Wind indlela. Ukuchongwa esweni

Ukumisela kwicala umoya namandla - ingxaki standard nakunyuka meteorology. Ezi zicwangciso luchaphazele amaqondo obushushu, waqonda kunye nemozulu ngokwawo - ngenxa yokuba imimoya aqhubeke khona umoya omkhulu. Ukusuka ehamba imozulu amaninzi ukuva ukuba ethile kukho iinkanyamba ezinkulu okanye anticyclones ukusuka kwi Arctic okanye, umzekelo, kwicala Atlantic. Wind - na intshukumo khona umoya emoyeni asezantsi ukusuka kwiindawo eziphakamileyo kwingcinezelo phantsi, ukuze amandla umahluko yokusebenza va xi endle enxulumene ixhomekeke ngamandla omoya. Yiloo nto iinkanyamba kunye zizaqhwithi abafane kwenzeka ngaphakathi kweli lizwekazi. Kodwa kufuphi nolwandle coast okanye ulwandle - kakhulu rhoqo. Zolani, oko kukuthi uzolile, kuba apho kulapho kukho uxinzelelo kwiindawo ezikufutshane ezifanayo. Kodwa le meko akuxhaphakanga kakhulu.

Ukumisela ulwalathiso umoya ezikhoyo, ingakumbi bakhe zemimoya isantya namandla, kubaluleke kakhulu ukuba abalathisi benqwelo-moya. Xa umoya onamandla umqhubi kuya kufuneka benze oku ukulungiswa, kwaye ukuba umoya onamandla kakhulu, usenokuba ukurhoxisa okanye elinye i moya. Oku kuyafana ngeenqanawa. Kwanaphezu amandla enqanaweni kunye ngakulo umoya zibalulekile. Yiloo nto bezulu irekhodi isantya somoya kunye nolwalathiso ngoncedo izixhobo ezikhethekileyo, uze emva koko nokuba wenze ishedyuli eyodwa, ikhampasi wavuka, obonisa ulwalathiso umoya nakolu kwindawo ethile. Ngokuqhelekileyo, Roza Vetrov nguye ekupheleni konyaka okanye ithuba nangaphezulu. Umzekelo, i okhoyo oya ngakulo umoya eMoscow kwiminyaka yakutshanje - emazantsi-ntshona. Oko kukuthi, ixesha elininzi oko ukuvuthela emazantsi okanye ngowasentshonalanga.

Ngendlela, xa sithetha kwicala umoya, ukwalathelwa iindawo zehlabathi kubaluleke ngokukhethekileyo. Ukuba umoya kuthiwa ngasezantsi, ngoko uvuthuza ukusuka ezantsi. Ngoko ke, kwavela ukudideka xa abantu babone kwicala iintolo ukusuka ekhohlo ukuya ekunene kwaye bakholelwa ukuba umoya wasempumalanga. Akukho imposiso! Kwimeko yokufumanisa iintolo umoya usoloko abonisa indlela apho umoya uvuthuza, kodwa hayi kakhulu. Kutheni le nto kunjalo, kuba kunzima ukutsho, iye yaphuhliswa njalo.

Ngoko ke musa ukuba indlela ophulaphula ngayo ulwalathiso ngumoya? Easy! Uluntu owasungula izixhobo ezininzi ukuvumela ukwenza ngokukhawuleza: i anemometer ezisetyenziswa kwiinqanawa, vane, nto leyo inceda ukuqinisekisa ulwalathiso ngamandla umoya, nkqu kubomi bemihla ngemihla, ngokunjalo nemiqondiso ngokukhethekileyo umoya, apho kusoloko kubonakala kwizikhululo zeenqwelo-moya: baba ngokohlobo elide orange-emhlophe ukufana abaphula umthetho.

Amandla omoya, lidla uzimisele kunye nolwalathiso yayo, ngokufuthi zibonakaliswe apha amanqaku okanye iimitha ngomzuzwana ngamnye. Ngamanye amaxesha, xa amanani ngqo awabalulekanga, ibinzana elithi "ngcathu", "ubuthathaka" njalo-njalo.

Ukongeza, kukho imimoya onyaka, ngokunjalo nabo baxhomekeke ulwalathiso ixesha losuku - ngokuqhelekileyo kwaphawulwa kunxweme yolwandle okanye namanye amaqumrhu omkhulu wamanzi. Oku malunga yimpepho kunye nemvula. Aba nempembelelo enkulu kwimozulu kunye nemozulu kwizixeko nakwiidolophu akhiwe kuphela kufutshane imizimba omkhulu wamanzi, kodwa ngaphakathi kweli lizwekazi.

Ngenxa yoko, indlela umoya nangamandla - ezi zezinye isitshixo zemozulu kunye nemozulu parameters, kunye lobushushu, uxinzelelo kunye kwezulu.