2001
DOI: 10.1007/s00376-001-0046-9
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Recent researches on aerosol in china

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Cited by 31 publications
(4 citation statements)
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“…Change in aerosol level is one of the key factors determining variations in the radiative budget of the climate system. Long-term measurements of key aerosol optical properties are urgently needed to better understand climate changes, such as changes in surface irradiance (Wang et al 2001, Streets et al 2009. Aerosol optical depth (AOD) data from the Advanced Very High Resolution Radiometer (AVHRR) satellite were used to account for the dimming and brightening tendencies (Mishchenko et al 2007, Zhao et al 2008.…”
Section: Introductionmentioning
confidence: 99%
“…Change in aerosol level is one of the key factors determining variations in the radiative budget of the climate system. Long-term measurements of key aerosol optical properties are urgently needed to better understand climate changes, such as changes in surface irradiance (Wang et al 2001, Streets et al 2009. Aerosol optical depth (AOD) data from the Advanced Very High Resolution Radiometer (AVHRR) satellite were used to account for the dimming and brightening tendencies (Mishchenko et al 2007, Zhao et al 2008.…”
Section: Introductionmentioning
confidence: 99%
“…Few studies considered the different components of aerosols including the absorbing or scattering aerosols and the corresponding DRF, except for the work of [29], which introduced the size fractional optical parameters and the DRF of different aerosol components, as well as the aerosol physical properties of the different size fractions in urban Nanjing. Since aerosols have complicated compositions and distributions throughout the vast territory of East Asia, especially in rapidly developing regions [43,[105][106][107], considerable differences might exist in the absorbing aerosol optical and physical properties as well as the corresponding DRF among various sites in East Asia. A few studies illustrated the DRF in the UV band where the ADE can affect near-surface photochemistry.…”
Section: Introductionmentioning
confidence: 99%
“…While the main natural sources of aerosol in city include raising dust, sand storm, ashes, pollens and seeds, the artificial sources of aerosol come mainly from the particles sent to the air from industry, traffic, agriculture, and construction activities. At the same time, many gaseous pollutants, such as CO 2 , NO x , NH x , etc can be coagulated into aerosol particles through the process of condensation [3,4] . Through the process above, the aerosol within the PBL affects evidently the surface climate, temperature and pressure field, wind field and the vertical evolvement field, etc.…”
Section: Introductionmentioning
confidence: 99%