PAKISTAN Annual Rainfall m Over 100 inches 7S /nc/ie s 10/00 Inches ITlIIJ [[IJ] 50 " 75 UTI] ,. 30 SO (( [DJ /0 " 30 It CJJ 5 (, /0 It Below S inches 0.. \.:"'••••..•-.""T"."':""".:- I., -,...,: : '. . \, . r." i. j . •.•••••• '"-4 • t : i' i..." . f'~ • ",,'-;'. . i ('..,.., \ ,.J r"-""" ._ •.........--" •." -'fo . ..' ('_0':> io) .--.. /. .~'-' "-\ , I I I I I I I I , I I : ' I I. I' 1;/;'-- ,r 'J ..J." V ,( I'. , Ii , . , , t... I I ' I I' '-.( , ')' , ' 'i' I I , " : I I I .~,O l:> (If ,uu d ni'\ .~ \ • \') i "'').J ''':' ./"- ..... 30 '-./ ' .....•.. I
There is a great difference in West and East Pakistan not only in <strong>the</strong> annual amounts but also in <strong>the</strong> periodicity <strong>of</strong> rainfall. Over <strong>the</strong> plain <strong>of</strong> West Pakistan and parts <strong>of</strong> <strong>the</strong> neighbouring highlands most <strong>of</strong> <strong>the</strong> rainfall takes place in late summer and has a secondary winter or spring maximum, <strong>the</strong> latter being very useful for <strong>the</strong> unirrigated Rabi crops like Wheat. In many parts <strong>of</strong> <strong>the</strong> montain region, both in <strong>the</strong> north and west, <strong>the</strong> winter and spring rains become more important than <strong>the</strong> summer rains as in Chitral-Swat (Drosh), Baltistan, Gilgit, Quetta-Sarwan. Drosh (Chitral) has more rains in spring than in winter while it is just <strong>the</strong> reverse at Quetta. In East Pakistan <strong>the</strong> rainy season is longer. While like West Pakistan most <strong>of</strong> <strong>the</strong> rainfall takes place in late summer during <strong>the</strong> prevalence <strong>of</strong> <strong>the</strong> summer Monsoons, here <strong>the</strong> pre-Monsoon or early summer months are also quite rainy. Also <strong>the</strong> rainy season is prolonged uptil October and even November. Unlike West Pakistan December and January are generally <strong>the</strong> driest months. Thus taking <strong>the</strong> two wings toge<strong>the</strong>r, <strong>the</strong> rainfall takes place in one part or <strong>the</strong> o<strong>the</strong>r all <strong>the</strong> year round. It takes place in East Pakistan in such amounts that make <strong>the</strong> cultivation <strong>of</strong> wettest crops possible. In West Pakistan, where it is deficient, nature has partly compensated for it by providing big perennial streams in <strong>the</strong> fertile plains. These streams are very nicely spaced where <strong>the</strong> plain is broadest. Even minor plains are not without streams. Winter rains in <strong>the</strong> hills and table-lands <strong>of</strong> West Pakistan introduce an element <strong>of</strong> Mediterranean climate. In East Pakistan <strong>the</strong> erlect <strong>of</strong> high rainfall is fur<strong>the</strong>r intensified by <strong>the</strong> inflow <strong>of</strong> enormous amounts <strong>of</strong> water which forms <strong>the</strong> run-<strong>of</strong>f from <strong>the</strong> neighbouring area. It is fur<strong>the</strong>r streng<strong>the</strong>ned ,by <strong>the</strong> low variability, from 15 to 30%. As compared with it <strong>the</strong> variability <strong>of</strong> rainfall in West Pakistan is 40 to 80%. Humidity. The climate <strong>of</strong> <strong>the</strong> whole <strong>of</strong> East Pakistan may be called humid. Humidity is high practically throughout <strong>the</strong> year. No month has a humidity less than 70% in any part <strong>of</strong> East Pakistan, while during <strong>the</strong> rainy season it is generally over 80%. In West Pakistrn <strong>the</strong> low rainfall, practically cloudless skies and high temperatures considerably reduce <strong>the</strong> humidity <strong>of</strong> <strong>the</strong> country. Only in <strong>the</strong> 8