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Author: Grafiati
Published: 10 December 2022
Last updated: 28 January 2023

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1

Witherell, W. D. Heat pumps in evaporation processes. South Charleston, WV: Electric Power Research Institute, 1986.

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2

Zudin, Yuri B. Non-equilibrium Evaporation and Condensation Processes. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-67306-6.

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3

Zudin, Yuri B. Non-equilibrium Evaporation and Condensation Processes. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-13815-8.

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4

Zudin, Yuri B. Non-equilibrium Evaporation and Condensation Processes. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-67553-0.

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5

Srikanthan, R. Stochastic generation of rainfall and evaporation data. Canberra: Australian Govt. Pub. Service, 1985.

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6

Liquid-vapor phase-change phenomena: An introduction to the thermophysics of vaporization and condensation processes in heat transfer equipment. 2nd ed. New York: Taylor and Francis, 2008.

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7

Bagayoko, Fafré. Impact of land-use intensity on evaporation and surface runoff: Processes and parameters for eastern Burkina Faso, West Africa. Göttingen [Germany]: Cuvillier, 2006.

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8

Carey, V. P. Liquid-vapor phase-change phenomena: An introduction to the thermophysics of vaporization and condensation processes in heat transfer equipment. Washington, D.C: Hemisphere Pub. Corp., 1992.

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9

Rifert, V. G. Condensation heat transfer enhancement. Southampton: WIT Press, 2004.

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10

Mer, Victor K. La. Retardation of Evaporation by Monolayers: Transport Processes. Elsevier Science & Technology Books, 2014.

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11

Zudin, Yuri B. Non-Equilibrium Evaporation and Condensation Processes: Analytical Solutions. Springer International Publishing AG, 2021.

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12

Zudin, Yuri B. Non-equilibrium Evaporation and Condensation Processes: Analytical Solutions. Springer, 2018.

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13

Zudin, Yuri B. Non-equilibrium Evaporation and Condensation Processes: Analytical Solutions. Springer, 2017.

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14

Zudin, Yuri B. Non-equilibrium Evaporation and Condensation Processes: Analytical Solutions. Springer, 2019.

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15

Zudin, Yuri B. Non-Equilibrium Evaporation and Condensation Processes: Analytical Solutions. Springer International Publishing AG, 2022.

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16

Harman, Rebecca. The Water Cycle: Evaporation, Condensation and Erosion (Earth's Processes). Heinemann, 2005.

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17

C, Sud Y., Kim J. H, and Goddard Space Flight Center, eds. Intercomparison of hydrologic processes in global climate models. Greenbelt, Md: National Aeronautics and Space Administration, Goddard Space Flight Center, 1995.

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18

Carey, Van P. Liquid Vapor Phase Change Phenomena: An Introduction to the Thermophysics of Vaporization and Condensation Processes in Heat Transfer Equipment. 2nd ed. Taylor & Francis, 2007.

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19

Carey, Van P. Liquid-Vapor Phase-Change Phenomena: An Introduction to the Thermophysics of Vaporization and Condensation Processes in Heat Transfer Equipment, Third Edition. Taylor & Francis Group, 2020.

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20

Carey, Van P. Liquid-Vapor Phase-Change Phenomena: An Introduction to the Thermophysics of Vaporization and Condensation Processes in Heat Transfer Equipment, Third Edition. Taylor & Francis Group, 2020.

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21

Carey, Van P. Liquid Vapor Phase Change Phenomena: An Introduction to the Thermophysics of Vaporization and Condensation Processes in Heat Transfer Equipment, Third Edition. Taylor & Francis Group, 2020.

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22

Carey, Van P. Liquid-Vapor Phase-Change Phenomena: An Introduction to the Thermophysics of Vaporization and Condensation Processes in Heat Transfer Equipment, Third Edition. Taylor & Francis Group, 2020.

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23

Carey, Van P. Liquid-Vapor Phase-Change Phenomena: An Introduction to the Thermophysics of Vaporization and Condensation Processes in Heat Transfer Equipment, Third Edition. Taylor & Francis Group, 2020.

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24

Carey, Van P. Liquid Vapor Phase Change Phenomena: An Introduction to the Thermophysics of Vaporization and Condensation Processes in Heat Transfer Equipment, Second Edition. Taylor & Francis Group, 2018.

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25

Carey, Van P. Liquid Vapor Phase Change Phenomena: An Introduction to the Thermophysics of Vaporization and Condensation Processes in Heat Transfer Equipment, Second Edition. Taylor & Francis Group, 2018.

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26

Carey, Van P. Liquid Vapor Phase Change Phenomena: An Introduction to the Thermophysics of Vaporization and Condensation Processes in Heat Transfer Equipment, Second Edition. Taylor & Francis Group, 2018.

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27

Carey, Van P. Liquid Vapor Phase Change Phenomena: An Introduction to the Thermophysics of Vaporization and Condensation Processes in Heat Transfer Equipment, Third Edition. Taylor & Francis Group, 2018.

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28

Carey, Van P. Liquid Vapor Phase Change Phenomena: An Introduction to the Thermophysics of Vaporization and Condensation Processes in Heat Transfer Equipment, Second Edition. Taylor & Francis Group, 2018.

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29

Rifert, V. G., and H. F. Smirnov. Condensation Heat Transfer Enhancement (Developments in Heat Transfer). Wit Pr/Computational Mechanics, 2004.

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30

Yang, Kun. Observed Regional Climate Change in Tibet over the Last Decades. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.587.

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The Tibetan Plateau (TP) is subjected to strong interactions among the atmosphere, hydrosphere, cryosphere, and biosphere. The Plateau exerts huge thermal forcing on the mid-troposphere over the mid-latitude of the Northern Hemisphere during spring and summer. This region also contains the headwaters of major rivers in Asia and provides a large portion of the water resources used for economic activities in adjacent regions. Since the beginning of the 1980s, the TP has undergone evident climate changes, with overall surface air warming and moistening, solar dimming, and decrease in wind speed. Surface warming, which depends on elevation and its horizontal pattern (warming in most of the TP but cooling in the westernmost TP), was consistent with glacial changes. Accompanying the warming was air moistening, with a sudden increase in precipitable water in 1998. Both triggered more deep clouds, which resulted in solar dimming. Surface wind speed declined from the 1970s and started to recover in 2002, as a result of atmospheric circulation adjustment caused by the differential surface warming between Asian high latitudes and low latitudes.The climate changes over the TP have changed energy and water cycles and has thus reshaped the local environment. Thermal forcing over the TP has weakened. The warming and decrease in wind speed lowered the Bowen ratio and has led to less surface sensible heating. Atmospheric radiative cooling has been enhanced, mainly through outgoing longwave emission from the warming planetary system and slightly enhanced solar radiation reflection. The trend in both energy terms has contributed to the weakening of thermal forcing over the Plateau. The water cycle has been significantly altered by the climate changes. The monsoon-impacted region (i.e., the southern and eastern regions of the TP) has received less precipitation, more evaporation, less soil moisture and less runoff, which has resulted in the general shrinkage of lakes and pools in this region, although glacier melt has increased. The region dominated by westerlies (i.e., central, northern and western regions of the TP) received more precipitation, more evaporation, more soil moisture and more runoff, which together with more glacier melt resulted in the general expansion of lakes in this region. The overall wetting in the TP is due to both the warmer and moister conditions at the surface, which increased convective available potential energy and may eventually depend on decadal variability of atmospheric circulations such as Atlantic Multi-decadal Oscillation and an intensified Siberian High. The drying process in the southern region is perhaps related to the expansion of Hadley circulation. All these processes have not been well understood.
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31

Risk Reduction Engineering Laboratory (U.S.), ed. Recycling nickel electroplating rinse waters by low temperature evaporation and reverse osmosis: Project summary. Cincinnati, OH: U.S. Environmental Protection Agency, Risk Reduction Engineering Laboratory, 1993.

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32

Balaban, Miriam. Desalination and Water Re-Use: Proceedings of the 12th International Sympoisum : Evaporative Processes-Operations, Cogeneration Electrodialysis Mater. Hemisphere Pub, 1991.

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33

Harrison, Roger G., Paul W. Todd, Scott R. Rudge, and Demetri P. Petrides. Bioseparations Science and Engineering. Oxford University Press, 2015. http://dx.doi.org/10.1093/oso/9780195391817.001.0001.

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Designed for undergraduates, graduate students, and industry practitioners, Bioseparations Science and Engineering fills a critical need in the field of bioseparations. Current, comprehensive, and concise, it covers bioseparations unit operations in unprecedented depth. In each of the chapters, the authors use a consistent method of explaining unit operations, starting with a qualitative description noting the significance and general application of the unit operation. They then illustrate the scientific application of the operation, develop the required mathematical theory, and finally, describe the applications of the theory in engineering practice, with an emphasis on design and scaleup. Unique to this text is a chapter dedicated to bioseparations process design and economics, in which a process simular, SuperPro Designer® is used to analyze and evaluate the production of three important biological products. New to this second edition are updated discussions of moment analysis, computer simulation, membrane chromatography, and evaporation, among others, as well as revised problem sets. Unique features include basic information about bioproducts and engineering analysis and a chapter with bioseparations laboratory exercises. Bioseparations Science and Engineering is ideal for students and professionals working in or studying bioseparations, and is the premier text in the field.
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34

Wang, Bin. Intraseasonal Modulation of the Indian Summer Monsoon. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.616.

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The strongest Indian summer monsoon (ISM) on the planet features prolonged clustered spells of wet and dry conditions often lasting for two to three weeks, known as active and break monsoons. The active and break monsoons are attributed to a quasi-periodic intraseasonal oscillation (ISO), which is an extremely important form of the ISM variability bridging weather and climate variation. The ISO over India is part of the ISO in global tropics. The latter is one of the most important meteorological phenomena discovered during the 20th century (Madden & Julian, 1971, 1972). The extreme dry and wet events are regulated by the boreal summer ISO (BSISO). The BSISO over Indian monsoon region consists of northward propagating 30–60 day and westward propagating 10–20 day modes. The “clustering” of synoptic activity was separately modulated by both the 30–60 day and 10–20 day BSISO modes in approximately equal amounts. The clustering is particularly strong when the enhancement effect from both modes acts in concert. The northward propagation of BSISO is primarily originated from the easterly vertical shear (increasing easterly winds with height) of the monsoon flows, which by interacting with the BSISO convective system can generate boundary layer convergence to the north of the convective system that promotes its northward movement. The BSISO-ocean interaction through wind-evaporation feedback and cloud-radiation feedback can also contribute to the northward propagation of BSISO from the equator. The 10–20 day oscillation is primarily produced by convectively coupled Rossby waves modified by the monsoon mean flows. Using coupled general circulation models (GCMs) for ISO prediction is an important advance in subseasonal forecasts. The major modes of ISO over Indian monsoon region are potentially predictable up to 40–45 days as estimated by multiple GCM ensemble hindcast experiments. The current dynamical models’ prediction skills for the large initial amplitude cases are approximately 20–25 days, but the prediction of developing BSISO disturbance is much more difficult than the prediction of the mature BSISO disturbances. This article provides a synthesis of our current knowledge on the observed spatial and temporal structure of the ISO over India and the important physical processes through which the BSISO regulates the ISM active-break cycles and severe weather events. Our present capability and shortcomings in simulating and predicting the monsoon ISO and outstanding issues are also discussed.
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35

United States. National Aeronautics and Space Administration., ed. Development of comprehensive numerical schemes for predicting evaporating gas-droplets flow processes of a liquid-fueled combustor: Semi-annual report, June 15, 1988-November 30, 1988. [Washington, DC]: National Aeronautics and Space Administration, 1990.

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36

United States. National Aeronautics and Space Administration., ed. Analysis of composite ablators using massively parallel computation. [Washington, DC: National Aeronautics and Space Administration, 1995.

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