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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>9</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-6957-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/6957/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/6957/2009/acpd-9-6957-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/6957/2009/acpd-9-6957-2009.pdf</fulltext_pdf>
	<start_page>6957</start_page>
	<end_page>6977</end_page>
	<publication_date>2009-03-16</publication_date>
	<article_title content_type="html">Study of successive contrasting monsoons (2001–2002) in terms of  aerosol variability over a tropical station Pune, India</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>R. L. Bhawar</name>
			<email>rohinibhawar@yahoo.com</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>P. C. S. Devara</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">DIFA, Università degli Studi della Basilicata, Viale dell&apos;Ateneo Lucano no. 10, 85100 Potenza, Italy</affiliation>
		<affiliation numeration="2" content_type="html">Indian Institute of Tropical Meteorology, Dr. Homi Bhabha Road, Pashan, Pune, Maharastra 411 008, India</affiliation>
	</affiliations>
	<abstract content_type="html">The present study confirms that aerosols play a major role in
      cloud formation and affect significantly the precipitation
      over a regional scale. The study here shows that there is a high variability
      of aerosol index during a bad monsoon year 2002 indicating an extension of
      cycle to more than 100 days from a normal 50 day cycle of absorbing and non-
      absorbing aerosols over a tropical urban station Pune. Pre-monsoon 2002 shows
      a high loading of coarse mode aerosols (absorbing aerosols)
      which indicates vertical and horizontal temperature variations
      in turn affecting the seasonal rainfall at a regional
      scale. Cloud formation highly depends on aerosol
      concentration, where surface meteorological features are
      essential to initiate the process. The surface temperatures
      were high during the pre-monsoon of 2002 as compared to
      2001. The effect of wind speed though, complicated to
      understand, reveal low values in 2002 with high aerosol
      optical depth and vice versa in 2001.</abstract>
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</article>

