Internal atmospheric gravity waves near the coast of Antarctica
Abstract Two gravity wave events as observed at Georg von Neumayer Station in Antarctica are described and analyzed. Wind and temperature are recorded at a meteorological tower. Surface pressure time series are available from four sites so that rather exact evaluations of phase speed and wavelength...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Egger, J. [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
1993 |
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| Schlagwörter: |
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| Anmerkung: |
© Kluwer Academic Publishers 1993 |
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| Übergeordnetes Werk: |
Enthalten in: Boundary layer meteorology - Kluwer Academic Publishers, 1970, 66(1993), 1-2 vom: Okt., Seite 1-17 |
|---|---|
| Übergeordnetes Werk: |
volume:66 ; year:1993 ; number:1-2 ; month:10 ; pages:1-17 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF00705457 |
|---|
| Katalog-ID: |
OLC2060937957 |
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| 520 | |a Abstract Two gravity wave events as observed at Georg von Neumayer Station in Antarctica are described and analyzed. Wind and temperature are recorded at a meteorological tower. Surface pressure time series are available from four sites so that rather exact evaluations of phase speed and wavelength are possible. Radiosonde ascents provide information on the structure of the atmosphere above the boundary layer. The pressure traces of both events are dominated by sinusoidal oscillations with a well defined frequency. Related variations of wind and temperature are small during the first event (16 July 1986) as are those of temperature on 29 September 1986. However, wind oscillations are quite large during this second event. An attempt is made to interpret the data in the light of linear gravity theory. It is found that linear gravity waves of frequency and phase speed as observed were able to propagate throughout the troposphere on 16 July. We conjecture on the basis of linear theory that the wave of 29 September was propagating on the surface inversion. | ||
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10.1007/BF00705457 doi (DE-627)OLC2060937957 (DE-He213)BF00705457-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Egger, J. verfasserin aut Internal atmospheric gravity waves near the coast of Antarctica 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1993 Abstract Two gravity wave events as observed at Georg von Neumayer Station in Antarctica are described and analyzed. Wind and temperature are recorded at a meteorological tower. Surface pressure time series are available from four sites so that rather exact evaluations of phase speed and wavelength are possible. Radiosonde ascents provide information on the structure of the atmosphere above the boundary layer. The pressure traces of both events are dominated by sinusoidal oscillations with a well defined frequency. Related variations of wind and temperature are small during the first event (16 July 1986) as are those of temperature on 29 September 1986. However, wind oscillations are quite large during this second event. An attempt is made to interpret the data in the light of linear gravity theory. It is found that linear gravity waves of frequency and phase speed as observed were able to propagate throughout the troposphere on 16 July. We conjecture on the basis of linear theory that the wave of 29 September was propagating on the surface inversion. Boundary Layer Gravity Wave Phase Speed Gravity Theory Wave Event Wamser, C. aut Kottmeier, C. aut Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 66(1993), 1-2 vom: Okt., Seite 1-17 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:66 year:1993 number:1-2 month:10 pages:1-17 https://doi.org/10.1007/BF00705457 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 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_4313 GBV_ILN_4700 AR 66 1993 1-2 10 1-17 |
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10.1007/BF00705457 doi (DE-627)OLC2060937957 (DE-He213)BF00705457-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Egger, J. verfasserin aut Internal atmospheric gravity waves near the coast of Antarctica 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1993 Abstract Two gravity wave events as observed at Georg von Neumayer Station in Antarctica are described and analyzed. Wind and temperature are recorded at a meteorological tower. Surface pressure time series are available from four sites so that rather exact evaluations of phase speed and wavelength are possible. Radiosonde ascents provide information on the structure of the atmosphere above the boundary layer. The pressure traces of both events are dominated by sinusoidal oscillations with a well defined frequency. Related variations of wind and temperature are small during the first event (16 July 1986) as are those of temperature on 29 September 1986. However, wind oscillations are quite large during this second event. An attempt is made to interpret the data in the light of linear gravity theory. It is found that linear gravity waves of frequency and phase speed as observed were able to propagate throughout the troposphere on 16 July. We conjecture on the basis of linear theory that the wave of 29 September was propagating on the surface inversion. Boundary Layer Gravity Wave Phase Speed Gravity Theory Wave Event Wamser, C. aut Kottmeier, C. aut Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 66(1993), 1-2 vom: Okt., Seite 1-17 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:66 year:1993 number:1-2 month:10 pages:1-17 https://doi.org/10.1007/BF00705457 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 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_4313 GBV_ILN_4700 AR 66 1993 1-2 10 1-17 |
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10.1007/BF00705457 doi (DE-627)OLC2060937957 (DE-He213)BF00705457-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Egger, J. verfasserin aut Internal atmospheric gravity waves near the coast of Antarctica 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1993 Abstract Two gravity wave events as observed at Georg von Neumayer Station in Antarctica are described and analyzed. Wind and temperature are recorded at a meteorological tower. Surface pressure time series are available from four sites so that rather exact evaluations of phase speed and wavelength are possible. Radiosonde ascents provide information on the structure of the atmosphere above the boundary layer. The pressure traces of both events are dominated by sinusoidal oscillations with a well defined frequency. Related variations of wind and temperature are small during the first event (16 July 1986) as are those of temperature on 29 September 1986. However, wind oscillations are quite large during this second event. An attempt is made to interpret the data in the light of linear gravity theory. It is found that linear gravity waves of frequency and phase speed as observed were able to propagate throughout the troposphere on 16 July. We conjecture on the basis of linear theory that the wave of 29 September was propagating on the surface inversion. Boundary Layer Gravity Wave Phase Speed Gravity Theory Wave Event Wamser, C. aut Kottmeier, C. aut Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 66(1993), 1-2 vom: Okt., Seite 1-17 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:66 year:1993 number:1-2 month:10 pages:1-17 https://doi.org/10.1007/BF00705457 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 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_4313 GBV_ILN_4700 AR 66 1993 1-2 10 1-17 |
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10.1007/BF00705457 doi (DE-627)OLC2060937957 (DE-He213)BF00705457-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Egger, J. verfasserin aut Internal atmospheric gravity waves near the coast of Antarctica 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1993 Abstract Two gravity wave events as observed at Georg von Neumayer Station in Antarctica are described and analyzed. Wind and temperature are recorded at a meteorological tower. Surface pressure time series are available from four sites so that rather exact evaluations of phase speed and wavelength are possible. Radiosonde ascents provide information on the structure of the atmosphere above the boundary layer. The pressure traces of both events are dominated by sinusoidal oscillations with a well defined frequency. Related variations of wind and temperature are small during the first event (16 July 1986) as are those of temperature on 29 September 1986. However, wind oscillations are quite large during this second event. An attempt is made to interpret the data in the light of linear gravity theory. It is found that linear gravity waves of frequency and phase speed as observed were able to propagate throughout the troposphere on 16 July. We conjecture on the basis of linear theory that the wave of 29 September was propagating on the surface inversion. Boundary Layer Gravity Wave Phase Speed Gravity Theory Wave Event Wamser, C. aut Kottmeier, C. aut Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 66(1993), 1-2 vom: Okt., Seite 1-17 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:66 year:1993 number:1-2 month:10 pages:1-17 https://doi.org/10.1007/BF00705457 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 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_4313 GBV_ILN_4700 AR 66 1993 1-2 10 1-17 |
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10.1007/BF00705457 doi (DE-627)OLC2060937957 (DE-He213)BF00705457-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Egger, J. verfasserin aut Internal atmospheric gravity waves near the coast of Antarctica 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1993 Abstract Two gravity wave events as observed at Georg von Neumayer Station in Antarctica are described and analyzed. Wind and temperature are recorded at a meteorological tower. Surface pressure time series are available from four sites so that rather exact evaluations of phase speed and wavelength are possible. Radiosonde ascents provide information on the structure of the atmosphere above the boundary layer. The pressure traces of both events are dominated by sinusoidal oscillations with a well defined frequency. Related variations of wind and temperature are small during the first event (16 July 1986) as are those of temperature on 29 September 1986. However, wind oscillations are quite large during this second event. An attempt is made to interpret the data in the light of linear gravity theory. It is found that linear gravity waves of frequency and phase speed as observed were able to propagate throughout the troposphere on 16 July. We conjecture on the basis of linear theory that the wave of 29 September was propagating on the surface inversion. Boundary Layer Gravity Wave Phase Speed Gravity Theory Wave Event Wamser, C. aut Kottmeier, C. aut Enthalten in Boundary layer meteorology Kluwer Academic Publishers, 1970 66(1993), 1-2 vom: Okt., Seite 1-17 (DE-627)129610410 (DE-600)242879-9 (DE-576)015105679 0006-8314 nnns volume:66 year:1993 number:1-2 month:10 pages:1-17 https://doi.org/10.1007/BF00705457 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 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_4313 GBV_ILN_4700 AR 66 1993 1-2 10 1-17 |
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Internal atmospheric gravity waves near the coast of Antarctica |
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Internal atmospheric gravity waves near the coast of Antarctica |
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Egger, J. |
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Boundary layer meteorology |
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Boundary layer meteorology |
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1993 |
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Egger, J. Wamser, C. Kottmeier, C. |
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Egger, J. |
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10.1007/BF00705457 |
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internal atmospheric gravity waves near the coast of antarctica |
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Internal atmospheric gravity waves near the coast of Antarctica |
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Abstract Two gravity wave events as observed at Georg von Neumayer Station in Antarctica are described and analyzed. Wind and temperature are recorded at a meteorological tower. Surface pressure time series are available from four sites so that rather exact evaluations of phase speed and wavelength are possible. Radiosonde ascents provide information on the structure of the atmosphere above the boundary layer. The pressure traces of both events are dominated by sinusoidal oscillations with a well defined frequency. Related variations of wind and temperature are small during the first event (16 July 1986) as are those of temperature on 29 September 1986. However, wind oscillations are quite large during this second event. An attempt is made to interpret the data in the light of linear gravity theory. It is found that linear gravity waves of frequency and phase speed as observed were able to propagate throughout the troposphere on 16 July. We conjecture on the basis of linear theory that the wave of 29 September was propagating on the surface inversion. © Kluwer Academic Publishers 1993 |
| abstractGer |
Abstract Two gravity wave events as observed at Georg von Neumayer Station in Antarctica are described and analyzed. Wind and temperature are recorded at a meteorological tower. Surface pressure time series are available from four sites so that rather exact evaluations of phase speed and wavelength are possible. Radiosonde ascents provide information on the structure of the atmosphere above the boundary layer. The pressure traces of both events are dominated by sinusoidal oscillations with a well defined frequency. Related variations of wind and temperature are small during the first event (16 July 1986) as are those of temperature on 29 September 1986. However, wind oscillations are quite large during this second event. An attempt is made to interpret the data in the light of linear gravity theory. It is found that linear gravity waves of frequency and phase speed as observed were able to propagate throughout the troposphere on 16 July. We conjecture on the basis of linear theory that the wave of 29 September was propagating on the surface inversion. © Kluwer Academic Publishers 1993 |
| abstract_unstemmed |
Abstract Two gravity wave events as observed at Georg von Neumayer Station in Antarctica are described and analyzed. Wind and temperature are recorded at a meteorological tower. Surface pressure time series are available from four sites so that rather exact evaluations of phase speed and wavelength are possible. Radiosonde ascents provide information on the structure of the atmosphere above the boundary layer. The pressure traces of both events are dominated by sinusoidal oscillations with a well defined frequency. Related variations of wind and temperature are small during the first event (16 July 1986) as are those of temperature on 29 September 1986. However, wind oscillations are quite large during this second event. An attempt is made to interpret the data in the light of linear gravity theory. It is found that linear gravity waves of frequency and phase speed as observed were able to propagate throughout the troposphere on 16 July. We conjecture on the basis of linear theory that the wave of 29 September was propagating on the surface inversion. © Kluwer Academic Publishers 1993 |
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Internal atmospheric gravity waves near the coast of Antarctica |
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