Correlation among cirrus ice content, water vapor and temperature in the TTL as observed by CALIPSO and Aura/MLS

Simulated model fields, including liquid water path (LWP), ice water path, cloud fraction, shortwave and longwave cloud forcing, precipitation, water vapor, and cloud droplet

The wa- ter vapor content along the line of sight between a ground station and a GPS satellite can be derived from GPS data and directly measured by a water vapor radiometer (WVR)

In addition, the mixing induced by the wake turbulence gen- erated during the vortex breakup in the dissipation regime is able to break the equilibrium between water vapor and

Solheim F, Godwin J, Ware R (1998) Passive ground-based remote sensing of atmospheric temperature, water vapor, and cloud liquid water profiles by a frequency synthesized

Para estabelecer qual das seqüências contidas no banco será fixada como centro, são calculadas as pontua- ções entre os pares de seqüências (5i,5)), 1 ~ i,j ~ k, i*-j.

ure 7 shows the time series of water vapor profile derived from MLS, tropopause level from sounder temperature profiles, and the altitude of daily mean maximum aerosol extinction

Water vapor and CO in the lowest altitude grid point for all longitudes is the v1.5 Aura MLS 147 hPa tropical zonal mean measurement interpolated to the model time.. Condensation,

Possible explanations for this high threshold are that (1) the expressions used for calcu- lating vapor pressure over supercooled water at low temper- atures give values are at