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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics</journal_title>
		<journal_url>www.atmos-chem-phys.net</journal_url>
		<issn>1680-7316</issn>
		<eissn>1680-7324</eissn>
		<volume_number>7</volume_number>
		<issue_number>13</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/acp-7-3497-2007</doi>
	<article_url>http://www.atmos-chem-phys.net/7/3497/2007/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/7/3497/2007/acp-7-3497-2007.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/7/3497/2007/acp-7-3497-2007.pdf</fulltext_pdf>
	<start_page>3497</start_page>
	<end_page>3505</end_page>
	<publication_date>2007-07-03</publication_date>
	<article_title content_type="html">The effects of heating by transported dust layers on cloud and precipitation: a numerical study</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>Y. Yin</name>
			<email>yyatnuist@yahoo.co.uk</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>L. Chen</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Nanjing University of Information Science and Technology, Nanjing 210044, China</affiliation>
	</affiliations>
	<abstract content_type="html">There have been numerous recent publications showing that mineral dust might
be a good absorber for solar radiation in addition to its capability to act
as cloud condensation nuclei (CCN) and ice forming nuclei (IFN), and could
lead to reduced cloud cover and precipitation in the region where it is
present. This effect is investigated using a dynamic cloud model with
detailed microphysics of both warm and ice phase processes. The model is
initialized using measured size distributions and concentrations of mineral
dust particles. Our results show that when dust appears at the cloud-base
height and below 3 km, where the temperature is warmer than &amp;minus;5&amp;deg;C, the
heating induced by the presence of dust layers can inhibit the formation of
cloud droplets and suppresses the development of precipitation, leading to
lower cloud optical depth and albedo. On the other hand, when the dust
layers are located at altitudes with temperature colder than &amp;minus;5&amp;deg;C, or
above the &amp;minus;5&amp;deg;C level, mineral aerosols can act as effective ice nuclei,
intensify the ice-forming processes, and may enhance the development of
cloud and precipitation. It is also found that the heating effect is more
pronounced in continental clouds than in maritime clouds.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Andreae, M. O., Charlson, R. J., Bruynseels, F., Storms, H., van Grieken, R., and Maenhaut, W.: Internal mixtures of sea salt, silicates and excess sulfate in marine aerosols, Science, 232, 1620&amp;ndash;1623, 1986. </reference>
		<reference numeration="2" content_type="text"> Bauer, S. E., Mishchenko, M. I., Lacis, A. A., Zhang, S., Perlwitz, J., and Metzger, S. M.: Do sulfate and nitrate coatings on mineral dust have important effects on radiative properties and climate modeling?, J. Geophys. Res., 112, D06307, doi:10.1029/2005JD006977, 2007. </reference>
		<reference numeration="3" content_type="text"> Cheng, T. and Shen, Z.: The radiative forcing of atmospheric dust in northwest China (in Chinese with English abstract), Plateau Meteorol., 21(5), 473&amp;ndash;478, 2002. </reference>
		<reference numeration="4" content_type="text"> Cooper, W. A. and Lawson, R. P.: Physical interpretation of results from the HIPLEX-1 experiment, J. Clim. Appl. Meteor., 23, 523&amp;ndash;540, 1984. </reference>
		<reference numeration="5" content_type="text"> Costa, M. J., Sohn, B.-J., Levizzani, V., and Silva, A. M.: Radiative forcing of Asian dust determined from the synergized GOME and GMS satellite data &amp;ndash; A case study, J. Meteorol. Soc. Jpn., 84, 85&amp;ndash;95, 2006. </reference>
		<reference numeration="6" content_type="text"> DeMott, P. J., Sassen, K., Poellot, M. R., et al.: African dust aerosols as atmospheric ice nuclei, Geophys. Res. Lett., 30(14), 1732, doi:10.1029/2003GL017410, 2003. </reference>
		<reference numeration="7" content_type="text"> Dubovik, O., Holben, B., Eck, T. F., et al.: Variability of absorption and optical properties of key aerosol types observed in worldwide locations, J. Atmos. Sci, 59, 590&amp;ndash;608, 2002. </reference>
		<reference numeration="8" content_type="text"> Huang, J., Minnis, P., Lin, B., et al.: Possible influences of Asian dust aerosols on cloud properties and radiative forcing observed from MODIS and CERES, Geophys. Res. Lett., 33, L06824, doi:10.1029/2005GL024724, 2006a. </reference>
		<reference numeration="9" content_type="text"> Huang, J., Lin, B., Minnis, P., et al.: Satellite-based assessment of possible dust aerosols semi-direct effect on cloud water path over East Asia, Geophys. Res. Lett., 33, L19802, doi:10.1029/2006GL026561, 2006b. </reference>
		<reference numeration="10" content_type="text"> Intergovernmental Panel on Climate Change (IPCC), World Meteorological Office, United Nations Environmental Programme: Summary for Policymakers, 2001. </reference>
		<reference numeration="11" content_type="text"> Israelevich, P. L., Levin, Z., Joseph, J. H., and Ganor, E.: Desert aerosol transport in the Mediterranean region as inferred from the TOMS aerosol index, J. Geophys. Res., 107(D21), 4572, doi:10.1029/2001JD002011, 2002. </reference>
		<reference numeration="12" content_type="text"> Jaenicke, R.: Aerosol physics and chemistry, in: Ladolt-Boernstein: Zahlenwerte und Funktionen aus Naturwissenschaften und Technik, Vol 4b, edited by: Fischer, G., Springer-Verlag, New York, 391&amp;ndash;457, 1988. </reference>
		<reference numeration="13" content_type="text"> Krauss, T. W., Bruintjes, R. T., Verlinde, J., and Kahn, A.: Microphysical and radar observations of seeded and unseeded continental cumulus clouds, J. Clim. Appl. Meteor., 26, 585&amp;ndash;606, 1987. </reference>
		<reference numeration="14" content_type="text"> Levin, Z., Ganor, E., and Gladstein, V.: The effects of desert particles coated with sulfate on rain formation in the eastern Mediterranean, J. Appl. Meteorol., 35, 1511&amp;ndash;1523, 1996. </reference>
		<reference numeration="15" content_type="text"> Levin, Z., Teller, A., Ganor, E., and Yin, Y.: On the interactions of mineral dust, sea salt particles and clouds &amp;ndash; Measurements and modeling study from the MEIDEX campaign, J. Geophys. Res., 110, D20202, doi:10.1029/2005JD005810, 2005. </reference>
		<reference numeration="16" content_type="text"> Lohmann, U. and Diehl, K.: Sensitivity Studies of the Importance of Dust Ice Nuclei for the Indirect Aerosol Effect on Stratiform Mixed-Phase Clouds, J. Atmos. Sci., 63, 968&amp;ndash;982, 2006. </reference>
		<reference numeration="17" content_type="text"> Niu, S., Zhang, C., and Sun, J.: A observational study of the particle spectra of dust aerosol over the Helan Mts. Region, Chinese J. Atmos. Sci., 25, 2, 243&amp;ndash;252, 2001. </reference>
		<reference numeration="18" content_type="text"> Prospero, J. M.: Long range transport of mineral dust in the global atmosphere: Impact of African dust on the environment of the southeastern United States, Proc. Nat. Acad. Sci., 96, 3396&amp;ndash;3403, 1999. </reference>
		<reference numeration="19" content_type="text"> Pruppacher, H. R. and Klett, J. D.: Microphysics of Clouds and Precipitation, D Reidel, 714~pp., 1997. </reference>
		<reference numeration="20" content_type="text"> Reisin, T., Levin, Z., and Tzivion, S.: Rain production in convective clouds as simulated in an axisymmetric model with detailed microphysics, Part I: Description of the model, J. Atmos. Sci., 53, 497&amp;ndash;519, 1996. </reference>
		<reference numeration="21" content_type="text"> Rosenfeld, D., Rudich, Y., and Lahav, R.: Desert dust suppressing precipitation: A possible desertification feedback loop, Proc. Natl. Acad. Sci. USA, 98, 11, 5975&amp;ndash;5980, 2001. </reference>
		<reference numeration="22" content_type="text"> Rudich Y., Khersonsky, O., and Rosenfeld, D.: Treating clouds with a grain of salt, Geophys. Res. Lett., 29, 22, 2060, doi:10.1029/2002GL016055, 2002. </reference>
		<reference numeration="23" content_type="text"> Teller, A. and Levin, Z.: The effects of aerosols on precipitation and dimensions of subtropical clouds: a sensitivity study using a numerical cloud model, Atmos. Chem. Phys., 6, 67&amp;ndash;80, 2006. </reference>
		<reference numeration="24" content_type="text"> Trochkine, D., Iwasaka, Y., Matsuki A., et al.: Mineral aerosol particles collected in Dunhuang, China, and their comparison with chemically modified particles collected over Japan, J. Geophys. Res., 108(D23), 8642, doi:10.1029/2002JD003268, 2003. </reference>
		<reference numeration="25" content_type="text"> Tzivion, S., Feingold, G., and Levin, Z.: A efficient numerical solution to the stochastic collection equation, J. Atmos. Sci., 44, 3139&amp;ndash;3149, 1987. </reference>
		<reference numeration="26" content_type="text"> Tzivion, S., Feingold, G., and Levin, Z.: The evolution of raindrop spectra. Part II: Collisional collection/breakup and evaporation in a rainshaft, J. Atmos. Sci., 46, 3312&amp;ndash;3327, 1989. </reference>
		<reference numeration="27" content_type="text"> Tzivion, S., Reisin, T., and Levin, Z.: A numerical solution of the kinetic collection equation using high spectral grid resolution: A proposed reference, J. Comput. Phys., 148, 527&amp;ndash;544, 1999. </reference>
		<reference numeration="28" content_type="text"> Wurzler, S., Reisin, T. G., and Levin, Z.: Modification of mineral dust particles by cloud processing and subsequent effects on drop size distributions, J. Geophys. Res., 105(D4), 4501&amp;ndash;4512, 2000. </reference>
		<reference numeration="29" content_type="text"> Yin, Y., Levin, Z., Reisin, T. G., et al.: The effect of giant cloud condensation nuclei on the development of precipitation in convective clouds &amp;ndash; A numerical study, Atmos. Res., 53, 91&amp;ndash;116, 2000. </reference>
		<reference numeration="30" content_type="text"> Yin, Y., Wurzler, S., Levin, Z., et al.: Effects on precipitation and cloud optical properties, J. Geophys. Res., 107(D23), 4724, doi:10.1029/2001JD001544, 2002. </reference>
		<reference numeration="31" content_type="text"> Yin, Y., Carslaw, K. S., and Feingold, G.: Vertical transport and processing of aerosols in a mixed-phase convective cloud and the feedback on cloud development, Q. J. Roy. Meteor. Soc., 131, 221&amp;ndash;246, 2005. </reference>
		<reference numeration="32" content_type="text"> Zhang, X. Y., Gong, S. L., Shen, Z. X., et al.: Characterization of soil dust aerosol in China and its transport and distribution during 2001 ACE-Asia: 1. Network observations, J. Geophys. Res., 108(D9), 4261, doi:10.1029/2002JD002632, 2003. </reference>
		<reference numeration="33" content_type="text"> Zhao, T. L., Gong, S. L., Zhang, X. Y., and McKendry, I. G.: Modeled size-segregated wet and dry deposition budgets of soil dust aerosol during ACE-Asia 2001: Implications for trans-Pacific transport, J. Geophys. Res., 108(D23), 8665, doi:10.1029/2002JD003363, 2003. </reference>
		<reference numeration="34" content_type="text"> Zhao, T. L., Gong, S. L., Zhang, X. Y., Blanchet, J. P., McKendry, I. G., and Zhou, Z. J.: A simulated climatology of Asian dust aerosol and its trans-Pacific transport. Part I: Mean climate and validation, J. Clim, 19, 88&amp;ndash;103, 2006. </reference>
	</references>
</article>

