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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Copernicus Publications
2008-03-01
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Series: | Annales Geophysicae |
Online Access: | https://www.ann-geophys.net/26/413/2008/angeo-26-413-2008.pdf |
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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° N, 79.2° E) during the period 1998–2002. This study shows that as the cloud optical depth (τ<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 (τ<sub><I>c</I></sub> and increases nonlinearly with an increase in (τ<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 (τ<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 (τ<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 (τ<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° N,
79.2° E) during the period 1998–2002. This study shows that as the cloud
optical depth (τ<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 (τ<sub><I>c</I></sub> and increases nonlinearly with an increase in
(τ<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 (τ<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 (τ<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 (τ<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 |
work_keys_str_mv |
AT svsunilkumar interdependenceoftropicalcirruspropertiesandtheirvariability AT kparameswaran interdependenceoftropicalcirruspropertiesandtheirvariability AT bvthampi interdependenceoftropicalcirruspropertiesandtheirvariability |
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