I-Anticyclone
Kwi-meteorology, i-anticyclones ziindawo zomoya zoxinzelelo oluphezulu kumhlaba onesetyhula okanye i-elliptical shape, ebangela ukuguquguquka okuthobekileyo kwiiparamitha zemeteorological, ngokuchaseneyo nemimandla ye-cyclonic okanye indawo yoxinzelelo oluphantsi : ngaphakathi Bayavuthelakuzo imimoya ibuthathaka, ihlala ibethwa ngumoya., kwaye uvuthele ngasekunene kuMntla weIkhweyitha uze uvuthele ngasekunene kuMazantsi eIkhweyitha.
Umoya, xa unzima, uyacinezela, ufudumale kwaye wome ngakumbi (into ebizwa ngokuba yi -atmospheric subsidence), edla ngokunyibilika amafu. Phambi kwe-anticyclone, nangona kunjalo, inkungu okanye inkungu inokuvela ngexesha lasebusika ngenxa yokuguquguquka kwamaqondo obushushu kufuphi nomhlaba, ngelixa ehlotyeni ukufudumala okunamandla komhlaba kunokubangela ukuvela ngokukhawuleza kwamafu e-cumulonimbus kunye neendudumo zendawo ukuya kuthi ga yokuqina ngamandla