Monsoons eIndiya

Namhlanje siza kuthetha ngesihloko esibaluleke kakhulu ekufuneka sazi ngaphambili hamba uye eIndiya, i iimvula. Ngokombono wejografi, iimvula zivela ngenxa yokuba kwilizwekazi amaqondo obushushu ayafudumala okanye apholise ngokukhawuleza kunakwilwandlekazi, ke ngoko, xa amazwe aseIndiya eqala ukufudumeza ubushushu ehlotyeni kwaye kwangaxeshanye inyambalala yabantu Umoya ovela kuLwandlekazi lwaseIndiya uqala ukufikelela usingasiqithi wamaHindu, intlekele iqala.

imvula

Ngeli xesha uza kuqala ukubhalisa utshintsho olukhulu kakhulu malunga namaqondo obushushu kunye nemvula, ebangela imvula eyintlekele kunye nemeko efumileyo yamaqondo obushushu ashushu kakhulu. Ngaphandle koku, iimonons ezenzeka eIndiya zinokuba nemozulu eyomileyo, isixa esikhulu semimoya enomoya omtsha nokomileyo (nangona iyingozi nje)

imvula2

Ukuhamba kweemonons kwimimandla yaseIndiya ngolu hlobo lulandelayo, icandelo lokuqala elichaphazelekayo liya kuhlala lilunxweme olusentshona lwecala elisemazantsi, apha ukunyaniseka akukabi namandla kangako, emva koko imozulu yangoku iya ngaselunxwemeni lwelizwe. ., iBay of Bengal, emva koko udlulele kwiiHimalaya ezintle, kwicala elingasentla laseIndiya.

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Ukudibana kwemonsoon kunye neeHimalaya kubangela ukuba eyangaphambili itshintshe indlela eya ngasentshona kwaye iqhubeke nohambo lwayo kumantla nakumbindi weIndiya. Kufuneka kuqatshelwe ukuba kweli candelo lokugqibela kukho iimvula ezinobundlobongela kunye nokwanda kokuhamba kweengxangxasi zaseBangladesh, eRajasthan nakwimimandla ekufuphi.


Umxholo wenqaku uyabambelela kwimigaqo yethu imigaqo yokuziphatha yokuhlela. Ukuxela impazamo cofa apha.

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