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55 1.5 10 .42 : 551. 591 : 551.593.4 Atmospheric extinction related to aerosol mass concentration and meteorolog ical conditions in the atmosphere of Qena (Egypt) SAYEO M. EL·SHAZLY. AllDELAZ EEM M. ABDEL MAG EED . GAM IL Y. HASSAN and llADRY NOBI 1. 1I ' mrator.1' 01' Atm ospheric Physics, Dept. of Physics. Qena ( Received 22 ,lugu.' 198 9 ) ""'" 'IR'O. 'I'I'l'lT'<;fr7 .... " q f" F "'''';Hrq r,,"'n iT for """iT ""r or" r;,;,,; 'TllI I lrnVT iR "'r<'" q it. 'T9T 97IT'n 'Wl lfTi": ;n, 'Wf11R 3flT'RoT m 'l i:r , ;;; <f 'f.T :R1J I f ;r,- "" <r?"f iTf 'I) 'P"l"fT ( l'ff. ir W "fir I• f"f"frT Jfrn<:iu b !:f;=i} :r. 'fT'f 'f l; fr.'ir rn r I ., . AHSTRACT. The depe nde nce of the utrnosphcric extinction on aerosols concentration, tempe ratu re anti wind speed is demon strated. The atmospheric extinction was determined by measu ring the transmission loss of radiation from u lighl source across 36 em path with J photcccl! detector. C o-clu-i ons include a general associa- lion of high extinction with high aerosols concentration. tem pera tu re and wind speed . but there arc no one-to- one relatio nships . A correlat ion study between the extinction coefficient and each of these parame ters was per- formed, Ke)' words c-Air pollution. Atmo-p hcrlc cxnnct lon . Atm osphe ric vi"il'lilily. Aenuol particles, Concentration. co nditi on... I. In uoductlon The environmental impacts of air pollutant... involve several cflccts on the earth's atmosphere and on atmo...- pheric proces... ev, One or the I1Hh t important effect, i ... the reduction or atmosph er ic vi-ihility. Particulate emission of dusts. fumes, fl y ash. and othersolid pa r! i- cles. which b gene ral ly classed a'" acrovol particles. is the O1 O :o,t common po llu tants with potential visibility impacts (Robinson 1984). The need 10 measure the amount of particulate ail pollutants ha s. produced an incrca ... ed intere st in a possible relation between atmospheric extinction and the mass concentrai ion of particulate matter in the atmosphere. The relation- ship between these two variablev has pri ma rily been studied in other work' {e.g.. Charl son 196Q. Noll <'I al. 1968. Pilat and Ensor 1970. 1971. Patterson and Gillcte 1976 and Chylek (' I al. 1979). The results of many of these studies indicate that the exi..tence of an unambi- glIO U'" relation between the extinction a nd the rnav concentration is limited. There arc also a number of meteorological factors that arc important in the deter- mination of extinction coeffi cient owing rc their effect -, on both the concentration of at mospheric part icles and their size (Robinson 19H4). The most important facto rs and relative humidity. mixing height. tempera- ture, wind speed and d irect ion . Th is pa per aims to study the relationship, which exist between the atmospheric extinction and aero sol mass concentration. temperature and wind speed in the atmo sphere of Qena city in upper Egypt. 2. EX(K' rimelll\ Simultaneous measurements of the extinction coeffi - cient, concentration of the aerosol par ticles and so me meteo rological c ond itions {wind speed and temperature) were carr ied out seven times daily in the atrnosphere of Qena city at the period from March 1988 to Ju ly 1988 and from August 1988 to J anu ary 1989 on the roo fs of the faculties of science (site I) and education (site 2) (about 25 m abo ve the gro und) respectively. Sites of measurements are mark ed on Fig. I. wh ich represents a location map of the study area. Site No. I locates in a desert area and far from the man activities while site No. 2 is urban area and lies in the centre of the city. In general. the atmosphere of the sa mpling area is mostly calm along the year of th e wind s frequency is calm ). The. prevailing wind directions are SW, W and NW With percent age of occurrence equal to 16. 2. 13.5 and 12.9 respectively (Met. Dept., A. R. Egypt 1988). Both the sites nrc located down- wind related to the direction of the prevailing wind' . The extinction coefficient was determined bv measur- inu the transmission los') of radiat ion from a light so'U: oc e caused bv aerosol particles and gaseous consti- tuents of the air"througha 36 111 path with a photocell detector using an optical device constructed by the authors. 1 he device consists mainly of brass metal chamber con nected to a tungsten light SOUrce and a pho tocell detect or. Measurement procedure includes recording of readings of a digital electrometer in nA (36V )

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Page 1: m'l or - Metnetmetnet.imd.gov.in/mausamdocs/54247.pdf · 551.510.42 : 551. 591 : 551.593.4 Atmospheric extinction related to aerosol mass concentration and meteorological conditions

551.510 .42 : 551. 591 : 551.593.4

Atmospheric extinction related t o aerosol massconcent ration and meteorolog ical conditionsin the atmosphere of Qena (Egypt)

SAYEO M. EL·S HA ZLY. AllDELAZEEM M. ABD EL MAG EED.GAM IL Y. HA SSA N and llADRY NO BI

1.1I'mrator.1' 01' Atm ospheric Physics , Dept. of Physics. Qena

( Received 22 ,l ugu.' 1989)

""'._~ ""'" 'IR'O. 'I'I'l'lT'<;fr7 .... " qf" F "'''';Hrqr,,"'n iT for"""iT ""ror" r;,;,,; 'TllI ~ I lrnVT iR "'r<'"q ~Ii it. zfr : %; l:p1 'f.W~;,jPf ;f f~rir,7lJf ir.~ T.T~;r f;1TI'TirCfmll~~<f7T 'T9T 97IT'n 1'J'"lfT ~I~:PTii~ 'Wl~ lfTi":;n, 'Wf11R 3flT'RoT m'l i:r , ;;;<ff~<n'1 'f.T :R1J ~r -m'1r~ ~ I f;r,-"" <r?"f iTf 'I) 'P"l"fT (l'ff. ir~ ) W"fir ~ I • f"f"frT Jfrn<:iu b ~.qt !:f;=i} :r. 'fT'f 'f l; ~)'f qlq;j~;r.r ~t::r n fr.'ir rn r ~ I ., .

AHSTRACT. The depe ndence of the utrnosphcric extinction on aerosols concentration, tempe ratu re antiwind speed is demonstrated . The atmosp heric extinct ion was determined by measu ring the transmission loss ofradiation from u lighl source across36em path with J photcccl! detecto r. Co-clu-ions include a general associa ­lion of high extinction with high aerosols co ncen tration. tem pera tu re and wind speed . but there arc no one-to­one relatio nships . A co rrelat ion study between the extinction coefficient and eac h of these parame ters was per­formed,

Ke)' words c-Air pollutio n. Atmo-phcrlc cxnnct lon . Atmospheric vi"il'lilily. Aenu ol par ticles, Co ncentra tio n.~ r ~ l eonl l og i\,;']1 conditi on...

I. Inuoductlon

The environmental impacts of air pollutant... involveseveral cflccts on the ear t h's atmosphere and on atmo...­pheric proces... ev, One or the I1Hh t important effect,i... the reduction or at mospher ic vi- ihility. Particulateemission of du sts. fumes, fl y ash. and other solid par! i­cles. which b general ly classed a'" acro vol part icles.is the O1O:o,t common pollutant s with potential visibilityimpacts ( Robinson 1984). T he need 10 measure theamount of particulate ail pollutants has. producedan incrca ...ed intere st in a possible relation betweenatmospheric extinction and the mass concent rai ionof particulate matter in the atmosphere. The relation­ship between these two variablev has primarily beenstud ied in other work ' {e.g.. Charl son 196Q. No ll <'I al.1968. Pilat and Ensor 1970. 1971. Pat terson and G illcte1976 and Chylek (' I al. 1979). The results of man y ofthese studies indicate that the exi..tence of an unambi­glIO U'" relation between the extinction and the rnavconcentration is limited. There arc also a number ofmeteorological factors that arc important in the deter­mination of extinction coefficient owing rc theireffect-,on both the concentration of at mosphe ric part iclesand their size (Robinson 19H4). The most importantfactors a nd relat ive hu midity. mixing height. tempera­ture, wind speed and d irect ion .

This pa per aims to study the relationsh ip, whichexist between the atmospheric extinction and aerosolmass concentration. temperature and wind speed inthe atmosph ere of Qena city in upper Egypt .

2. EX(K'rimelll\

Simultaneous measurements of the extinction coeffi­cient, concentration of the aerosol particles and so memeteo rological cond itions {wind speed and temperature)were carr ied out seven ti mes daily in the atrnospher eof Qena city at the period fro m March 1988 to Ju ly1988 and fro m August 1988 to January 1989 on theroofs of the faculties of science (site I) a nd education(site 2) (about 25 m above t he ground) respectively.Sites o f measure ments a re mark ed on Fig. I. wh ichrepresents a locati on ma p of the study area. Site No . Ilocates in a desert area and far from the man activitieswhile site No . 2 is urban area and lies in the centreof the city . In general . the atmosp here of the sa mplingarea is mostly calm alon g the year (50 ~;'; of the wind sfrequency is calm ). The. prevailing wind direct ionsare SW, W and N W With percentage of occu rrenceequal to 16. 2. 13 . 5 and 12 .9 respect ively (Met. Dept.,A. R. Egypt 1988). Both the sites nrc located down­wind related to th e direct ion of the prevail ing wind' .

The extinction coefficient was determined bv measur­inu the transmission los') of radiation from a lightso'U:oce caused bv aerosol particles and gaseous consti ­tuents of the air"through a 36 111 path with a photocelldetector using an optical device constructed by theauthors. 1 he device consists mainly of brass metalchamber connected to a tungsten light SOUrce and aphotocell de tector. Measu rement procedure includesrecordi ng of readi ngs of a d igita l elect rometer in nA

(36V )

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