Drift of large-scale hot thermals in stratified air flows
Abstract A difference method developed for the calculation of the three-dimensional unsteady flows of a viscous heat-conducting gas is used to investigate the influence of a horizontal wind, stratified with respect to height, on the motion of the eruption clouds of a volcano. It is shown that as the...
Ausführliche Beschreibung
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1984 |
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| Umfang: |
3 |
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| Reproduktion: |
Springer Online Journal Archives 1860-2002 |
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| Übergeordnetes Werk: |
in: Fluid dynamics - 1966, 19(1984) vom: Juni, Seite 1012-1014 |
| Übergeordnetes Werk: |
volume:19 ; year:1984 ; month:06 ; pages:1012-1014 ; extent:3 |
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| 520 | |a Abstract A difference method developed for the calculation of the three-dimensional unsteady flows of a viscous heat-conducting gas is used to investigate the influence of a horizontal wind, stratified with respect to height, on the motion of the eruption clouds of a volcano. It is shown that as the intensity of the air flow rises and its stratification increases the rate of ascent of the thermal decreases. Data are obtained for the features of the motion of the vortex rings formed. | ||
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(DE-627)NLEJ190543086 DE-627 ger DE-627 rakwb eng Drift of large-scale hot thermals in stratified air flows 1984 3 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract A difference method developed for the calculation of the three-dimensional unsteady flows of a viscous heat-conducting gas is used to investigate the influence of a horizontal wind, stratified with respect to height, on the motion of the eruption clouds of a volcano. It is shown that as the intensity of the air flow rises and its stratification increases the rate of ascent of the thermal decreases. Data are obtained for the features of the motion of the vortex rings formed. Springer Online Journal Archives 1860-2002 Andrushchenko, V. A. oth Chudov, L. A. oth in Fluid dynamics 1966 19(1984) vom: Juni, Seite 1012-1014 (DE-627)NLEJ188992693 (DE-600)2039450-0 1573-8507 nnns volume:19 year:1984 month:06 pages:1012-1014 extent:3 http://dx.doi.org/10.1007/BF01411597 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 19 1984 6 1012-1014 3 |
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(DE-627)NLEJ190543086 DE-627 ger DE-627 rakwb eng Drift of large-scale hot thermals in stratified air flows 1984 3 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract A difference method developed for the calculation of the three-dimensional unsteady flows of a viscous heat-conducting gas is used to investigate the influence of a horizontal wind, stratified with respect to height, on the motion of the eruption clouds of a volcano. It is shown that as the intensity of the air flow rises and its stratification increases the rate of ascent of the thermal decreases. Data are obtained for the features of the motion of the vortex rings formed. Springer Online Journal Archives 1860-2002 Andrushchenko, V. A. oth Chudov, L. A. oth in Fluid dynamics 1966 19(1984) vom: Juni, Seite 1012-1014 (DE-627)NLEJ188992693 (DE-600)2039450-0 1573-8507 nnns volume:19 year:1984 month:06 pages:1012-1014 extent:3 http://dx.doi.org/10.1007/BF01411597 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 19 1984 6 1012-1014 3 |
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(DE-627)NLEJ190543086 DE-627 ger DE-627 rakwb eng Drift of large-scale hot thermals in stratified air flows 1984 3 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract A difference method developed for the calculation of the three-dimensional unsteady flows of a viscous heat-conducting gas is used to investigate the influence of a horizontal wind, stratified with respect to height, on the motion of the eruption clouds of a volcano. It is shown that as the intensity of the air flow rises and its stratification increases the rate of ascent of the thermal decreases. Data are obtained for the features of the motion of the vortex rings formed. Springer Online Journal Archives 1860-2002 Andrushchenko, V. A. oth Chudov, L. A. oth in Fluid dynamics 1966 19(1984) vom: Juni, Seite 1012-1014 (DE-627)NLEJ188992693 (DE-600)2039450-0 1573-8507 nnns volume:19 year:1984 month:06 pages:1012-1014 extent:3 http://dx.doi.org/10.1007/BF01411597 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 19 1984 6 1012-1014 3 |
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(DE-627)NLEJ190543086 DE-627 ger DE-627 rakwb eng Drift of large-scale hot thermals in stratified air flows 1984 3 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract A difference method developed for the calculation of the three-dimensional unsteady flows of a viscous heat-conducting gas is used to investigate the influence of a horizontal wind, stratified with respect to height, on the motion of the eruption clouds of a volcano. It is shown that as the intensity of the air flow rises and its stratification increases the rate of ascent of the thermal decreases. Data are obtained for the features of the motion of the vortex rings formed. Springer Online Journal Archives 1860-2002 Andrushchenko, V. A. oth Chudov, L. A. oth in Fluid dynamics 1966 19(1984) vom: Juni, Seite 1012-1014 (DE-627)NLEJ188992693 (DE-600)2039450-0 1573-8507 nnns volume:19 year:1984 month:06 pages:1012-1014 extent:3 http://dx.doi.org/10.1007/BF01411597 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 19 1984 6 1012-1014 3 |
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(DE-627)NLEJ190543086 DE-627 ger DE-627 rakwb eng Drift of large-scale hot thermals in stratified air flows 1984 3 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract A difference method developed for the calculation of the three-dimensional unsteady flows of a viscous heat-conducting gas is used to investigate the influence of a horizontal wind, stratified with respect to height, on the motion of the eruption clouds of a volcano. It is shown that as the intensity of the air flow rises and its stratification increases the rate of ascent of the thermal decreases. Data are obtained for the features of the motion of the vortex rings formed. Springer Online Journal Archives 1860-2002 Andrushchenko, V. A. oth Chudov, L. A. oth in Fluid dynamics 1966 19(1984) vom: Juni, Seite 1012-1014 (DE-627)NLEJ188992693 (DE-600)2039450-0 1573-8507 nnns volume:19 year:1984 month:06 pages:1012-1014 extent:3 http://dx.doi.org/10.1007/BF01411597 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 19 1984 6 1012-1014 3 |
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Drift of large-scale hot thermals in stratified air flows |
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Abstract A difference method developed for the calculation of the three-dimensional unsteady flows of a viscous heat-conducting gas is used to investigate the influence of a horizontal wind, stratified with respect to height, on the motion of the eruption clouds of a volcano. It is shown that as the intensity of the air flow rises and its stratification increases the rate of ascent of the thermal decreases. Data are obtained for the features of the motion of the vortex rings formed. |
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Abstract A difference method developed for the calculation of the three-dimensional unsteady flows of a viscous heat-conducting gas is used to investigate the influence of a horizontal wind, stratified with respect to height, on the motion of the eruption clouds of a volcano. It is shown that as the intensity of the air flow rises and its stratification increases the rate of ascent of the thermal decreases. Data are obtained for the features of the motion of the vortex rings formed. |
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Abstract A difference method developed for the calculation of the three-dimensional unsteady flows of a viscous heat-conducting gas is used to investigate the influence of a horizontal wind, stratified with respect to height, on the motion of the eruption clouds of a volcano. It is shown that as the intensity of the air flow rises and its stratification increases the rate of ascent of the thermal decreases. Data are obtained for the features of the motion of the vortex rings formed. |
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