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The vertical structure of tropical convection and its impact on the budgets of water vapor and ozone
(American Meteorological Society, 2005)
Convective clouds in the Tropics that penetrate the boundary layer inversion preferentially detrain into a shallow outflow layer (2-5 km) or a deep outflow layer (10-17 km). The properties of these layers are diagnosed ...
Infrared water vapor continuum absorption at atmospheric temperatures
(American Institute of Physics Inc, 2005)
We have used a continuous-wave carbon dioxide laser in a single-mode realization of cavity ring-down spectroscopy to measure absorption coefficients of water vapor at 944 cm-1 for several temperatures in the range 270-315 ...