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conduction can turn into convection

Convection- A type of thermal energy transfer that occurs from the motion of fluid in liquid or gas that is caused by differences in temperature.

-the process of heat moving through a liquid or gas

-heat want to rise and then it cools off then it sinks this is convection

-

hydrosphere is all the water on earth

all the water on earth moves because of the sun

what happens first is when the sun heats up the water it evaporates; evaporation

once it is in the gas stage it goes up in the sky while it gets colder and colder so it wants to condense ;condensation

when there is dust particles in the air they want to condense on the dust particles forming clouds

once the clouds get too heavy the water will fall back to the earth; precipitation

common forms of precipitation are rain snow sleet hail

once it falls back to earth it will start the cycle again

reflected or radiated back out into space, it can get absorbed by thermosphere, or it can reach the ground





evaporate up, condense, and then precipitate

the earths atmosphere is the unique atmosphere in the solar system.

without the atmosphere there would be a lot of UV light



Energy is transferred from the Sun to the Earth through radiation.

Water vapor rising in the atmosphere cools and condenses.

The water cycle affects weather and climate through the transfer of heat and moisture between regions. As water is heated by the sun, it evaporates. The water vapor then condenses and forms clouds in the atmosphere. The moisture eventually returns to Earth as precipitation, sometimes great distances from where it evaporated.

Conduction warms the atmosphere as fast-moving molecules come into contact with lower-energy molecules until all molecules are moving at about the same rate. As the atmosphere warms, molecules move apart. As the heated air flows, heat is transferred by convection from warm, low-pressure air to cooler, high-pressure air.

Water moves between the hydrosphere and atmosphere in a cycle of evaporation and condensation.

     
 
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