標(biāo)題: Titlebook: Aerosol Pollution Impact on Precipitation; A Scientific Review Zev Levin,William R. Cotton Book 2009 Springer Science+Business Media B.V. 2 [打印本頁(yè)] 作者: graphic 時(shí)間: 2025-3-21 16:49
書(shū)目名稱(chēng)Aerosol Pollution Impact on Precipitation影響因子(影響力)
書(shū)目名稱(chēng)Aerosol Pollution Impact on Precipitation影響因子(影響力)學(xué)科排名
書(shū)目名稱(chēng)Aerosol Pollution Impact on Precipitation網(wǎng)絡(luò)公開(kāi)度
書(shū)目名稱(chēng)Aerosol Pollution Impact on Precipitation網(wǎng)絡(luò)公開(kāi)度學(xué)科排名
書(shū)目名稱(chēng)Aerosol Pollution Impact on Precipitation被引頻次
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書(shū)目名稱(chēng)Aerosol Pollution Impact on Precipitation讀者反饋
書(shū)目名稱(chēng)Aerosol Pollution Impact on Precipitation讀者反饋學(xué)科排名
作者: 夾克怕包裹 時(shí)間: 2025-3-22 00:08
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作者: Aura231 時(shí)間: 2025-3-22 04:27 作者: figment 時(shí)間: 2025-3-22 05:44
http://image.papertrans.cn/a/image/150520.jpg作者: Adornment 時(shí)間: 2025-3-22 11:25
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作者: CESS 時(shí)間: 2025-3-22 13:42 作者: Thyroid-Gland 時(shí)間: 2025-3-22 18:25 作者: Infraction 時(shí)間: 2025-3-22 22:20 作者: 緯線(xiàn) 時(shí)間: 2025-3-23 01:35
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作者: ALLEY 時(shí)間: 2025-3-23 06:15
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作者: Desert 時(shí)間: 2025-3-23 12:56
Convergence or Divergence in Europe?over 50 years. Efforts to understand the processes involved have led to a significant body of knowledge about clouds and about the effects of the seeding aerosol. A number of projects focused on the statistical evaluation of whether a seeding effect can be distinguished in the presence of considerab作者: 結(jié)束 時(shí)間: 2025-3-23 15:30
Convergence and Divergence in External Traden and to a lesser extent altering the profile of IR absorption in the atmosphere. Second, by serving as cloud condensation nuclei (CCN) and ice nuclei (IN), they determine cloud microphysics, the formation of precipitating particles and cloud radiative properties, particularly cloud albedo and emiss作者: Radiation 時(shí)間: 2025-3-23 21:10 作者: Oafishness 時(shí)間: 2025-3-24 01:06 作者: Diaphragm 時(shí)間: 2025-3-24 04:30
In Situ and Remote Sensing Techniques for Measuring Aerosols, Clouds and Precipitation,In this chapter we review the methods presently available and expected in the near future to measure the effect of aerosols on clouds and precipitation, and the limitations of current measurements that make it difficult to assess this connection.作者: Femine 時(shí)間: 2025-3-24 07:58 作者: Cpap155 時(shí)間: 2025-3-24 12:02
978-90-481-7953-4Springer Science+Business Media B.V. 2009作者: dissent 時(shí)間: 2025-3-24 16:17
Introduction,le 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作者: 大約冬季 時(shí)間: 2025-3-24 22:57
Principles of Cloud and Precipitation Formation,t concepts are discussed, and terms defined, which will be used in later chapters. For more detail on these topics the reader is referred to textbooks by Pruppacher and Klett (1997), Rogers and Yau (1989), relevant chapters in Wallace and Hobbs (2006), Cotton and Anthes (1989), and Houze (1993) and 作者: 填滿(mǎn) 時(shí)間: 2025-3-25 01:06 作者: 疲勞 時(shí)間: 2025-3-25 07:10
The Distribution of Atmospheric Aerosols: Transport, Transformation and Removal,c aerosols, there is no location on the globe that is not influenced by aerosol sources. Once released into the atmosphere from primary production or produced via gas-to-particle conversion (for source details, see Chapter 3), aerosols are subject to many processes that affect their global distribut作者: 農(nóng)學(xué) 時(shí)間: 2025-3-25 10:45 作者: 貪婪的人 時(shí)間: 2025-3-25 12:55 作者: 約會(huì) 時(shí)間: 2025-3-25 17:24 作者: 小平面 時(shí)間: 2025-3-25 21:47 作者: 猛擊 時(shí)間: 2025-3-26 02:45 作者: Inflammation 時(shí)間: 2025-3-26 04:55
Book 2009in, 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 ev作者: Narcissist 時(shí)間: 2025-3-26 09:02 作者: agnostic 時(shí)間: 2025-3-26 14:41
Convergence or Divergence in Europe?, precipitation as well as processes occurring in cloud-free air. During the life cycle of an aerosol in the atmosphere, gas to particle conversion and mixing of aerosols from different sources changes the chemical, physical and optical properties of the original aerosols.作者: BOON 時(shí)間: 2025-3-26 19:30 作者: 孤獨(dú)無(wú)助 時(shí)間: 2025-3-26 23:10
The Distribution of Atmospheric Aerosols: Transport, Transformation and Removal,, precipitation as well as processes occurring in cloud-free air. During the life cycle of an aerosol in the atmosphere, gas to particle conversion and mixing of aerosols from different sources changes the chemical, physical and optical properties of the original aerosols.作者: 外貌 時(shí)間: 2025-3-27 03:37 作者: triptans 時(shí)間: 2025-3-27 08:54 作者: nonchalance 時(shí)間: 2025-3-27 13:12
Convergence or Divergence in Europe?cloud droplet number concentration (CDNC), hence increasing cloud microphysical stability and potentially reducing precipitation efficiency. Although the connection between increased CCN and increased CDNC has been supported by many in situ observations, the impact of CCN on precipitation is less well established.作者: Accolade 時(shí)間: 2025-3-27 14:13 作者: REIGN 時(shí)間: 2025-3-27 19:59 作者: amputation 時(shí)間: 2025-3-28 00:57
Effects of Pollution and Biomass Aerosols on Clouds and Precipitation: Observational Studies,cloud droplet number concentration (CDNC), hence increasing cloud microphysical stability and potentially reducing precipitation efficiency. Although the connection between increased CCN and increased CDNC has been supported by many in situ observations, the impact of CCN on precipitation is less well established.作者: DOSE 時(shí)間: 2025-3-28 05:59
Parallels and Contrasts Between Deliberate Cloud Seeding and Aerosol Pollution Effects,the general question of aerosol effects on precipitation. Definite proof from the seeding projects for an induced increase in precipitation as a result of the addition of seeding material to the clouds would represent a powerful demonstration of at least one type of dominant aerosol-precipitation link in the clouds involved.作者: 羽飾 時(shí)間: 2025-3-28 08:17
Summary,can therefore affect regional cloud properties and may affect precipitation amounts. If these effects are large enough, they could adversely affect water availability, and will impact global climate by changing land-surface radiative properties and surface energy budgets, which can alter the general circulation of the atmosphere and climate.作者: 決定性 時(shí)間: 2025-3-28 12:30
ho discuss in detail the most recent findings in the field.T.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 ba作者: 口味 時(shí)間: 2025-3-28 15:02
T.–T. Kim,Muhan Choi,Yushin Kim,Bumki Min via wind-driven evaporation and biosphere-modulated evapo/transpiration followed by transport and dispersion, multiple cycles of cloud formation/evaporation, and ultimately removal as precipitation (rain or snow) or by fog water deposition or dew formation.作者: Reservation 時(shí)間: 2025-3-28 19:22
Ultrabroadband Terahertz Spectroscopy by Pruppacher and Klett (1997), Rogers and Yau (1989), relevant chapters in Wallace and Hobbs (2006), Cotton and Anthes (1989), and Houze (1993) and review articles by Stewart (1985) and Cantrell and Heymsfield (2005).作者: LVAD360 時(shí)間: 2025-3-29 01:52
Olivier de Bandt,Jean-Pierre Villetelleynamical parameters (i.e. updraft velocity) on the number and size distribution of cloud droplets. To this day similar models are in wide use to examine the effects of aerosol composition and atmospheric trace gases on droplet activation (e.g. Kulmala et al. 1993; Ghan et al. 1997; Feingold and Chuang 2002; Nenes et al. 2002).作者: Costume 時(shí)間: 2025-3-29 05:42 作者: 羅盤(pán) 時(shí)間: 2025-3-29 08:26 作者: jaunty 時(shí)間: 2025-3-29 13:59
