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Curenţii ascendenţi din interiorul norului antrenează granule de gheaţă aflate în partea superioară a norului.
Grindina este asociată, de cele mai multe ori, cu averse, vânt şi descărcări electrice. Aceasta este provocată de nori cumulo-nimbus.
Sursă: YouTube
În România, grindina apare frecvent în Bărăgan, Dobrogea şi în sudul Moldovei. Grindina este provocată de nori cumulo-nimbus, de dimensiuni mari, care ajung să se dezvolte pe vârticală până la 15-17 kilometri.
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