9 Water Vapor and Entropy Production in the Earth’s Atmosphere

Author(s):  
Olivier M. Pauluis
1998 ◽  
Vol 103 (D4) ◽  
pp. 3847-3858 ◽  
Author(s):  
S. Solomon ◽  
R. W. Portmann ◽  
R. W. Sanders ◽  
J. S. Daniel

2011 ◽  
Vol 4 (1) ◽  
pp. 135-212 ◽  
Author(s):  
R. A. Anthes

Abstract. The launch of the proof-of-concept mission GPS/MET in 1995 began a revolution in profiling earth's atmosphere through radio occultation (RO). GPS/MET; subsequent single-satellite missions CHAMP, SAC-C, GRACE, METOP-A, and TerraSAR-X; and the six-satellite constellation, FORMOSAT-3/COSMIC, have proven the theoretical capabilities of RO to provide accurate and precise profiles of electron density in the ionosphere and refractivity, containing information on temperature and water vapor, in the stratosphere and troposphere. This paper summarizes results from these RO missions and the applications of RO observations to atmospheric research and operational weather analysis and prediction.


1992 ◽  
Vol 31 (16) ◽  
pp. 3068 ◽  
Author(s):  
D. N. Whiteman ◽  
S. H. Melfi ◽  
R. A. Ferrare

2020 ◽  
Author(s):  
E.A. Shirokova ◽  
◽  
A.G. Razuvaev ◽  
A.V. Mayorov ◽  
B. Aradi ◽  
...  

In order to estimate the effect of orientational isomerism on the thermodynamic parameters and concentrations of water clusters in the gas phase, all possible structures of book, cageand prismconformations of water hexamer (H2O)6have been studied using the DFT (B3LYP/6-311++G(2d,2p)), G4, DFTB, W1BD and MB-pol calculations. It was found that taking into account of the orientational isomerism leads to the values of water cluster gas-phase concentrations different by 1–2 orders of magnitude from the results obtained when only single or several most energetically favorable structures are considered. The concentrations of all the considered hexamer structuresin the saturated water vapor at T= 298.15 K are estimated as 1.61 103(G4) and 8.17 105 (DFT) molecules/cm3.


2005 ◽  
Vol 5 (5) ◽  
pp. 8209-8232
Author(s):  
T. J. Garrett ◽  
C. Liu ◽  
J. Dean-Day ◽  
B. K. Barnett ◽  
G. G. Mace ◽  
...  

Abstract. Thin stratiform clouds called pileus can form in the earth's atmosphere when humid air is lifted above rising convection. In the lower troposphere pileus lifetimes are short, so they have been considered little more than an attractive curiosity. This paper describes pileus cloud forming near the tropopause at low-latitudes, and discusses how they may be associated with a redistribution of water vapor and ice at cold temperatures.


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