RAINFALL

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Hello my great steemians

I am delighted to share with you all my idea on this topic titled rainfall,but first of all what is rainfall.

Rainfall is defined as the release of excess water in the atmosphere into the earth.

FORMS IF PRECIPITATION

• Snow
• Hail
• See
• Fog
• Frast
• most

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• SNOW: snow is formed when water vapour condensed in the atmosphere at temperature below freezing point resulting in the formed of nice crystal.
• Hail: This is formed from condensed water droplets at greats vertical night and usually associated with thunderstorms ice crystals are also formed.
• DEW: See is formed when condensation takes place in the temperature if which condensation occurs is known as dew point.
• FOG: This is also formed when condensation takes place when the ground or over the sea resulting in tiny particles of dirt and dust in the air.
• Frast: This is formed as a result of the direct condensation of water droplets into crystals when the temperature is below freasy point.
• MIST: Mist is just like fog is formed when condensation takes place near the ground when of occurs as tiny water droplets that are mist think as fog.

TYPES OF RAINFALL
CONVECTION RAINFALL
OROGRAPHIC RAINFALL
CRYCLONIC RAINFALL

• CONVECTION RAINFALL: formation convection rainfall occurs in the area intensively healed. Hot warm air humidity takes places. The rising air become saturates and water vapour condenses with cloud being formed quickly this result in the healing rains. Accompanied by thunder and lighting.
  CHARACTERISTICS OF CONVECTION RAINFALL

• It is short liked and characteristics heavy winds lighting and thunder.

• Rainfall within limited area usually in the afternoon.

• The sky become clear immediately after the rain.

• Hail stones may occur.
  The cloud is associated with thunderstorms and convectional rainfall is called camclonim busi.

• OROGRAPHIC OR RELIEF RAINFALL
  orograpic rainfall moist air is ferced to rise above a mountain or barrier, usually on the wind ward slopes of mountain. Rising air expands and become cooler and relative humidity rises and air becomes saturated.
  CHARACTERISTICS OF OROGRAPIC RAINFALL

• It also characterized by ascending and descending wind.

• Wind ward area has rainfall.
  This rainfall only form or take place on the wind ward side of a mountain

In conclusion I hope I have been able to talk about rainfall.

Special mentioning
@bessie2023
@goodybest
@okere-blessing

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