Iimpawu kunye lobushushu amanzi oLwandle of Azov

Yintoni na ke ubushushu amanzi oLwandle Azov? Kwaye the Black? Waya phi? Mhlawumbi ngoku le mibuzo ayikwazanga zibe semxholweni. Ngoku lixesha lokuba ngeeholide zehlobo kwaye wonke umntu ufuna ubuncinane ngeveki hamba uye elwandle, hlukana umzi, ingxolo rhoqo kunye nomzi.

Ubushushu kwamanzi olwandle Azov. incazelo jikelele

Ukuba lokumba imbali, ungenza ngokukhawuleza bana phandle kumaxesha amandulo abazange akukho Sea Azov, kwaye i-Don River aphuma nje waya kuLwandle Mnyama indawo yamanje Kerch Strait.

Kumaxesha amandulo, amaGrike wayibiza Maeotis chibi, kamva igama amaRoma kwi kumgxobhozo ofanayo.

Nakule yolwandle igama izihlandlo ezininzi: Umva-dengiz, Mayutis, Saksin ulwandle Salakar, Samakush, Chabak-dengiz. Kwaye kuphela kwisiqingatha sesibini senkulungwane 18 egameni umzimba ngamanzi Iqinisekile Azov Sea, owenzeka ekusenokwenzeka igama lendoda efileyo kwi Ugu Prince Azuma (Azufa) Polovtsian.

ulwandle Azov ukuba zihlelwe kweelwandle ngaphakathi emhlabeni kwinxalenye esempuma Europe. Ngokutsho kweengcali, kuphela ukuqonda uhlobo kunye neempawu zayo, ungakwazi ukwenza izigqibo ekunene ngokuphathelele lobushushu yokusithwa ichibi.

Okokuqala, kufanele kuqatshelwe ukuba uLwandle Azov ithathwa ukuba incinane ehlabathini, ubunzulu balo asidluli mitha ezilishumi elinesine,-avareji efanayo, ukusukela zabamakishi meters 6,8-8, kweemitha 7.4.

Ubushushu kwamanzi olwandle Azov. Kunokuba kungenxa?

Ukususela ngokombono izazinzulu, kuba le nto iphawulwa njenge Ukwahluka eliphezulu zexeshana lweendawo iimeko ezisisiseko thermal. Lo msebenzisi kunokucaciswa izinto ezininzi:

• sendawo, ekubeni Sea kubekwe ekunene kwi kumda kweelwandle iintlobo ezimbini: ukuqanda non-qhwa;
• kukha enkulu;
• ugu lungqamane aneleyo;
• ophelelwe eliphantsi.

Kodwa mthombo uphambili ubushushu, nto leyo ngokutyebileyo ukuya phezu kolwandle, nguye lo imisebe yelanga. Ukuba ubalo ngokubanzi, Azov kunyaka 4000 iyakwazi ukufunxa MJ / umzimba amandla m2 yasezulwini. Kule mali, 2200 MJ / m 2 kuyimfuneko ukuphunyezwa komphunga 1500 MJ / m2 sisetyenziselwa radiation olusebenzayo 300 MJ kuphela / m2 lo qha ubushushu wotshintshiselwano kunye nokusingqongileyo.

A indima ebalulekileyo nayo wadlala exchange ngamanzi kunye esasayame Sea Black, kwakunye imilambo-off elibaleka-ngokupheleleyo ezimbini - i-Don kunye Kuban. Nangona impembelelo yabo yahlukile. Umzekelo, i-Kuban noLwandle Black of Azov amanzi ezifudumeleyo, kodwa Don, ngokuchasene noko, kobubi ebalulekileyo.

Hayi kudala, oosonzululwazi baqhuba uhlalutyo ukukhetha kwedatha izikwere ezahlukeneyo echibini. Iziphumo zabonisa ukuba ubushushu yamanzi phezu kolwandle Azov ingachazwa ngaphezulu ngokwemiqathango termostruktury nkqo. Ukusebenza iyizinzise ndazigcina Meyi ukuya kuJulayi, xa amanzi oluqalayo amanzi nzulu ngokuthe ukuzifudumeza, ufikelela ixabiso layo eliphezulu. Okulandelayo kukho inkqubo ezinzileyo of zokupholisa, yaye ekugqibeleni ngo-Oktobha ezithile ngokwezinga aze uba ezingazinzanga.

Iqondo lobushushu kwamanzi kuLwandle Azov kwi onyaka kweshushu

Yenyanga amaxabiso ubushushu namanzi ungcono, xa kuthelekiswa nomyinge, leyo, ngokutsho iingcali, ezo kunokuba izinzile. ubushushu Water kulawulwa ezimbini Azov hydrometeostation ulwandle ilahlwe kwi Berdyansk kunye headlands. izixhobo zale mihla ifakiwe zibonisa ukuba kude olusezantsi kuluhlu wenyanga ukususela 0,7 ukuya 2,2 ° C.

amazinga aphezulu kwenzeka ngo-Apreli nango-Oktobha, okt E. Ngaba. ixesha xa kukho utshintsho ngamaxesha athile kakhulu kwi lobushushu.

Komncinane sinako uqaphele ehlotyeni nasekuqaleni kokwindla. Ngeli xesha, isantya utshintsho yamaxesha kwamaqondo amanzi eziphantsi kakhulu. Le meko efanayo liyasetyenziswa ngoJanuwari noFebruwari, kodwa kuphela Berdyansk, ngokuba Apha cover ice kakhulu ukuzinzisa iqondo lobushushu.

Qaphela ukuba amaxabiso aphezulu ubushushu nezi amanzi 29,3-32,8 ° C. Abaninzi low - ukusuka malunga -2,4 ° C kwi Henichesk ukuya malunga -0,5 ° C eTaganrog.