m'l or - Metnetmetnet.imd.gov.in/mausamdocs/54247.pdf · 551.510.42 : 551. 591 : 551.593.4...

Preview:

Citation preview

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 )

Recommended