A study of tropical tropopause using MST radar

Using the MST radar data of vertical wind, the characteristics of the tropical tropopause, following four different definitions, depending on 1) temperature lapse rate, 2) cold point, 3) convective outflow and 4) potential temperature lapse rate minimum, are studied. From the vertical wind data...

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Main Authors: K. Satheesan, B. V. Krishna Murthy
Format: Article
Language:English
Published: Copernicus Publications 2005-10-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/23/2441/2005/angeo-23-2441-2005.pdf
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author K. Satheesan
K. Satheesan
B. V. Krishna Murthy
author_facet K. Satheesan
K. Satheesan
B. V. Krishna Murthy
author_sort K. Satheesan
collection DOAJ
description Using the MST radar data of vertical wind, the characteristics of the tropical tropopause, following four different definitions, depending on 1) temperature lapse rate, 2) cold point, 3) convective outflow and 4) potential temperature lapse rate minimum, are studied. From the vertical wind data of the radar, the altitude profiles of temperature and horizontal divergence are derived, from which the tropopause levels corresponding to i) the lapse rate ii) cold point iii) convective outflow level and iv) potential temperature lapse rate minimum are determined. The convective outflow level and hence the convective tropopause altitude is determined, for the first time using the MST radar data. The tropopause altitudes and temperatures obtained following the four definitions are compared on a day-to-day basis for the summer and winter seasons. Winter and summer differences in the tropopause altitude and temperature are also studied.<br><br> <b>Keywords.</b> Meteorology and atmospheric dynamics (convective process; middle atmosphere dynamics; tropical meteorology)
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spelling doaj.art-45b0fb1be8cf4325a71a0057313e78872022-12-21T23:56:37ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762005-10-01232441244810.5194/angeo-23-2441-2005A study of tropical tropopause using MST radarK. Satheesan0K. Satheesan1B. V. Krishna Murthy2now at: Meteorology and Oceanography Group, Space Applications Centre, Ahmedabad, 380015, IndiaDepartment of Atmospheric Sciences, Cochin University of Science and Technology, Cochin, IndiaB1,Ceebros,47/20,IIIrd Main Road, Gandhinagar, Adyar, Chennai 600020, IndiaUsing the MST radar data of vertical wind, the characteristics of the tropical tropopause, following four different definitions, depending on 1) temperature lapse rate, 2) cold point, 3) convective outflow and 4) potential temperature lapse rate minimum, are studied. From the vertical wind data of the radar, the altitude profiles of temperature and horizontal divergence are derived, from which the tropopause levels corresponding to i) the lapse rate ii) cold point iii) convective outflow level and iv) potential temperature lapse rate minimum are determined. The convective outflow level and hence the convective tropopause altitude is determined, for the first time using the MST radar data. The tropopause altitudes and temperatures obtained following the four definitions are compared on a day-to-day basis for the summer and winter seasons. Winter and summer differences in the tropopause altitude and temperature are also studied.<br><br> <b>Keywords.</b> Meteorology and atmospheric dynamics (convective process; middle atmosphere dynamics; tropical meteorology)https://www.ann-geophys.net/23/2441/2005/angeo-23-2441-2005.pdf
spellingShingle K. Satheesan
K. Satheesan
B. V. Krishna Murthy
A study of tropical tropopause using MST radar
Annales Geophysicae
title A study of tropical tropopause using MST radar
title_full A study of tropical tropopause using MST radar
title_fullStr A study of tropical tropopause using MST radar
title_full_unstemmed A study of tropical tropopause using MST radar
title_short A study of tropical tropopause using MST radar
title_sort study of tropical tropopause using mst radar
url https://www.ann-geophys.net/23/2441/2005/angeo-23-2441-2005.pdf
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