“Parcham Classes ke students, aaj hum samjhenge ki...

“Parcham Classes ke students, aaj hum samjhenge ki Bharat mein Monsoon kaise aata hai.” Garmiyon ke dauran Bharat ki zameen, Indian Ocean ke comparison mein kaafi tezi se garam hoti hai. Is wajah se northern aur central India mein low-pressure area develop hota hai. Dusri taraf, Indian Ocean ke upar pressure comparatively high hota hai. Isi pressure difference ki wajah se moisture se bhari hawa samundar se Bharat ki taraf move karti hai. Ye south-west monsoon winds mainly do branches mein divide hoti hain — Arabian Sea Branch aur Bay of Bengal Branch. Jab ye moisture-laden winds Western Ghats jaise mountains se takrati hain, hawa upar uthti hai, thandi hoti hai aur condensation ke baad rainfall hoti hai. Himalayas bhi in monsoon winds ko north ki taraf escape hone se rokne mein important role play karte hain. Toh Parcham Classes ke students, ise ek simple sequence mein yaad rakhiye: Land heat hoti hai → low pressure banta hai → moisture-rich winds India mein enter karti hain → hawa upar uthti hai → condensation hoti hai → aur humein monsoon rainfall milti hai. Isi basic mechanism ki wajah se Bharat mein har saal South-West Monsoon develop hota hai.