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Tabela de nuvens
Grupo de nuvens Altura das nuvens Tipo de nuvem
Nuvens altas = Cirrus 5km / 13 km
Cirrus
Cirrostratus
Cirrocumulus
Nuvens de média altura
= Alto
2km / 7km
Altostratus
Altocumulus
Nuvens baixas = Stratus até 2km;
Stratus
Stratocumulus
Nimbostratus
Nuvens verticais
Cumulus
Cumulonimbus
Nuvens especiais
Mammatus
Lenticularis
Neblina
Rastos de condensação
Nuvens
Uma nuvem é uma grande acumulação de
pequeníssimas gotículas de água ou cristais
de gelo. Estas gotículas são tão pequenas e
leves, que conseguem fl utuar no ar. Todo o
ar contém água, mas próximo do solo ele ap-
resenta-se normalmente na forma de um gás
invisível chamado vapor de água. Quando o
ar quente sobe, ele expande-se e arrefece.
No entanto, o ar frio não consegue conter
tanto vapor de água como o ar quente, razão
pela qual parte do vapor se condensa numa
pequena poeira fl utuante no ar e forma pe-
quenas gotículas.
Quando muitas destas gotículas se juntam,
elas formam uma nuvem visível.
Registar o tempo
Utiliza as páginas que se seguem para regis-
tares os teus resultados.
Completa os teus registos de acordo com a
leitura dos resultados da estação meteoroló-
gica. Se possível, regista as informações to-
dos os dias à mesma hora, para que os teus
registos sejam conclusivos.
Se registares os resultados num determina-
do período de tempo, irás perceber que há
modelos que se repetem. Isto pode ajudar-te
nas previsões do tempo local.
58


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