what are 5 examples of convection?
11992
['Breeze. The formation of sea and land breeze form the classic examples of convection. ... ', 'Boiling Water. Convection comes into play while boiling water. ... ', 'Blood Circulation in Warm-Blooded Mammals. ... ', 'Air-Conditioner. ... ', 'Radiator. ... ', 'Refrigerator. ... ', 'Hot Air Popper. ... ', 'Hot Air Balloon.']
989867
['Coronal hole.', 'Coronal mass ejection.', 'Geomagnetic storm.', 'Solar flare.', 'Solar particle event.', 'Solar prominence.', 'Sunspot.', 'Space Weather.']
289435
['Cold Front. A cold front is the leading edge of a colder air mass. ... ', 'Warm Front. Warm fronts tend to move slower than cold fronts and are the leading edge of warm air moving northward. ... ', 'Stationary Front. ... ', 'Occluded Front.']
118182
The movement of heat from a warmer object to a cooler one is called heat transfer. There are three methods of heat transfer: conduction, convection, and radiation. Conduction is the movement of heat energy through a substance or from one substance to another by direct contact of atoms and molecules.
1013250
The movement of particles of matter results in thermal energy. This energy is then transferred to other substances in three ways, conduction, convection, and radiation. In conduction, thermal energy is transferred through direct contact. ... Convection is the transfer of heat by the actual movement of the warmed matter.
205113
Forced convection - This is where a fan, pump or suction device is used to facilitate convection.
1035980
Thermal energy is transferred from hot places to cold places by convection. Convection occurs when warmer areas of a liquid or gas rise to cooler areas in the liquid or gas. Cooler liquid or gas then takes the place of the warmer areas which have risen higher. This results in a continous circulation pattern.
1177118
There are three methods of thermal energy transfer: conduction, convection, and radiation. Conduction transfers thermal energy through direct contact.
13047
Mantle convection is the very slow creeping motion of Earth's solid silicate mantle caused by convection currents carrying heat from the interior to the planet's surface. The Earth's surface lithosphere rides atop the asthenosphere and the two form the components of the upper mantle.
1311877
['Seismonastic Movement: This type of movement is caused by the mechanical stimuli like shock, touch or contact, fast moving wind, rain drops, etc. ... ', 'Photonasty Movement: ... ', 'Thermonastic movement: ... ', 'Nyctinastic movement: ... ', 'Thigmonasty movement:']
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Convection currents drive the movement of Earth's rigid tectonic plates in the planet's fluid molten mantle. In places where convection currents rise up towards the crust's surface, tectonic plates move away from each other in a process known as seafloor spreading (Fig.
274406
['Moisture,', 'Instability, and.', 'a lifting mechanism.']
962937
['Frost Wedging or Freeze-Thaw. ••• Water expands by 9 percent when it freezes into ice. ... ', 'Crystal Formation or Salt Wedging. ••• Crystal formation cracks rock in a similar way. ... ', 'Unloading and Exfoliation. ••• ... ', 'Thermal Expansion and Contraction. ••• ... ', 'Rock Abrasion. ••• ... ', 'Gravitational Impact. •••']
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['Displacement of Water.', 'Upwards Delivery.', 'Downwards Delivery.']
736491
And unless people interfere, thermal energy — or heat — naturally flows in one direction only: from hot toward cold. Heat moves naturally by any of three means. The processes are known as conduction, convection and radiation. Sometimes more than one may occur at the same time.
363133
['lithosphere.', 'asthenosphere.', 'mesosphere.', 'outer core.', 'inner core.']
1358057
['Conduction: Heat is thermal energy, and in solids it can be transferred by conduction. ... ', 'Convection: Fluids, that is both gases and liquids, can transfer heat energy by convection. ... ', 'Radiation:']