear orthogonal system of coordinates along the model surface is introduced. The hydrodynamical equations of motion are transformed into this system of coordinates. By applying boundary-layer assumptions, the equations of motion for the atmospheric boundary layer (ABL) above the model are derived. The equations and boundary conditions show an equivalence of the ABL above the model with that above a flat surface with external pressure gradient. © D. Reidel Publishing Company 1975 |
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