Kuyadabukisa kakhulu ukubona ukuthi, emizuzwini engemingaki, ukuthi yini ethathe iminyaka, imvamisa amakhulu eminyaka, ukuthi ikhule ibe ngumlotha. Umlilo wehlathi uyingxenye yezindawo ezithile zemvelo. Eqinisweni, kunezitshalo eziningi ezingahluma kuphela ngemuva komcimbi onjengalona, njengalezo zohlobo lweProtea ezihlala e-Afrika. Kodwa-ke, isikhathi esiningi zibangelwa ngabantu, futhi manje nokuguquka kwesimo sezulu.
Ikusasa lamahlathi livela "elimnyama", futhi akukaze kushiwo okungcono: ukuncipha kwemvula nokuqiniswa kwesomiso kuzodala ukuthi izitshalo zinciphe ngokushesha, okwathi ngesikhathi isikhathi se-canicular imililo kuzoba ngabaphikisi besikhathi sethu sanamuhla.
Imililo ingeyezilwane (kufaka phakathi abantu), inkinga enkulu kakhulu. Usongo abangafuni ukuba nalo. Umlilo uqothula konke okusendleleni yawo, uqothula indawo yokuhlala yamakhulu ezinhlobo zezinto eziphilayo futhi ubeka impilo yabantu engcupheni esendaweni. Naphezu kwakho konke, namuhla, sisekude ukuthi isibalo semililo sinciphe.
Izinga lokushisa lomhlaba liyakhula. Izinto eziphilayo kufanele zivumelane nezimo, kepha ngeke zikwenze ngokushesha. Ukuzivumelanisa nezimo kungathatha izinyanga ngisho neminyaka, futhi leso yisikhathi okungenzeka ukuthi abanaso.
Ngakho-ke, usosayensi uJosé Antonio Vega Hidalgo, oxhunyaniswe neSpain Society of Environmental Sciences kanye neForest Research Center yaseLourizán, kusho lokho kuyadingeka ukubheja kwezemfundo, ukuqapha okwandisiwe futhi ikakhulukazi ukwenqatshwa kwezenhlalo njengethuluzi eliyisisekelo lokwenza. Ngokunjalo, wengeze nokuthi isimo sezitshalo ezivuthayo kufanele sithuthukiswe ngenhlanganisela yezinhlobo zezihlahla kanye nemikhawulo yezinhlobo ze-pyrophilic, ukwehlukaniswa kokusetshenziswa kwehlathi kanye nokutshalwa kwemali okukhulu ocwaningweni.
Mhlawumbe yileyo ndlela amahlathi angasindiswa ngayo.