Results 301 to 310 of about 676,822 (358)
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Journal of Geophysical Research: Oceans, 1982
Water vapor in the earth's mesosphere has been observed at the frequency of 22.235 Ghz as an absorption against the sun by utilizing a ground‐based radio telescope. The H2O mixing ratio of 4.3±1 ppm is obtained in the height 40–70 km for a constant distribution model.
S. Deguchi, D. O. Muhleman
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Water vapor in the earth's mesosphere has been observed at the frequency of 22.235 Ghz as an absorption against the sun by utilizing a ground‐based radio telescope. The H2O mixing ratio of 4.3±1 ppm is obtained in the height 40–70 km for a constant distribution model.
S. Deguchi, D. O. Muhleman
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Russian Journal of Physical Chemistry A, 2008
The characteristics of water vapor polarization were calculated, and several polarization theory equations applicable to different states of aggregation of molecular systems were obtained.
N. M. Putintsev, D. N. Putintsev
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The characteristics of water vapor polarization were calculated, and several polarization theory equations applicable to different states of aggregation of molecular systems were obtained.
N. M. Putintsev, D. N. Putintsev
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Water and Water Vapor Environment
2002Water movement in soil is much more complicated than that of CO2 because not only is water present in two phases, one liquid and the other gas, but also water movement is related to heat flow. However, in order to simplify the problem and understand the system clearly, it is again assumed that vapor flow in soil is independent of heat flow, as we ...
Tadashi Takakura, Wei Fang
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Photoinduced Nucleation of Water Vapor
Science, 1978Strong photoinduced nucleation of pure water vapor was found to occur in a wavelength range where no ultraviolet absorption of water vapor has been reported. Systematic studies were made of the dependence of the nucleation rate and the delay time for the initiation of nucleation on light intensity.
F C, Wen, T, McLaughlin, J L, Katz
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Water Vapor Adsorption on Goethite
Environmental Science & Technology, 2013Goethite (α-FeOOH) is an important mineral contributing to processes of atmospheric and terrestrial importance. Their interactions with water vapor are particularly relevant in these contexts. In this work, molecular details of water vapor (0.0-19.0 Torr; 0-96% relative humidity at 25 °C) adsorption at surfaces of synthetic goethite nanoparticles ...
Xiaowei, Song, Jean-François, Boily
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Journal of Geophysical Research: Oceans, 1983
We present a tutorial review of our understanding of stratospheric H2O and the processes controlling it. We attempt to synthesize a consistent global picture that requires rejection of a minimum of the conflicting observational data. As such, this synthesis is determined somewhat by the personal opinions and beliefs of the author. We note the paradoxes
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We present a tutorial review of our understanding of stratospheric H2O and the processes controlling it. We attempt to synthesize a consistent global picture that requires rejection of a minimum of the conflicting observational data. As such, this synthesis is determined somewhat by the personal opinions and beliefs of the author. We note the paradoxes
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Electrical Breakdown in Water Vapor
Physical Review E, 2011In this paper investigations of the voltage required to break down water vapor are reported for the region around the Paschen minimum and to the left of it. In spite of numerous applications of discharges in biomedicine, and recent studies of discharges in water and vapor bubbles and discharges with liquid water electrodes, studies of the basic ...
Skoro, N. +4 more
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Eos, Transactions American Geophysical Union, 1932
This note is a protest (Astroph. J., v. 37, 359, 1913) against the continued use of Hann's formula (l.c.) for the determination of the amount of water‐vapor above a given place by way of the amount of water‐vapor at that place. In the data here used the former is obtained as a function of the depth of the water‐vapor band ρ calibrated in the laboratory
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This note is a protest (Astroph. J., v. 37, 359, 1913) against the continued use of Hann's formula (l.c.) for the determination of the amount of water‐vapor above a given place by way of the amount of water‐vapor at that place. In the data here used the former is obtained as a function of the depth of the water‐vapor band ρ calibrated in the laboratory
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WATER VAPOR IN THE STRATOSPHERE
Soviet Physics Uspekhi, 1963CONTENTS 1. Introduction 390 2. Local Measurements of Humidity 392 3. Spectral Measurements 398 4. Indirect Methods of Estimating Humidity 405 5. Possible Sources and Sinks of Moisture in the Stratosphere 406 6.
M.S. Malkevich +2 more
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