Interdependence of tropical cirrus properties and their variability

The mean properties of tropical cirrus, such as cloud top, cloud base, optic centre, cloud strength/optical depth, asymmetry factor and cloud depolarization, as well as their heterogeneities are examined using lidar observations over 281 nights from a tropical station Gadanki (13.5° N, 7...

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Main Authors: S. V. Sunilkumar, K. Parameswaran, B. V. Thampi
Format: Article
Language:English
Published: Copernicus Publications 2008-03-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/26/413/2008/angeo-26-413-2008.pdf
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spelling doaj-01bd3e06f592436a91d3f12dcbcaeda02020-11-24T22:36:42ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762008-03-012641342910.5194/angeo-26-413-2008Interdependence of tropical cirrus properties and their variabilityS. V. Sunilkumar0K. Parameswaran1B. V. Thampi2Space Physics Laboratory, Vikram Sarabhai Space Centre, Trivandrum-695022, Kerala, IndiaSpace Physics Laboratory, Vikram Sarabhai Space Centre, Trivandrum-695022, Kerala, IndiaSpace Physics Laboratory, Vikram Sarabhai Space Centre, Trivandrum-695022, Kerala, IndiaThe mean properties of tropical cirrus, such as cloud top, cloud base, optic centre, cloud strength/optical depth, asymmetry factor and cloud depolarization, as well as their heterogeneities are examined using lidar observations over 281 nights from a tropical station Gadanki (13.5&deg; N, 79.2&deg; E) during the period 1998&ndash;2002. This study shows that as the cloud optical depth (&tau;<sub><I>c</I></sub>) increases the cloud becomes more asymmetric in its scattering property. The amount of asymmetry is less than 2% for very low values of (&tau;<sub><I>c</I></sub> and increases nonlinearly with an increase in (&tau;<sub><I>c</I></sub>. The physical properties of these clouds also show significant variation with different time scales during the course of each night. On average, while the short-term variations in (&tau;<sub><I>c</I></sub> are in opposite phase with those of the asymmetry factor (ξ) and volume depolarization ratio (δ), the long-term variation in (&tau;<sub><I>c</I></sub> extending over a night are found to be in opposite phase with that of ξ and in-phase with that of δ. The short-term variations in δ and (&tau;<sub><I>c</I></sub> were attributed to possible changes in the cloud particle orientation and the long period variations to cloud evolution process. The value of δ shows a pronounced variation along the vertical, with low values near the cloud top and cloud base and high values in the middle, which is attributed to the cloud dynamics.https://www.ann-geophys.net/26/413/2008/angeo-26-413-2008.pdf
collection DOAJ
language English
format Article
sources DOAJ
author S. V. Sunilkumar
K. Parameswaran
B. V. Thampi
spellingShingle S. V. Sunilkumar
K. Parameswaran
B. V. Thampi
Interdependence of tropical cirrus properties and their variability
Annales Geophysicae
author_facet S. V. Sunilkumar
K. Parameswaran
B. V. Thampi
author_sort S. V. Sunilkumar
title Interdependence of tropical cirrus properties and their variability
title_short Interdependence of tropical cirrus properties and their variability
title_full Interdependence of tropical cirrus properties and their variability
title_fullStr Interdependence of tropical cirrus properties and their variability
title_full_unstemmed Interdependence of tropical cirrus properties and their variability
title_sort interdependence of tropical cirrus properties and their variability
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2008-03-01
description The mean properties of tropical cirrus, such as cloud top, cloud base, optic centre, cloud strength/optical depth, asymmetry factor and cloud depolarization, as well as their heterogeneities are examined using lidar observations over 281 nights from a tropical station Gadanki (13.5&deg; N, 79.2&deg; E) during the period 1998&ndash;2002. This study shows that as the cloud optical depth (&tau;<sub><I>c</I></sub>) increases the cloud becomes more asymmetric in its scattering property. The amount of asymmetry is less than 2% for very low values of (&tau;<sub><I>c</I></sub> and increases nonlinearly with an increase in (&tau;<sub><I>c</I></sub>. The physical properties of these clouds also show significant variation with different time scales during the course of each night. On average, while the short-term variations in (&tau;<sub><I>c</I></sub> are in opposite phase with those of the asymmetry factor (ξ) and volume depolarization ratio (δ), the long-term variation in (&tau;<sub><I>c</I></sub> extending over a night are found to be in opposite phase with that of ξ and in-phase with that of δ. The short-term variations in δ and (&tau;<sub><I>c</I></sub> were attributed to possible changes in the cloud particle orientation and the long period variations to cloud evolution process. The value of δ shows a pronounced variation along the vertical, with low values near the cloud top and cloud base and high values in the middle, which is attributed to the cloud dynamics.
url https://www.ann-geophys.net/26/413/2008/angeo-26-413-2008.pdf
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