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Interannual Variability of Surface and Integrated Water Vapor and Atmospheric Circulation in Europe of the atmosphere and the surface partial pressure of water vapor for the territory of Europe over a long period

Manifestation of Equatorial Processes in Water Vapor Variations over Europe-surface water vapor partial pressure on the territory of Europe over a multiyear period. It is found

Interannual variability of the integral water vapor in Europe, global circulation and El Niño. However, the coherence of variations of ENSO and the surface partial pressure of water vapor is irregular

Tropospheric Water Vapor Long-term Periodicities and ENSO Relation in European Territory of Russia of American Geophysical Union The variability of time series of the surface partial pressure of water vapor

Partial molar volumes of organic solutes in water. XXIII. Cyclic ketones at T = (298 to 573) K and pressures up to 30 MPa at temperatures from T = 298 K up to T = 573 K. Experimental pressures were close to the saturated vapor pressure

Partial molar volumes of organic solutes in water. XXIII. Cyclic ketones at T = (298 to 573) K and pressures up to 30 MPa at temperatures from T = 298 K up to T = 573 K. Experimental pressures were close to the saturated vapor pressure

Математическое моделирование переноса парообразной влаги под действием разности парциального давления водяного пара в стеновых ограждающих конструкциях зданийThe problem of water vapor transfer in the building walls under the water vapor partial pressure

Changes in the composition and properties of Ashalchinskoye bitumen-saturated sandstones when exposed to water vapor
for enhanced of oil recovery in reservoir used pressurization a water vapor with a temperature of ∼ 180 C (SAGD

Hydration of α-chymotrypsin: Excess partial enthalpies of water and enzyme of the dried and hydrated enzyme in water at 25 °C. From these thermochemical data the excess partial

Inter-annual variability of variations of ground and integrated atmospheric water vapor content in Europe
with increasing latitude and further from the coast. The intensity of variations in the partial pressure of water

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