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2012
Gaseous and volatile chemical species reside not only in the atmosphere. Because they dissolve in water, they are also distributed in the hydrosphere. The by far largest part of the hydrosphere is the ocean. Therefore, the exchange between atmosphere and oceans is the most important process for the fate of gaseous and volatile chemical species (Table 8.
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Gaseous and volatile chemical species reside not only in the atmosphere. Because they dissolve in water, they are also distributed in the hydrosphere. The by far largest part of the hydrosphere is the ocean. Therefore, the exchange between atmosphere and oceans is the most important process for the fate of gaseous and volatile chemical species (Table 8.
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Water and Ice in the Atmosphere
The Journal of the Royal Aeronautical Society, 1959Over the past years many questions which come under the broad heading of cloud physics have been put to the Meteorological Office by aircraft firms and others, questions on the water and ice crystal contents of clouds and the size distribution of raindrops are examples.
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Condensation of Water in the Atmosphere
Nature, 1934IN NATURE of December 16, p. 938, it is stated: “A number of workers, notably Defant, Kohler,: Niederdorfer, claim to have shown that the volume of droplets in the atmosphere are most frequently integral multiples of some standard minimum size”. The “law” claimed by Defant and Kohler is much more interesting than this statement implies.
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Dual-Stage Atmospheric Water Harvesting Device for Scalable Solar-Driven Water Production
Joule, 2021Yang Zhong, Evelyn Wang, Árný Leroy
exaly
Sorption‐Based Atmospheric Water Harvesting: Materials, Components, Systems, and Applications
Advanced Materials, 2023Liang An, R Z Wang
exaly
Polyzwitterionic Hydrogels for Efficient Atmospheric Water Harvesting
Angewandte Chemie - International Edition, 2022Guihua Yu, Hengyi Lu, Youhong Guo
exaly
Sorbents for Atmospheric Water Harvesting: From Design Principles to Applications
Angewandte Chemie - International Edition, 2022Guihua Yu
exaly

