In the realm of atmospheric sciences, the vertical air motion in any region dictates the structure and dynamics of that region. Importantly in the lower part of the atmosphere, wide spread deterioration and improvement of weather is usually caused by the vertical air motion. Adiabatic cooling due to upward motion leads to formation of clouds and adiabatic warming due to downward motion leads to dissipation of clouds. Thus vertical air motion plays a vital role in controlling the day to day weather. Also the information of convective updrafts/downdrafts is crucial for aviation industry and also for rocket launches. The direct measurements of vertical air motion were not possible until the advent of wind profilers. Realizing the importance of vertical air motion in the tropical atmosphere, the present thesis brings out unique results on the mean structure and variability of vertical velocity during fair-weather and convection using long term data (10 years) from Indian Mesosphere Stratosphere Troposphere (MST) Radar.- Dr. K. N. Uma
Die Inhaltsangabe kann sich auf eine andere Ausgabe dieses Titels beziehen.
Dr.K.N.Uma has obtained her PhD degree in Physics. She has advanced several hypotheses which have been extensively used for research on convective dynamics. Dr. Uma has worked at NARL and presently Scientist at SPL/VSSC (ISRO). She is the author of several research articles published in reputed international journals.
„Über diesen Titel“ kann sich auf eine andere Ausgabe dieses Titels beziehen.
Anbieter: BuchWeltWeit Ludwig Meier e.K., Bergisch Gladbach, Deutschland
Taschenbuch. Zustand: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -In the realm of atmospheric sciences, the vertical air motion in any region dictates the structure and dynamics of that region. Importantly in the lower part of the atmosphere, wide spread deterioration and improvement of weather is usually caused by the vertical air motion. Adiabatic cooling due to upward motion leads to formation of clouds and adiabatic warming due to downward motion leads to dissipation of clouds. Thus vertical air motion plays a vital role in controlling the day to day weather. Also the information of convective updrafts/downdrafts is crucial for aviation industry and also for rocket launches. The direct measurements of vertical air motion were not possible until the advent of wind profilers. Realizing the importance of vertical air motion in the tropical atmosphere, the present thesis brings out unique results on the mean structure and variability of vertical velocity during fair-weather and convection using long term data (10 years) from Indian Mesosphere Stratosphere Troposphere (MST) Radar.- Dr. K. N. Uma 180 pp. Englisch. Bestandsnummer des Verkäufers 9783846558331
Anzahl: 2 verfügbar
Anbieter: moluna, Greven, Deutschland
Zustand: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Autor/Autorin: Uma K. N.Dr.K.N.Uma has obtained her PhD degree in Physics. She has advanced several hypotheses which have been extensively used for research on convective dynamics. Dr. Uma has worked at NARL and presently Scientist at SPL/VSSC (ISR. Bestandsnummer des Verkäufers 5498970
Anzahl: Mehr als 20 verfügbar
Anbieter: preigu, Osnabrück, Deutschland
Taschenbuch. Zustand: Neu. Vertical Air Motion and its Variability using MST Radar | Observational Aspects on Vertical Air Motion during Fair-Weather and Convection Over a Tropical Region | K. N. Uma (u. a.) | Taschenbuch | 180 S. | Englisch | 2011 | LAP LAMBERT Academic Publishing | EAN 9783846558331 | Verantwortliche Person für die EU: BoD - Books on Demand, In de Tarpen 42, 22848 Norderstedt, info[at]bod[dot]de | Anbieter: preigu. Bestandsnummer des Verkäufers 106714485
Anzahl: 5 verfügbar
Anbieter: buchversandmimpf2000, Emtmannsberg, BAYE, Deutschland
Taschenbuch. Zustand: Neu. This item is printed on demand - Print on Demand Titel. Neuware -In the realm of atmospheric sciences, the vertical air motion in any region dictates the structure and dynamics of that region. Importantly in the lower part of the atmosphere, wide spread deterioration and improvement of weather is usually caused by the vertical air motion. Adiabatic cooling due to upward motion leads to formation of clouds and adiabatic warming due to downward motion leads to dissipation of clouds. Thus vertical air motion plays a vital role in controlling the day to day weather. Also the information of convective updrafts/downdrafts is crucial for aviation industry and also for rocket launches. The direct measurements of vertical air motion were not possible until the advent of wind profilers. Realizing the importance of vertical air motion in the tropical atmosphere, the present thesis brings out unique results on the mean structure and variability of vertical velocity during fair-weather and convection using long term data (10 years) from Indian Mesosphere Stratosphere Troposphere (MST) Radar.- Dr. K. N. UmaVDM Verlag, Dudweiler Landstraße 99, 66123 Saarbrücken 180 pp. Englisch. Bestandsnummer des Verkäufers 9783846558331
Anzahl: 1 verfügbar
Anbieter: AHA-BUCH GmbH, Einbeck, Deutschland
Taschenbuch. Zustand: Neu. nach der Bestellung gedruckt Neuware - Printed after ordering - In the realm of atmospheric sciences, the vertical air motion in any region dictates the structure and dynamics of that region. Importantly in the lower part of the atmosphere, wide spread deterioration and improvement of weather is usually caused by the vertical air motion. Adiabatic cooling due to upward motion leads to formation of clouds and adiabatic warming due to downward motion leads to dissipation of clouds. Thus vertical air motion plays a vital role in controlling the day to day weather. Also the information of convective updrafts/downdrafts is crucial for aviation industry and also for rocket launches. The direct measurements of vertical air motion were not possible until the advent of wind profilers. Realizing the importance of vertical air motion in the tropical atmosphere, the present thesis brings out unique results on the mean structure and variability of vertical velocity during fair-weather and convection using long term data (10 years) from Indian Mesosphere Stratosphere Troposphere (MST) Radar.- Dr. K. N. Uma. Bestandsnummer des Verkäufers 9783846558331
Anzahl: 1 verfügbar
Anbieter: Revaluation Books, Exeter, Vereinigtes Königreich
Paperback. Zustand: Brand New. 180 pages. 8.66x5.91x0.41 inches. In Stock. Bestandsnummer des Verkäufers 3846558338
Anzahl: 1 verfügbar
Anbieter: Mispah books, Redhill, SURRE, Vereinigtes Königreich
paperback. Zustand: New. NEW. SHIPS FROM MULTIPLE LOCATIONS. book. Bestandsnummer des Verkäufers ERICA82938465583386
Anzahl: 1 verfügbar