List of <strong>Abstracts</strong> 167the highest value in the industrial sites. Whereas, other metals i.e. Cr, Ni, Cu and Pb showed the highestvalue the in commercial sites. The toxic metals i.e. As, Hg and Se species are quantified. The correlation ofthe metals with ions i.e. Cl-, NO3-, SO42-, Na+, K+, Mg2+ and Ca2+ are described. The sources of themetals and ions are apportioned by using various models.P-Observations 2.9 ID:4370 10:30Atmospheric composition over Namibia (austral Africa) from the MOZAIC programme.Jean-Pierre Cammas 1 , Bastien Sauvage 1 , Jérémy Vouzelaud 1 , Romain Bort 1 , Jérôme Coquelin 1 , ValérieThouret 1 , Philippe Nédélec 1 , Jean-Marc Cousin 1 , Jérôme Brioude 2 , Herman Smit 3 , Andreas Volz-Thomas 31 CNRS, Université de Toulouse, France2 NOAA, ESRL, Boulder, CO, USA3 Institut fuer Chemie und Dynamik der Geosphaere 2, Forschungszentrum Juelich, GermanyContact: Jean-Pierre.Cammas@aero.obs-mip.frThe general aim is to document the climatology of vertical profiles over Windhoek (Namibia) from 2006-2008 MOZAIC data. This dataset is very dense, i.e. two profiles per day every two day for ozone, carbonmonoxide and meteorological parameters. Windhoek is pretty far away from the African regions whereozone precursors are emitted, either from biomass fires, or from deep continental convection (LiNOx), orfrom anthropogenic sources. It is a place where the impact of long-range transport of these emissions can bedocumented. We will focus on the two seasons during which intra-seasonal variabilities are the largest, i.e.spring (SON) and summer (DJF). During SON, intra-seasonal variabilities come from the long-rangetransport of lower- and upper-tropospheric CO plumes emitted by biomass fires over both southern Africaand southern America. SON is also the season during which stratospheric intrusions may have an impact onthe upper tropospheric ozone distribution down to the latitude of Windhoek (22S). During DJF, intraseasonalvariabilities come from the long-range transport of mid- and upper-tropospheric O3 plumes that weintend to attribute to ozone production processes activated by LiNOx emissions over convective regions bothover southern Africa and southern America.The results show (i) the climatology in SON and DJF, (ii) representative case studies of each class (i.e., lowtroposphericand upper-tropospheric CO plumes, stratospheric intrusions, LiNOx plumes), (iii) the historyand origin of case studies using the Lagrangian dispersion model Flexpart and satellite data for the detectionof biomass fires and lightning flashes, and (iv) MOZAIC composites of every class of plumes anddifferences between the composite and the climatology. General characteristics of the plumes, as well ascomponents of intra-seasonal variabilities coming either from the long-range transport (meteorologicalsituation) or from the emissions are discussed.P-Observations 2.10 ID:4374 10:30Lulin Atmospheric Background Station (LABS, 2,862m MSL): A newly established baseline site inEast AsiaNeng-Huei Lin 1 , Jia-Lin Wang 2 , Chung-Te Lee 3 , Guey-Rong Sheu 11 Department of Atmospheric Sciences, National Central University2 Department of Chemistry, National Central University3 Graduate Institute of Environmental Engineering, National Central UniversityContact: nhlin@cc.ncu.edu.twThe Lulin Atmospheric Background Station (LABS) in Taiwan held its grand opening for operation on 13April 2006. It is located at the Mt. Lulin (2,862 m MSL; 230 28'07"N, 120052’25"E) in central Taiwan. TheiCACGP-<strong>IGAC</strong> 2010 14 July, 2010
List of <strong>Abstracts</strong> 168LABS is unique because its location and altitude can enhance the global network of GAW (GlobalAtmosphere Watch) in the Southeast Asian region where no high-elevation baseline station is available. Oursite is located between the GAW Waliguan station (3,810 m) in Tibetian plateau and Mauna LaoObservatory (3,397m) in Hawaii. Trajectory study indicates that this site provides us a great of opportunityto observe a variety of air masses originated from source regions, giving a distinctive contrast of atmosphericchanges. Present continuous operations include precipitation chemistry, aerosol chemistry, trace gases (CO,CO2, O3, CFCs, NOy), mercury, atmospheric radiation, and meteorological variables. Mission orientedmeasurements of HCFCs, HFCs, and VOCs were also performed on a needed basis, mainly to helpdeconvolute long range transport phenomena from local circulation. Till present time, the averageconcentrations of CO, O3 and PM10 are about 121 ppb, 34 ppb and 10 microgram m-3, respectively. Theaverage pH value of precipitation is 5.73 with the major ions of SO42-, NO3- and NH4+. The averageconcentrations of mercury such as GEM, RGM and PHg are about 1.78 ng m-3, 41.7 pg m-3 and 9.0 pg m-3,respectively. The average aerosol optical depth is 0.101. The background concentrations of CO, O3 andPM10 are estimated to be about µ82 ppb, 28 ppb and 6 microgram m-3, respectively. About 32 % of thedays in a year can be categorized as polluted, which mainly occurred in March, and the concentrations ofabove three pollutants could elevate to as high as twice their background values. To summarize the results,the maximum concentration of pollutants generally occurred during spring time, especially in March,corresponding to the biomass burning from SE Asia. The LABS is also one of US/NOAA CCGG networkand NASA AeroNet. Relevant data will be presented.P-Observations 2.11 ID:4360 10:30Trace Species over the Central Himalayan and Indo-Gangetic Plain Regions: Contribution ofRegional Pollution and Long-range TransportManish Naja 1 , N. Ojha 1 , R. Kumar 1 , T. Sarangi 1 , H. Joshi 1 , P. Pant 1 , K.P. Singh 2 , Y. Kant 3 , S.Venkatramani 4 , S. Lal 41 ARIES, Nainital, India2 GBPUA&T, Pantnagar, India3 IIRS, Dehradun, India4 PRL, Ahmedabad, IndiaContact: manish@aries.res.inSatellite based observations and model results show that the northern India is the most polluted region inIndia. In view of this, for the first time, observations of various trace gases (O3, NO-NOy, CO, SO2, CO2and Hydrocarbons), aerosols (AOD, black carbon, aerosol number concentration and chemical composition)and meteorological parameters are initiated at a high altitude site (Nainital, 29.4N, 79.5E, 1958m) in thecentral Himalayas. Surface ozone and black carbon observations are also made at two other low altitude sites(Pantnagar, 29.0N, 79.5E, 231m; Dehradun, 30.3N, 78.1E, 640m) in the Indo-Gangetic regions.Observations at Nainital are representative of regional environment in the Northern Indian subcontinent andare also useful to study influences of long-range transport. Observations at Pantnagar and Dehradun are usedfor studying sources of regional pollution.Observations of ozone, NO-NOy and CO suggest that daytime net ozone production is not dominating overNainital. While other two sites show daytime higher ozone typical of urban/rural sites. In contrast to thediurnal variations, seasonal variations are more-or-less similar at these three sites with a spring maxima andsummer/monsoon minima. Seasonal variations in trace species over this region are different than those overthe western India. Based on residence time of air masses, net ozone production over Northern IndianSubcontinent in regionally-polluted air masses is estimated to be ~3 ppbv/day in spring but no clear build-upis seen in other months. Background ozone levels are estimated to be 30-35 ppbv and contribution of long-iCACGP-<strong>IGAC</strong> 2010 14 July, 2010
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List of Authors 237Beck, Veronica .
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List of Authors 251Van Donkelaar, A