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BORIShOTi atmosferi

boronBORIShOTi atmosferi, obest dar holati moe yo sakht, ki az abr meborad (boron, barf, jola) yo bevosita dar sathi zaminu ashyoi ruyi on ba tufayli kondensatsiyai bukhori obi tarkibi havo paydo meshavad (yakhcha, kirav, shabnam). Borishotro bo asbobhoi makhsusi borishsanj bo mm chen mekunand. Miqdori Borishot vobasta ba arzi jugrofiyoi, masofa az uqyonus, samti bod va relyefi mahal dar mavzehoi gunoguni kurai Zamin gunogun meshavad.

Dar Tojikiston miqdori Borishoti solona 456 mm (dar Du­shanbe – 644 mm, Khujand – 178, Kurgonteppa – 271, Khorug – 291 mm) ast. Qatorkuhhoi Hisor peshi jarayoni nami havoro megirand. Dar natija miqdori solonai Borishot dar in vodi az 2000 mm ziyod meshavad. Dar janubi Tojikiston va Po­miri Sharqi miqdori solonai Borishot kam (82-160 mm), dar havzai Qarokul va nohiyai Murgob az in ham kamtar (70- 73 mm) ast. In mintaqaho nohiyahoi kamborishi jumhuri mahsub megardand. Dar vodiho Borishot mohhoi mart – aprel, dar kuhiston mohhoi zimiston va bahor mushohida mesha­vad. Dar nohiyahoi balandkuh ba vujud omadani namrezavu yakhcha ba hodisahoi iqlimi Tojikiston khos ast. Ba gayr az ob dar tarkibi Borishot zarrahoi chang, mikroorganizmho, unsurhoi kimiyoi niz vomekhurand.

Adabiyot: Khrgian A. X. Fizika atmosferi. Leningrad, 1969.

A. Homidov.

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