The tropopause height and tropopause temperature are sensitive to temperature changes in troposphere and stratosphere. These are the measures of global climatic variability. Atmospheric profiles of temperature, refractivity and water vapour are always needed for communication, navigation and atmospheric modeling studies. The tropopause characteristics over the Indian region have been studied using radio occultation measurements (CHAMP) on the basis of cold point criterion. Tropopause height shows large variation in the latitude range ∼30◦–40◦N during winter. Tropopause temperature less than −82◦C, assumed to facilitate troposphere to stratosphere air transport, is observed at a number of tropical Indian locations and no seasonal pattern ...
This research presents atmospheric temperature profiles and trends retrieved using COSMIC RO techniq...
Abstract. The diurnal variation, driven by solar forcing, is a fundamental mode in the Earth’s weath...
In this paper, it is shown that the altitude of the stratopause can be identified directly from the ...
158-161Tropical atmosphere hold key to much of variability in global climate change. But many proces...
Characteristics of the lapse rate tropopause are analyzed globally for tropopause altitude and te...
Structure and variability of the tropical tropopause are presented using radio occultation measureme...
The status of the tropopause has impact on weather phenomena and climate change occurring in the atm...
The present study examines the possible role of the "freeze and dry effect", which is generally beli...
The present study examines the possible role of the "freeze and dry effect", which is generally beli...
320-331In this study, an attempt is made to understand the ‘freeze drying’ process in the tropopau...
15th MST Radar WorkshopSession M6: Middle atmosphere dynamics and structureMay 31 (Wed), NIPR Audito...
The global characteristics and trends of the tropopause physical parameters, height and temperature,...
The vertical temperature structure of the tropical atmosphere has been explained as controlled by th...
15th MST Radar WorkshopSession M5: Meteorology and forecasting/nowcastingMay 31 (Wed), NIPR Auditori...
We have shown the relationship between seasonal, annual, and large-scale variations in convective av...
This research presents atmospheric temperature profiles and trends retrieved using COSMIC RO techniq...
Abstract. The diurnal variation, driven by solar forcing, is a fundamental mode in the Earth’s weath...
In this paper, it is shown that the altitude of the stratopause can be identified directly from the ...
158-161Tropical atmosphere hold key to much of variability in global climate change. But many proces...
Characteristics of the lapse rate tropopause are analyzed globally for tropopause altitude and te...
Structure and variability of the tropical tropopause are presented using radio occultation measureme...
The status of the tropopause has impact on weather phenomena and climate change occurring in the atm...
The present study examines the possible role of the "freeze and dry effect", which is generally beli...
The present study examines the possible role of the "freeze and dry effect", which is generally beli...
320-331In this study, an attempt is made to understand the ‘freeze drying’ process in the tropopau...
15th MST Radar WorkshopSession M6: Middle atmosphere dynamics and structureMay 31 (Wed), NIPR Audito...
The global characteristics and trends of the tropopause physical parameters, height and temperature,...
The vertical temperature structure of the tropical atmosphere has been explained as controlled by th...
15th MST Radar WorkshopSession M5: Meteorology and forecasting/nowcastingMay 31 (Wed), NIPR Auditori...
We have shown the relationship between seasonal, annual, and large-scale variations in convective av...
This research presents atmospheric temperature profiles and trends retrieved using COSMIC RO techniq...
Abstract. The diurnal variation, driven by solar forcing, is a fundamental mode in the Earth’s weath...
In this paper, it is shown that the altitude of the stratopause can be identified directly from the ...