Hostname: page-component-586b7cd67f-r5fsc Total loading time: 0 Render date: 2024-11-24T08:03:20.019Z Has data issue: false hasContentIssue false

Relationship between lidar-based observations of aerosol content and monsoon precipitation over a tropical station, Pune, India

Published online by Cambridge University Press:  30 October 2003

P C S Devara
Affiliation:
Physical Meteorology and Aerology Division, Indian Institute of Tropical Meteorology,Pune 411 008, India
P E Raj
Affiliation:
Physical Meteorology and Aerology Division, Indian Institute of Tropical Meteorology,Pune 411 008, India
G Pandithurai
Affiliation:
Physical Meteorology and Aerology Division, Indian Institute of Tropical Meteorology,Pune 411 008, India
K K Dani
Affiliation:
Physical Meteorology and Aerology Division, Indian Institute of Tropical Meteorology,Pune 411 008, India
R S Maheskumar
Affiliation:
Physical Meteorology and Aerology Division, Indian Institute of Tropical Meteorology,Pune 411 008, India
Get access

Abstract

This paper reports the results of the aerosol lidar experiments that have been performed at the Indian Institute of Tropical Meteorology (IITM), Pune (18.54°N, 73.85°E, 559 m amsl), a tropical station in India. The lidar-observed cloud macro-physical parameters (cloud-base and cloud-ceiling heights, vertical thickness, etc.) and polarisation characteristics and their association with surface-generated aerosols at the experimental site are presented and discussed. The correspondence among the lidar-derived aerosol distributions, meteorological parameters and south-west (SW) monsoon (June-September) activity over Pune during 12 successive SW monsoon seasons (1987-98) including two pairs of contrasting seasons of 1987-8 and 1993-4 is also examined. The results indicate an association between variations in aerosol loading in the boundary layer during the pre-monsoon season (March-May) and precipitation intensity during the ensuing monsoon season. Moreover, the decrease in aerosol content from pre-monsoon to monsoon season is found to follow the SW monsoon season total precipitation. Thus the results suggest that (i) the IITM lidar can also be a useful remote sensor for aerosol characterisation studies from polarisation measurements, and some important physical properties of clouds in the lower atmosphere over the station, and (ii) there exists a correspondence between boundary-layer aerosol content and SW monsoon precipitation over Pune, which is explained in terms of the type of aerosols and the environmental and meteorological processes, particularly during pre-monsoon and monsoon months prevailing over the experimental station.

Type
Research Article
Copyright
© 2003 Royal Meteorological Society

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)