Question

hiw does the annual distribution of precipitation vary between the two cities

Answer 1

Aual austnbutHo Preuputao va betun two Hlon may dspend om Jarjousaton Suin as weath Coudithous ueoapuio Couditon Tyfe jgetaton cumatic Couditous Sralug tot Area Satunotiar oj 4l lnd o duwoit eguetoria Bet oj Let loulspuore Stuadiou tuat Ars Cylouas aud autyloes Lwlotuar Couditious, Tu cevent Ctta, j dut Louutru, uar SatuatHon u wich e Preuptatou Lagfa Maoinaraun or an erampla T etatft dia Subuoutiuant. In Masiuasan" te NoAuuonolo Ahr rom Bay Begaj onsoon, haue t Caver uide Ar& by But fuis arad to suesge narvro Zone last JiU, Sa -tue' clyppaut dapend audl wolotue igut Concewdra He wet Couolito ane tuae

So, uly coudittous أممملما ,مفقيا ,J4ه to ay aijau t Area wwrle T Jorpun layoatton e desat lan Preuputotou aLutuere lhe Laad to Sttuaton aud duougt duke in tu Avea Stuatious So, the Preuptatio, betwes depndr pn Sour uore 'teuluaical terru felote to two Ctta tuatr Ceagrp uiol toualutio dead to Preiptation Clven Relows

lajorpli the ocane aralation ard dislribpn walor m ydnabij car face ond is omophene onolen, havig diffenent residence time in coch phan Resicence Hme: Thu ii the aunage tme lken ky a Lafen pantide An aing one perhiclon phaxe the hydalgicye Nole The nd phase cloes not UAcntially mean Aplid qid gas phate) Nfoh volume Residence time V Qeag oig Shehange Runth ocean Lond PPE Evatorahion> Raifall (Preaipitat") Precipiteaom evaporastion Note: ove the cean Awface evaporction igreater than freciblkation. -. (apbroxi matdy g .). where as on He andmats preipikaHom reater than evaporaHon Mydro logtcal cycle must Coristain land Catchment aneai- dride tsatergivride grde -aldhmentoreo {waler.Ahed) Ara into Hver or gheam i called the atchment aned hat Atream ai a penhicudar lbation. Tti auo cailed at 19alh shed

Precibitation Preupilation denots all the liffenent ways or procees by which mjstune reache the carth's face following ane Phe difforent typea f prepitahon Rain I the most cominenft form peceipitotion in India.and it olenote walen draplets which Aize varyizg from0S om On the tnAis d inknsity rainfall ii Uauified a to follorss: Ca Light rainfal b) Medium/Maderoakrainfa 5mm/h heawynfa mmh 0-25 mmhr gndio deperdi on orographic Pain fall Convechive Poinpl fromtat Rain fall gelowi Rainfols -haraleyan Conypane to mumba Alener berala S.u Nave Leeuond joinfa

yckme ign rame Nothenn Hamitphene they ane Audiea yclome drection Anti ycbne clirechon Sauthern Hemi^phene 26 S.H Nole: In Idio rainfali dlola hau ouestol euoy doy at 30 a and ainfau on a penhiculan dlay i more thoan 5mm Ha day i Called ai rainy dlay. 9 cm 120 um Average annual Rainfai in 9ndia Area India 3.3 MEm2 or (projecked aneg/ pbn anea) Rain anter hanvestiog : 330Mha (3.98M u6. Punff total volume Note: Moa dominent mechanism reinfal in India ainfall (i) Arizzle:- Bihan lood-Man made due to forakkka baroy Tt denofe fine dbufHetn 4 walch whoae he euno5mm and anlensty leu Han Imm/hr vdloaty ogog Sitahont, velum Capocihyd goyol (Si )Srae;- Thete are ice tynal haing density ol gmfee watn level for ome (M) Ghze:- bhen dnopleta cf water Comcs in Contact wilth cdd gand Awface ,then Hate uComvertd ibo ice ,kich Ged a glaze (Sleet Thee are foe eindnapa banspanent natwie vi) Hai Thee ahe lump e ohepe le greate on 6m Nofe: As per ^ntenrational Con venhion (MO) Aumpi te gre Han 5mm alied a haond lumb Amalos Hhon san are Called aGa Grawpet IM. India mehologica 'elepantment (office Delhi

availabliy mskune following dnugkt ahe he diffenent tybes deficiency in pre cihitation. 1f defiolency iu mort ii CaUed au dought. than 1 If deficieny is betseen 25- 50% alled a modenal da and 5oy Coled Aeere draght A porticlar year jcalled coygtt yean e affekad hy drougl u mre than 20% the total area of the Counhy" If Broght occuru in on areo with a probabiuty betxen 02 too4 then that area i Called as drougt pme aneg. IF the probabi uty greate than o.4 Hhen Hhe anea i oUed Coically droug prome anea. Abod 33 Note Tndio's ares omeu under Hhe Calegomy either deught ame Croni cally droglt prone anea i)Hyenological dsoug Thiu tybe 9 drought denates beloo cunrage alue Aheam Ho, otur Content i, lakes rucr Coir urdenground water ek. ciAriceltral drught : isalen Ashch red formecting the evapotranspirahion nee for theCrop I Called a Aridity inde denotd b a four PET AGT ET Cropbed aren x loo irdex PET PE1- poteni eabohanspirahon AfT Actual evapotahspiration - auailable actualy achual need for full groat fpn .that plant numi

prm Lemes from precipitation: Tn hycnetloy un Concern alo Called os outpuf a catchment) where a atu other Procene Coneunden the Calegory owes. to Alate at the fee Aurface 4 Liauid. evoporation i hasicaly oung procea in which Raten heat o vaborisahion must be povide by Hhe aten bady Latent heat voporisahion d wat.n ; 585 Callgm Vapou Apeci al tybe f gas which can be easily Converted into lquid b decreacing the kempenatune. Factors affectine evaboration: ) vabo prewre: Rate q evaportion iu dirtetly proporhional fo t dffenence behocen Aahurated uabour preuune and vatoow þresuure c air () Temperat une fak d eveforation a dietly proportonmal io prtvo.by toeoταίτε (i Sind peed: Rale vabotAation inctae sith faster puindi 1f the LSind veloufy i vey hist and ii Aufficient to emove av uapou abov he Onid unface .hen any furthen inoreae evaporaton More the e- hore humid Wind vele

Almophovie premune: evaforation rafe ir jinvey properhod fo the atmaspheric premwre V Saluble alt:. If palta ane preuent in ater j vapour Preune decrea plch in torm rsults in reduction in the ral evaperalion, A duth ecporahion from dea water ju abu -3 less au Compane to fresh water Suy( parlpen fhousond (PDE) , ag talinity i about as ppt (vi Debth nton bedy: In jummer Ahauos depth d wat permit Fabidintreaen kmberature dwi7 he day t ond hence euaporaHon u ałon n o shallow aten body Tn winfo lomperatwre dswvrourdig ar fealls bus Phe kmbeahue deep Rake docunt fall easily and thuy Jatcr rerrains Helahvdy wumer, Gnsequenty in Lsinter evaporaticn i more a deep tnles hady bave phenomenon i primahily due to heat Akrge 4 ator (viiSunface anea: eaoraion directty proportiomal the Aunface area. ConAeh vation 4 resenyeir wr PolH B 2 О- RES: Reseuoir induced Aeijmidty follawirg ethadi roy b ed in rden to Contenve the ruouor alr cl ouidingreaton deph to ater body i Aunfae aro i redu«d uhich in oum deduce the poraHon 'c) By braidng mechanicad Covor in he form ro Ahed c th pEthod Can be ted orly ferAmall salon body Auch a toke or L oond

f Cer tain rermi (ols pach os' hezn decones ( and oclo decanek (ig CH) (han oleaf) an be effecintiy inas and non topic film i fid on sohon pwtar obid parnian fre Crcdahem and arbm di-oude, (in oden to poosorut he aquati Lik). Arrp ods jhe cericada Cy fod e be the moA effedive one ord by ing evoont duced by abut 40-67. Modnum edution in euckrotion presczas d esrd. efciencythue chemicals is odser ofe .() By inrea alinity d en shorekion rou tonte edsons Meaurementd evaboration: fodlasirg rerods a be n Crder to fd he value deferation. ( Clam A eEvabaraion Pan Thi j o dardod Pr hat has ben developed U.S. eother Bnur, ord haso i Fdaneknd121o mm ord dh 955mm. The oni. normally made unpaied Gt. t. In ora $en orves lon is a problern monal mekad ii uxd (allay 4 r Gbo} ( TS. Eatorotion fan: Thi i the rodified fom 4 dass a eszperaken ban in ohich damekn i i220mn ord depi s 355 mn Thi pon iu mode ipen Ahaed bouinga cnn og Tep dthe ban i futiy end sih a taogoras 1Sirt retting in orden to prket he ater frorn any Canfom kempietne inamd dina doy ond ngtt time i) Colorado Sunto fant Main osvan ge tis bybe of disturkance ard to enwe hat indu Erding sin-Sau rardend sa Pan iu thal it rk iian rodiation ord anarari fest