2014
DOI: 10.1002/asl2.517
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Impact of monsoon‐associated deep‐penetrating clouds on the hydration of the tropical upper troposphere

Abstract: This paper examines the relationship between water vapor mixing ratio (WVMR) and cloud top height (CTH) in the tropical upper troposphere. The region of high WVMR and CTH is collocated and observed over the core convective region. WVMR over South Asia shows significant correlation with CTH. Increase in CTH is observed during the moist phase of water vapor followed by a decrease in CTH during the dry phase. Daily CTH data show that some convective turrets reach above 150 hPa. Present analysis shows that moisten… Show more

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Cited by 4 publications
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“…This might be due to the transport of atmospheric moisture from Arabian Sea by strong southwesterlies during the monsoon. Over Indian region during monsoon period the convective clouds reaches ~7 km and these clouds can influence the moisture content in the upper troposphere (Jain et al ., ). The enhancement of mid‐troposphere moisture after the onset of ISM is well known characteristics of ISM.…”
Section: Resultsmentioning
confidence: 97%
“…This might be due to the transport of atmospheric moisture from Arabian Sea by strong southwesterlies during the monsoon. Over Indian region during monsoon period the convective clouds reaches ~7 km and these clouds can influence the moisture content in the upper troposphere (Jain et al ., ). The enhancement of mid‐troposphere moisture after the onset of ISM is well known characteristics of ISM.…”
Section: Resultsmentioning
confidence: 97%