<?xml version="1.0"?>
<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:title>Hygroscopic properties of aerosols in the Sahel : preliminary results</dc:title>
  <dc:creator>Bedou, M.</dc:creator>
  <dc:creator>Konare, A.</dc:creator>
  <dc:creator>Seidou-Sanda, I.</dc:creator>
  <dc:creator>Assamoi, P.</dc:creator>
  <dc:creator>/Diedhiou, Arona</dc:creator>
  <dc:subject>aerosol</dc:subject>
  <dc:subject>optical depth</dc:subject>
  <dc:subject>Angstrom coefficient</dc:subject>
  <dc:subject>atmospheric water content</dc:subject>
  <dc:subject>and hygroscopic growth</dc:subject>
  <dc:description>Approximately three years of sunphotometric measurements carried out in the locality of Bidi (13.36 degrees N; 2.30 degrees W) in Burkina Faso (West Africa) from October 1986 to January 1989 were used to estimate the atmospheric precipitable water vapour (APW) and the Angstrom exponent values a. A study of the relationship between these two parameters on a seasonal time scale shows that an increase of water vapour in the Sahel is associated with a decrease of a values, indicating hygroscopic growth of aerosol particles. This result shows that the Sahel aerosol particles may grow in size through water vapour absorption due to hygroscopic properties.</dc:description>
  <dc:date>2007</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/fdi:010044085</dc:identifier>
  <dc:identifier>fdi:010044085</dc:identifier>
  <dc:identifier>Bedou M., Konare A., Seidou-Sanda I., Assamoi P., Diedhiou Arona. Hygroscopic properties of aerosols in the Sahel : preliminary results. 2007, 2 (6),  177-183</dc:identifier>
  <dc:language>EN</dc:language>
</oai_dc:dc>
