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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>8</volume_number>
		<issue_number>16</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acp-8-4547-2008</doi>
	<article_url>http://www.atmos-chem-phys.net/8/4547/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/8/4547/2008/acp-8-4547-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/8/4547/2008/acp-8-4547-2008.pdf</fulltext_pdf>
	<start_page>4547</start_page>
	<end_page>4558</end_page>
	<publication_date>2008-08-06</publication_date>
	<article_title content_type="html">Variability of cirrus clouds in a convective outflow during the Hibiscus campaign</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>F. Fierli</name>
			<email>f.fierli@isac.cnr.it</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>G. Di Donfrancesco</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>F. Cairo</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>V. MarÃ©cal</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>M. Zampieri</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>E. Orlandi</name>
		</author>
		<author numeration="7" affiliations="4,5">
			<name>G. Durry</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Istituto di Scienze dell&apos;Atmosfera e del Clima, CNR, Italy</affiliation>
		<affiliation numeration="2" content_type="html">Ente Nazionale Energia e Ambiente, Dipartimento Clima, Italy</affiliation>
		<affiliation numeration="3" content_type="html">Laboratoire de Physique et Chimie de l&apos;Environnement, CNRS and UniversitÃ© d&apos;OrlÃ©ans, France</affiliation>
		<affiliation numeration="4" content_type="html">Groupe de Spectroscopie MolÃ©culaire et AtmosphÃ©rique, CNRS and UniversitÃ© de Reims, France</affiliation>
		<affiliation numeration="5" content_type="html">Service d&apos;AÃ©ronomie, CNRS and Institut Pierre et Simon Laplace, France</affiliation>
	</affiliations>
	<abstract content_type="html">Light-weight microlidar and water vapour measurements were taken on-board a
stratospheric balloon during the HIBISCUS 2004 campaign, held in Bauru,
Brazil (49&amp;deg; W, 22&amp;deg; S). Cirrus clouds were observed throughout
the flight between 12 and 15 km height with a high mesoscale variability in
optical and microphysical properties. It was found that the cirrus clouds
were composed of different layers characterized by marked differences in
height, thickness and optical properties. Simultaneous water vapour
observations show that the different layers are characterized by different
values of the saturation with respect to ice. A mesoscale simulation and a
trajectory analysis clearly revealed that the clouds had formed in the
outflow of a large and persistent convective region and that the observed
variability of the optical properties and of the cloud structure is likely
linked to the different residence times of the convectively-processed air in
the upper troposphere.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Ackerman, T. P., Liou, K.-N., Valero P. J., and Pfister L.: Heating rates in tropical anvils, J. Atmos. Sci., 45, 1606â€“1623, 1988. </reference>
		<reference numeration="2" content_type="text"> Buzzi, A. and Foschini, L.: Mesoscale meteorological features associated with heavy precipitation in the southern Alpine region, Meteorol. Atmos. Phys., 72, 131â€“146, 2000. </reference>
		<reference numeration="3" content_type="text"> Corti T., Luo, B. P., Fu, Q., Vomel, H., and Peter, T.: The impact of cirrus clouds on tropical troposphere-to-stratosphere transport, Atmos. Chem. Phys., 6, 2539â€“2547, 2006. </reference>
		<reference numeration="4" content_type="text"> Davies H. C.: A lateral boundary formulation for multilevel prediction models, Q. J. R. Meteorol. Soc., 102, 405â€“418, 1976. </reference>
		<reference numeration="5" content_type="text"> Dessler, A. E. and Yang, P.: The Distribution of Tropical Thin Cirrus Clouds Inferred from Terra MODIS Data, J. Climate, 16, 1241â€“1247,2003. </reference>
		<reference numeration="6" content_type="text"> Di Donfrancesco, G., Cairo, F., Buontempo, C., et al. : Balloonborne Lidar for cloud physics studies, Appl. Opt., 42, 22, 5701â€“5708, 2006. </reference>
		<reference numeration="7" content_type="text"> Durry, G., Huret, N., Hauchecorne, A., Marecal, V., Pommereau, J.-P., Jones, R. L., Held, G., Larsen, N., and Renard, J.-B.: Isentropic advection and convective lifting of water vapor in the UT - LS as observed over Brazil (22&amp;deg; S) in February 2004 by in situ high-resolution measurements of H2O, CH4, O3 and temperature, Atmos. Chem. Phys. Discuss., 6, 12469â€“12501, 2006. </reference>
		<reference numeration="8" content_type="text"> Folkins, I. and Martin, R.V.: The vertical structure of tropical convection and its impact on the budgets of water vapor and ozone, J. Atmos. Sci.,62, 1560â€“1573, 2005. </reference>
		<reference numeration="9" content_type="text"> Fueglistaler, S., Bonazzola, M., Haynes, P. H., Peter, T.: Stratospheric water vapor predicted from the Lagrangian temperature history of air entering the stratosphere in the tropics, J. Geophys. Res., 110, D08107, doi:10.1029/2004JD005516, 2005. </reference>
		<reference numeration="10" content_type="text"> Fueglistaler, S. and Fu, Q.: Impact of clouds on radiative heating rates in the tropical lower stratosphere, J. Geophys. Res., 111, D23202, doi:10.1029/2006JD007273, 2006. </reference>
		<reference numeration="11" content_type="text"> Gettelman, A., Salby, M. L., and Sassi, F.: Distribution and influence of convection in the tropical tropopause region, J. Geophys. Res.-Atmos.,1737â€“1746, doi:1029/2006JD004080, 2002. </reference>
		<reference numeration="12" content_type="text"> Gheusi, F. and Stein, J.: Lagrangian description of airflows using Eulerian passive tracers, Q. J. R. M. S., 128, 579, 337â€“360, 2002. </reference>
		<reference numeration="13" content_type="text"> Hartmann, R. L.: Radiative effects of clouds on Earth&apos;s climate. Aerosol-Cloud-Climate Interactions,International Geophysical Series, 54, Academic Press, P. V. Hobbs Editor, 151â€“173, 1993. </reference>
		<reference numeration="14" content_type="text"> Holton, J. R., Haynes, P. H. , Douglass, A. R., Rood ,R. B., and Pfister, L.: Stratosphere-troposphere exchange. Rev. Geophys., 33(4),403â€“439, 1995. </reference>
		<reference numeration="15" content_type="text"> Kain, J. S. and Fritsch, J. M.: A one-dimensional entraining/detraining plume model and its application in convective parameterization. J. Atmos. Sci., 47, 2784â€“2802, 1990. </reference>
		<reference numeration="16" content_type="text"> Kain, J. S. and Fritsch, J. M.: Multiscale Convective Overturning in Mesoscale Convective Systems: Reconciling Observations, Simulations, and Theory, Mon. Wea. Rev., 126, 2254â€“2273, 1998. </reference>
		<reference numeration="17" content_type="text"> Kain J. S.: The Kain-Fritsch convective parametrization: an update, J. App. Meteorol., 43, 170â€“181, 2004. </reference>
		<reference numeration="18" content_type="text"> King, M. A., Chee, S., Platinick, S. E., Wang, M., and Liou, K.: Cloud Retrieval Algorithms for MODIS: Optical Thickness, Effective Particle Radius, and Thermodynamic Phase, Algorithm Theoretical Basis Document No ATBD-MOD-MOD06 Cloud product, 1997. </reference>
		<reference numeration="19" content_type="text"> Lehman, R.: On the choice of relaxation coefficients for Davies&apos; lateral boundaries scheme for regional weather prediction models, Meteorol. Atmos. Phys., 52, 1â€“14, 1993. </reference>
		<reference numeration="20" content_type="text"> Liou, K.-N.: Influence of cirrus clouds on weather and climate processes: A global perspective, 1986, Mon. Wea. Rev., 114, 1167â€“1200, 1986. </reference>
		<reference numeration="21" content_type="text"> Liu, L. and Mishchenko, M. I.: Constraints on PSC particle microphysics derived from lidarobservations, Journal of Quantitative Spectroscopy and Radiative Transfer, 70, 817â€“831, 2001. </reference>
		<reference numeration="22" content_type="text"> Liu, C. and Zipser, E. J.: Global distribution of convection penetrating the tropical tropopause, J. Geophys. Res., 110, D23104, doi:10.1029/2005JD006063, 2005. </reference>
		<reference numeration="23" content_type="text"> Mace, G. G., Zhang, Y., Platnick, S., King, M. D., Minnis, P., and Yang, P.: Evaluation of Cirrus Cloud Properties Derived from MODIS Data Using Cloud Properties Derived from Ground-Based Observations Collected at the ARM SGP Site, J. Appl. Meteorol., 44, 221â€“240, 2005. </reference>
		<reference numeration="24" content_type="text"> Mace, G. G., Benson, S., and Vernon, E.: Cirrus Clouds and the Large-Scale Atmospheric State: Relationships Revealed by Six Years of Ground-Based Data, J. Climate, 19, 3257â€“3278, doi:10.1175/JCLI3786.1, 2006. </reference>
		<reference numeration="25" content_type="text"> MarÃ©cal V., Durry G., Longo K., Freitas S., Riviere E.D. and M. Pirre: Mesoscale modelling of water vapour in the tropical UTLS: two case studies from the HIBISCUS campaign, Atmos. Chem. Phys., 7, 1471â€“1489, 2007. </reference>
		<reference numeration="26" content_type="text"> Marti, L. and Mauersberger, K.:A survey and new measurements of ice vapor pressure at temperatures between 170 and 250 K, Geophys. Res. Lett., 20, 363â€“366, 1993. </reference>
		<reference numeration="27" content_type="text"> Massie, S., Gettelman, A., Randel, W., and Baumgardner, D.: Distribution of tropical cirrus in relation to convection, J. Geophys. Res., 107(D21), 4591, doi:10.1029/2001JD001293, 2002. </reference>
		<reference numeration="28" content_type="text"> McFarquhar, G. M. and Heymsfield, A. J.: Microphysical characteristics of three anvils sampled during the Central Equatorial Pacific Experiment, J. Atmos. Sci.,53, 2401â€“2423, 1996. </reference>
		<reference numeration="29" content_type="text"> Morcrette, J. J., Clough, S. A., Mlawer, E. J., and Iacono, M. J.: Impact of a validated radiative transfer scheme, RRTM, on the ECMWF model climate and 10-day forecasts. ECMWF Technical Memo., 252, 1998. %</reference>
		<reference numeration="30" content_type="text"> %Mullendore G.L., D.R. Durran, Holton J.R.: Cross.tropopause tracer transport in midlatitude convection, J. Geophys. Res., 116, D06113, doi:10.129/2004JD005059, 2005 </reference>
		<reference numeration="31" content_type="text"> Noel, V., Winker, D. M., McGill, M., and Lawson P.:Classification of particle shapes from lidar depolarization ratio in convective ice clouds compared to in situ observations during CRYSTAL-FACE, J. Geophys. Res., 109, D24213, doi:10.1029/2004JD004883, 2004. </reference>
		<reference numeration="32" content_type="text"> Pfister, L., Selkirk, H. B., Jensen, E. J., et al.: Aircraft observations of thin cirrus clouds near the tropical tropopause, J. Geophys. Res., 106(D9), 9765â€“9786, 2001. </reference>
		<reference numeration="33" content_type="text"> Pommereau, J.-P., Garnier, A., Held, G., Gomes, A.-M., Goutail, F., Durry, G., Borchi, F., Hauchecorne, A., Montoux, N., Cocquerez, P., Letrenne, G., Vial, F., Hertzog, A., Legras, B., Pisso, I., Pyle, J. A., Harris, N. R. P., Jones, R. L., Robinson, A., Hansford, G., Eden, L., Gardiner, T., Swann, N., Knudsen, B., Larsen, N., Nielsen, J., Christensen, T., Cairo, F., Pirre, M., Marécal, V., Huret, N., Riviére, E., Coe, H., Grosvenor, D., Edvarsen, K., Di Donfrancesco, G., Ricaud, P., Berthelier, J.-J., Godefroy, M., Seran, E., Longo, K., and Freitas, S.: An overview of the HIBISCUS campaign, Atmos. Chem. Phys. Discuss., 7, 2389â€“2475, 2007. </reference>
		<reference numeration="34" content_type="text"> Pressman, D. J.: Chislennaja model&apos; gidrotermicheskikh processov v pochve kak chast&apos; skhemy mezomasshtabnogo prognoza (A numerical model of hydrothermical processes in soil as a part of a mesoscale weather forecast scheme), Meteorologiya i gidrologiya (Meteorology and Hydrology), 11, 62â€“75, 1994 (in Russian). </reference>
		<reference numeration="35" content_type="text"> Ren, C., MacKenzie, A. R., Schiller, C., Shur, G., and Yushkov, V.: Diagnosis of processes controlling water vapour in the tropical tropopause layer by a Lagrangian cirrus model, Atmos. Chem. Phys., 7, 5401â€“5413, 2007. </reference>
		<reference numeration="36" content_type="text"> Ritter, B. and Geleyn, J.: A comprehensive radiation scheme for numerical weather prediction models with potential applications in climate simulations, Mon. Wea. Rev., 120, 303â€“325, 1992. </reference>
		<reference numeration="37" content_type="text"> Sassen, K. and Benson, S.: A Midlatitude Cirrus Cloud Climatology from the Facility for Atmospheric Remote Sensing. Part II: Microphysical Properties Derived from Lidar Depolarization, Journal of Atmospheric Sciences, 58, 2103â€“2112, 2001. </reference>
		<reference numeration="38" content_type="text"> Saunders, R. and Brunel, P.: RTTOV 8.5 user guide, EUMETSAT SAFNWP http://www.metoffice.gv.uk/research/interproj/nwpsaf/rtm/, 2004. </reference>
		<reference numeration="39" content_type="text"> Schultz, P.: An explicit cloud physics parameterization for operational numerical weather prediction, Mon. Wea. Rev, 123, 3331â€“3343, 1995. </reference>
		<reference numeration="40" content_type="text"> Shibata T., Voemel H., Hamdi S., Kaloka S., Hasebe F., Fujiwara M., and Shiotani M.: Tropical cirrus near cold point tropopause under ice supersaturated condition observed by lidar and balloon-borne cryogenic frost point hygrometer, J. Geophys. Res., 112, D03210, doi:10.1029/2006JD007631, 2007. %</reference>
		<reference numeration="41" content_type="text"> %Stohl, A., Haimberger L., Scheele M.P., Wernli H.: An intercomparison of results from three %trajectory models, Meteorol. Applications, 127â€“135, 1999 </reference>
		<reference numeration="42" content_type="text"> Tompkins A. M., Gierens, K., and Radel G.: Ice Supersaturation in the ECMWF Integrated Forecast System, ECMWF technical memorandum, 481, 2005. </reference>
		<reference numeration="43" content_type="text"> Wang, P. H., Minnis, P., McCormick, M. P., Kent, G. S., and Skeens, K. M.: A 6-year climatology of cloud occurence frequency from Stratospheric Aerosol and Gas Experiment II observations (1985â€“1990), J. Geophys. Res., 101, 29 407â€“29 429, 1996. </reference>
		<reference numeration="44" content_type="text"> Whiteway, J., Cook, C., Gallagher, M., et al.: Anatomy of cirrus clouds: Results from the Emerald airborne campaigns, Geophys. Res. Lett., 31, L24102, doi:10.1029/2004GL021201, 2004. </reference>
		<reference numeration="45" content_type="text"> Zampieri, M., Buzzi A., and Malguzzi, P.: Sensitivity of quantitative precipitation forecasts to boundary layer parameterization: a flash flood case study in the Western Mediterranean, Nat. Hazards Earth Syst. Sci., 5, 603â€“612, 2005. </reference>
	</references>
</article>

