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Uraren egoerak eta meteorologia

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Uraren egoerak eta meteorologia

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Played 1 %Accuracy 91 Average time 18:27
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About this activity

Hodeiak eta ur-lurrunaren zikloaren oinarrizko kontzeptuak

Created by

Antxelenia
Antxelenia
Spain

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Uraren egoerak eta meteorologiaOnline version

Hodeiak eta ur-lurrunaren zikloaren oinarrizko kontzeptuak

by Antxelenia
1

: Airean pilatzen da landare eta gainerako izaki bizidunetatik , eta itsaso , eta lakuen lurrunketatik datorren - . Ur - lurruna egiten da , tenperatura eremuetara iritsi arte . Orduan , eta hodeiak sorrarazten ditu , oso ur tanta txikiz edo eratuak .


: Atmosfera oso dagoenean eta behera egiten duenean , hodeiak sorrarazten dituzten ur tanta horiek eta erortzen dira .

2

: Lurzorutik hurbil sortutako oso osatzen da . Ohikoa da ibai edo hurbil egotea , adierazgarria baita leku horietan .

: Atmosferan handirik ez badago , euririk egin jaitsi daiteke . jaisten bada , lainoetako ura egiten da , eta - txikiak erortzen dira ; izotz - kristal horiek multzokatu egin daitezke , - eratuz .

3

: Hezetasuna denean eta 0 ? - tik beherakoa denean , uraren gainazala eta - geruzak sor daitezke .

: Izoztutako ur tantak , goranzko bultzatuta , berriro barneratzen direnean eratzen da . Hor beste partikula batzuetara batzen dira , eta sortzen da .

4

: , zerua dagoenean eta lurzoruko 0 C - ra iristen denean , giroko hezetasuna egiten da gainazal , ur tantak eratuz .

: Ihintzaren ordez sortzen da , giroko kondentsatu eta solidoetan denean , adibidez ; landareetako .

5

zuria : altuera daudenean ikusten da . erretzean , askatzen dira , eta horietako bat - da . Altuera garaietan , - 50 ? - koa da . Hor lurruna berehala da , eta hegazkinaren arrasto hori sortzen da .

: Izaki guztiek - askatzen dute gasekin . Lurruna azkar bada , egiten da , eta moduko bat eratzen da .

 
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