A simple explanation for the increase in relative humidity between 11 and 14 km in the tropics

Journal of Geophysical Research Atmospheres

Volumn 107, Issue 23, 2002, Pages ACL-26-1-ACL-26-7

  Folkins, Ian ^a   Kelly, K K ^b   Weinstock, E M ^c,d  

^a DALHOUSIE UNIVERSITY   (Canada)

^b NOAA EARTH SYSTEM RESEARCH LABORATORY   (United States)

^c HARVARD UNIVERSITY   (United States)

^d HARVARD UNIVERSITY   (United States)

Author keywords

0322 Atmospheric Composition and Structure: Constituent sources and sinks; 0365 Atmospheric Composition and Structure: Troposphere composition and chemistry; 0368 Atmospheric Composition and Structure: Troposphere constituent transport and chemistry

Indexed keywords

ATMOSPHERIC HUMIDITY; COMPUTER SIMULATION; EVAPORATION; HEAT CONVECTION; RADIATION; TROPICS; TROPOSPHERE; VAPORS;

CONVECTION; HUMIDITY;

EID: 85080838805     PISSN: 01480227     EISSN: None     Source Type: Journal    
DOI: 10.1029/2002JD002185     Document Type: Article

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