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Titlebook: Aerosol Pollution Impact on Precipitation; A Scientific Review Zev Levin,William R. Cotton Book 2009 Springer Science+Business Media B.V. 2

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發(fā)表于 2025-3-21 16:49:27 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
期刊全稱(chēng)Aerosol Pollution Impact on Precipitation
期刊簡(jiǎn)稱(chēng)A Scientific Review
影響因子2023Zev Levin,William R. Cotton
視頻videohttp://file.papertrans.cn/151/150520/150520.mp4
發(fā)行地址A comprehensive review of the effects of aerosol pollution, including biomass burning, on precipitation.Each article is written by experts who discuss in detail the most recent findings in the field.T
圖書(shū)封面Titlebook: Aerosol Pollution Impact on Precipitation; A Scientific Review Zev Levin,William R. Cotton Book 2009 Springer Science+Business Media B.V. 2
影響因子.Life on Earth is critically dependent upon the continuous cycling of water between oceans, continents and the atmosphere. Precipitation (including rain, snow, and hail) is the primary mechanism for transporting water from the atmosphere back to the Earth’s surface. It is also the key physical process that links aspects of climate, weather, and the global hydrological cycle. Changes in precipitation regimes and the frequency of extreme weather events, such as floods, droughts, severe ice/snow storms, monsoon fluctuations and hurricanes are of great potential importance to life on the planet. One of the factors that could contribute to precipitation modification is aerosol pollution from various sources such as urban air pollution and biomass burning. Natural and anthropogenic changes in atmospheric aerosols might have important implications for precipitation by influencing the hydrological cycle,?which in turn could feed back to climate changes...From an Earth Science perspective, a key question is how changes expected in climate will translate into changes in the hydrological cycle, and what trends may be expected in the future. We require a much better understanding and hence pre
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tive, a key question is how changes expected in climate will translate into changes in the hydrological cycle, and what trends may be expected in the future. We require a much better understanding and hence pre978-90-481-7953-4978-1-4020-8690-8
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T.–T. Kim,Muhan Choi,Yushin Kim,Bumki Minle depicted as a cartoon in Fig. 1.1 is dynamic and complex. The atmospheric component of this cycle involves surface water moving into the atmosphere via wind-driven evaporation and biosphere-modulated evapo/transpiration followed by transport and dispersion, multiple cycles of cloud formation/evap
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Convergence or Divergence in Europe?centrations and size distributions), and precipitation has received a great deal of attention for over 50 years. The pioneering work of Gunn and Phillips (1957), Squires (1958), Squires and Twomey (1961), Warner (1968) and Warner and Twomey (1967), to mention just a few, pointed out that high concen
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Olivier de Bandt,Jean-Pierre Villetelleconsidered the growth of a population of aerosol particles in a rising parcel of air. Models such as these addressed the effects of both aerosol and dynamical parameters (i.e. updraft velocity) on the number and size distribution of cloud droplets. To this day similar models are in wide use to exami
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