Results 161 to 170 of about 165,706 (218)
Regulating the Hydrophilicity of Hyper-Cross-Linked Polymers via Thermal Oxidation for Atmospheric Water Harvesting. [PDF]
ACS Appl Mater InterfacesSchweng P, Präg L, Woodward RT.
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Design of a Compact Multicyclic High-Performance Atmospheric Water Harvester for Arid Environments. [PDF]
ACS Energy LettLi X +8 more
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Research Progress on Hygroscopic Agents for Atmospheric Water Harvesting Systems. [PDF]
Materials (Basel)Bai Q, Zhou W, Cui W, Qi Z.
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Journal of Chemical Education, 2004
None of eight college-level general chemistry texts gave a mean value for water in the atmosphere, despite its being the third most prevalent constituent at about 1.5% by mass as vapor and about 2%...
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None of eight college-level general chemistry texts gave a mean value for water in the atmosphere, despite its being the third most prevalent constituent at about 1.5% by mass as vapor and about 2%...
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Proceedings of the International School of Physics “Enrico Fermi”
In this article, the multiple roles of water in the Earth's atmosphere are reviewed. In particular, the behavior of atmospheric water in its various physical states such as water vapor, liquid water, and crystalline ice are discussed. Special emphasis is given towards its pure metastable and stable phases at ambient conditions. Moreover, the occurrence
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In this article, the multiple roles of water in the Earth's atmosphere are reviewed. In particular, the behavior of atmospheric water in its various physical states such as water vapor, liquid water, and crystalline ice are discussed. Special emphasis is given towards its pure metastable and stable phases at ambient conditions. Moreover, the occurrence
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Water Substance and the Atmosphere
1967Water is the working substance in so many thermal processes that its properties are of particular interest. First let us consider its density, or the reciprocal of density, which is called specific volume. Starting with ice, say at − 20C, and increasing the temperature, we find that ice expands, like most solids, until at 0C its specific volume is 1 ...
J. S. Marshall +2 more
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2017
Among the planets in the Solar System, Earth is unique in possessing large quantities of water, and water’s properties are highly significant in determining weather. This is because water readily exists in three different phases (ice, liquid water, and water vapour) at temperatures frequently encountered on Earth.
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Among the planets in the Solar System, Earth is unique in possessing large quantities of water, and water’s properties are highly significant in determining weather. This is because water readily exists in three different phases (ice, liquid water, and water vapour) at temperatures frequently encountered on Earth.
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2019
The pole of cold in the Northern Hemisphere is located in eastern Siberia, where precipitation is low. In addition to the regional climate, the water cycle in eastern Siberia is characterized by geographical and terrestrial environmental factors involving topography, distance from the ocean, vegetation type, and permafrost.
Kazuhiro Oshima, Koji Yamazaki
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The pole of cold in the Northern Hemisphere is located in eastern Siberia, where precipitation is low. In addition to the regional climate, the water cycle in eastern Siberia is characterized by geographical and terrestrial environmental factors involving topography, distance from the ocean, vegetation type, and permafrost.
Kazuhiro Oshima, Koji Yamazaki
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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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