Kammala wannan jumla: Hawan yanayi wanda ya haifar da haɗuwa da iska mai zurfi a cikin ƙasa yana kawo girgije da yiwuwar hazo. Ruwan sama na yankin da ke da ƙananan matsin lamba yana aiki don rage bambancin yanayin zafin jiki na rana. Tun da girgije yana nuna hasken rana, hasken rana da ke shigowa ba shi da yawa, wanda ke sa yanayin zafi ya yi sanyi da rana. Da daddare, tasirin girgije akan fitowar radiation mai tsawo, kamar makamashin zafi daga farfajiyar, yana ba da damar yanayin zafi mai zafi a cikin dukkan yanayi. Da ƙarfi yankin ƙananan matsin lamba, da ƙarfi iskar da aka samu a kusa da shi. A duk duniya, tsarin ƙananan matsin lamba galibi ana samun su a kan Tibet Plateau da kuma a cikin dutsen Dutsen Rocky. A cikin Turai - musamman, United Kingdom da Netherlands - tsarin yanayi na ƙananan matsin lamba da ke faruwa sau da yawa ana kiransu matsin lamba. Mafi ƙasƙanci da aka rubuta ba-tornadic barometric matsa lamba shi ne, faruwa a yammacin Pacific a lokacin
Guguwar Tip a ranar 12 ga Oktoba 1979.