Convection - Revision history

Jmdonev: 1 revision imported

2021-10-15T19:13:32Z

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energy>Jmdonev at 21:52, 18 May 2021

2021-05-18T21:52:37Z

← Older revision		Revision as of 21:52, 18 May 2021
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	[[Category:Done ~~2016~~-04-30]]		[[Category:Done 2021-01-31]]
	<onlyinclude>'''Convection''' is ~~the motion~~ of a [[fluid]] driven by [[temperature]] differences across that fluid. When a fluid is [[heat]]ed, the region in closest contact with the heat source becomes less [[density\|dense]] due to increased [[kinetic energy]] in the particles</onlyinclude>. The portion of fluid that is less dense then rises, while the denser portion of fluid sinks. The process repeats itself because the less dense fluids cool down as they move away from their heat source, making them sink, while the denser fluids heat up as they near the heat source, making them rise. This creates convection currents.		<onlyinclude>'''Convection''' is a way for [[heat]] to move, also referred to as a [[Heat transfer mechanisms\|heat transfer mechanism]]. This transfer of [[heat]] happens when a [[fluid]] such as air or water is in motion. <onlyinclude> Convection is driven by [[temperature]] differences across that fluid. When a fluid is [[heat]]ed, the region in closest contact with the heat source becomes less [[density\|dense]] due to increased [[kinetic energy]] in the particles</onlyinclude>. The portion of fluid that is less dense then rises, while the denser portion of fluid sinks. The process repeats itself because the less dense fluids cool down as they move away from their heat source, making them sink, while the denser fluids heat up as they near the heat source, making them rise. This creates convection currents.

			<gallery caption="Natural Convection" mode=packed heights=200px>
			File:Convection cell atmos labeled.gif\|thumb\|none\|Figure 1. Air over land heats faster than air over water, leading to convection which feels like a cool ocean breeze.<ref name=Book1>”Properties of Matter Reading Selection: Density Creates Currents.” [Online]. Available: http://www.propertiesofmatter.si.edu/Density_Creates.html</ref>
			File: Convection cell room labeled.gif\|thumb\|none\|Figure 2. Convection warming a room is quiet and energy efficient.<ref name=Book1/>
			</gallery>

	Convection is one of the fundamental ways that heat is [[Heat transfer mechanisms\|transferred]]. The others are [[thermal conduction]],<ref name=Knight>R. D. Knight, "Work," in ''Physics for Scientists and Engineers: A Strategic Approach,'' 2nd ed. San Francisco: Pearson Addison-Wesley, 2008, ch. 11, pp. 325–327</ref> [[radiant energy]]<ref name=Knight/> and [[evapotranspiration]].<ref>R. Wolfson, "High-Energy Society," in ''Energy, Environment and Climate,'' 2nd ed. New York: Norton, 2012, ch. 12, pp. 333</ref>

	[[File:Convection cell atmos labeled.gif\|thumb\|350px\|left\|Figure 1. Air over land heats faster than air over water, leading to convection which feels like a cool ocean breeze.<ref name=Book1>”Properties of Matter Reading Selection: Density Creates Currents.” [Online]. Available: http://www.propertiesofmatter.si.edu/Density_Creates.html</ref>]]
	~~[[File: Convection cell room labeled.gif\|thumb\|375px\|right\|Figure 2. Convection warming a room is quiet and energy efficient.<ref name=Book1/>]]~~
	~~<br/><br/><br/><br/><br/><br/><br/><br/><br/><br/><br/><br/><br/>~~
	Convection plays a large role in wind patterns and in passive ventilation. The movement of wind across the globe is dependent on various spots where warm air rises and cool air sinks, creating large wind currents that affect weather. For example, air over land will typically get heated up by the sun during the day, while air over the sea will remain cool. The hot air over land will rise in the atmosphere. As it rises, it also cools down and becomes denser, causing it to sink once more. This concept is illustrated in Figure 1.<br />		Convection plays a large role in wind patterns and in passive ventilation. The movement of wind across the globe is dependent on various spots where warm air rises and cool air sinks, creating large wind currents that affect weather. For example, air over land will typically get heated up by the sun during the day, while air over the sea will remain cool. The hot air over land will rise in the atmosphere. As it rises, it also cools down and becomes denser, causing it to sink once more. This concept is illustrated in Figure 1.<br />

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	While natural convection can be used inside houses, [[forced convection]] is more common. This is where air currents are forced through a room by a fan. Forced convection can achieve the same effects as natural convection, the process is simply aided through devices like fans. If your house has heating vents on the bottom of your walls, this is an example of forced convection.		While natural convection can be used inside houses, [[forced convection]] is more common. This is where air currents are forced through a room by a fan. Forced convection can achieve the same effects as natural convection, the process is simply aided through devices like fans. If your house has heating vents on the bottom of your walls, this is an example of forced convection.

	[[File:winter.png\|~~400px~~\|~~framed\|right~~\|Figure 4. In the winter, ceiling fans should rotate clockwise to pull cool air up from the room and force warm air downwards, creating an updraft.<ref name=pic>''Created internally by a member of the Energy Education team''</ref>]]		<gallery caption="Ceiling fans" mode=packed heights=250px>
	[[~~File:summer~~.~~png\|400px\|framed\|left\|Figure 3~~. ~~In the summer~~, ~~ceiling fans should rotate counterclockwise to mix warm air~~ and ~~force a cool breeze downwards~~, ~~creating a downdraft~~.<ref name=~~pic~~/> ]]		File:summer.png\|thumb\|none\|Figure 3. In the summer, ceiling fans should rotate counterclockwise to mix warm air and force a cool breeze downwards, creating a downdraft.<ref name=pic/>
	<~~br/~~><~~br/><br/><br/><br/><br/><br~~/>		File:winter.png\|thumb\|none\|Figure 4. In the winter, ceiling fans should rotate clockwise to pull cool air up from the room and force warm air downwards, creating an updraft.<ref name=pic>''Created internally by a member of the Energy Education team''</ref>
	~~<br/><br/><br/><br/><br/><br/><br/>~~		</gallery>


			Convection is one of the fundamental ways that heat is [[Heat transfer mechanisms\|transferred]]. The others are [[thermal conduction]],<ref name=Knight>R. D. Knight, "Work," in ''Physics for Scientists and Engineers: A Strategic Approach,'' 2nd ed. San Francisco: Pearson Addison-Wesley, 2008, ch. 11, pp. 325–327</ref> [[radiant energy]]<ref name=Knight/> and [[evapotranspiration]].<ref>R. Wolfson, "High-Energy Society," in ''Energy, Environment and Climate,'' 2nd ed. New York: Norton, 2012, ch. 12, pp. 333</ref>

			==Further Reading==
			*[[Fluid]]
			*[[Heat]]
			*[[Temperature]]
			*[[Heat transfer mechanisms]]
			*Or explore a [[Special:Random\|random page]]

	==References==		==References==
	{{reflist}}		{{reflist}}
	[[Category:Uploaded]]		[[Category:Uploaded]]

Jmdonev: 1 revision imported: From the summer

2016-09-17T22:29:37Z

1 revision imported: From the summer

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Jmdonev at 22:30, 1 August 2016

2016-08-01T22:30:13Z

← Older revision		Revision as of 22:30, 1 August 2016
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	[[~~category~~:~~done 2014~~-08-16]]		[[Category:Done 2016-04-30]]
	<onlyinclude>Convection is the motion of a fluid driven by temperature differences across that fluid. When a fluid is ~~heated~~, the region in closest contact with the heat source becomes less dense due to increased [[kinetic energy]] in the particles</onlyinclude>. The portion of fluid that is less dense then rises, while the denser portion of fluid sinks. The process repeats itself because the less dense fluids cool down as they move away from their heat source, making them sink, while the denser fluids heat up as they near the heat source, making them rise. This creates convection currents.		<onlyinclude>'''Convection''' is the motion of a [[fluid]] driven by [[temperature]] differences across that fluid. When a fluid is [[heat]]ed, the region in closest contact with the heat source becomes less [[density\|dense]] due to increased [[kinetic energy]] in the particles</onlyinclude>. The portion of fluid that is less dense then rises, while the denser portion of fluid sinks. The process repeats itself because the less dense fluids cool down as they move away from their heat source, making them sink, while the denser fluids heat up as they near the heat source, making them rise. This creates convection currents.

	Convection~~, along with~~ [[thermal conduction]]<ref name=Knight>R. D. Knight, "Work," in ''Physics for Scientists and Engineers: A Strategic Approach,'' 2nd ed. San Francisco: Pearson Addison-Wesley, 2008, ch. 11, pp. 325–327</ref>, [[radiant energy]]<ref name=Knight/> and [[evapotranspiration]]<ref>R. Wolfson, "High-Energy Society," in ''Energy, Environment and Climate,'' 2nd ed. New York: Norton, 2012, ch. 12, pp. 333</ref~~>, is one of the fundamental ways that heat is [[Heat transfer mechanisms\|transferred]].~~		Convection is one of the fundamental ways that heat is [[Heat transfer mechanisms\|transferred]]. The others are [[thermal conduction]],<ref name=Knight>R. D. Knight, "Work," in ''Physics for Scientists and Engineers: A Strategic Approach,'' 2nd ed. San Francisco: Pearson Addison-Wesley, 2008, ch. 11, pp. 325–327</ref> [[radiant energy]]<ref name=Knight/> and [[evapotranspiration]].<ref>R. Wolfson, "High-Energy Society," in ''Energy, Environment and Climate,'' 2nd ed. New York: Norton, 2012, ch. 12, pp. 333</ref>
	~~<br /~~>

	[[File:Convection cell atmos labeled.gif\|~~framed~~\|left\|Figure 1. Air over land heats faster than air over water, leading to convection which feels like a cool ocean breeze<ref name=Book1>”Properties of Matter Reading Selection: Density Creates Currents.” [Online]. Available: http://www.propertiesofmatter.si.edu/Density_Creates.html</ref>. ]]		[[File:Convection cell atmos labeled.gif\|thumb\|350px\|left\|Figure 1. Air over land heats faster than air over water, leading to convection which feels like a cool ocean breeze.<ref name=Book1>”Properties of Matter Reading Selection: Density Creates Currents.” [Online]. Available: http://www.propertiesofmatter.si.edu/Density_Creates.html</ref>]]
			[[File: Convection cell room labeled.gif\|thumb\|375px\|right\|Figure 2. Convection warming a room is quiet and energy efficient.<ref name=Book1/>]]
			<br/><br/><br/><br/><br/><br/><br/><br/><br/><br/><br/><br/><br/>
	Convection plays a large role in wind patterns and in passive ventilation. The movement of wind across the globe is dependent on various spots where warm air rises and cool air sinks, creating large wind currents that affect weather. For example, air over land will typically get heated up by the sun during the day, while air over the sea will remain cool. The hot air over land will rise in the atmosphere. As it rises, it also cools down and becomes denser, causing it to sink once more. This concept is illustrated in Figure 1.<br />		Convection plays a large role in wind patterns and in passive ventilation. The movement of wind across the globe is dependent on various spots where warm air rises and cool air sinks, creating large wind currents that affect weather. For example, air over land will typically get heated up by the sun during the day, while air over the sea will remain cool. The hot air over land will rise in the atmosphere. As it rises, it also cools down and becomes denser, causing it to sink once more. This concept is illustrated in Figure 1.<br />
	~~<br />~~
			Similar to how convection works in the atmosphere, convection also causes passive ventilation (natural air movement) in a room, as shown in Figure 2. While natural convection can be used inside houses, [[forced convection]] is more common.

	==Forced convection==		==Forced convection==
	::''[[forced convection\|main article]]''		::''[[forced convection\|main article]]''
	[[File: Convection cell room labeled.gif\|framed\|left\|Figure 2. Convection warming a room is quiet and energy efficient<ref name=Book1/>.]] Similar to how convection works in the atmosphere, convection also causes passive ventilation (natural air movement) in a room, as shown in Figure 2.While natural convection can be used inside houses, [[forced convection]] is more common. This is where air currents are forced through a room by a fan. Forced convection can achieve the same effects as natural convection, the process is simply aided through devices like fans. If your house has heating vents on the bottom of your walls, this is an example of forced convection.		While natural convection can be used inside houses, [[forced convection]] is more common. This is where air currents are forced through a room by a fan. Forced convection can achieve the same effects as natural convection, the process is simply aided through devices like fans. If your house has heating vents on the bottom of your walls, this is an example of forced convection.


	<br />		[[File:winter.png\|400px\|framed\|right\|Figure 4. In the winter, ceiling fans should rotate clockwise to pull cool air up from the room and force warm air downwards, creating an updraft.<ref name=pic>''Created internally by a member of the Energy Education team''</ref>]]
			[[File:summer.png\|400px\|framed\|left\|Figure 3. In the summer, ceiling fans should rotate counterclockwise to mix warm air and force a cool breeze downwards, creating a downdraft.<ref name=pic/> ]]
			<br/><br/><br/><br/><br/><br/><br/>
			<br/><br/><br/><br/><br/><br/><br/>

	==References==		==References==
	{{reflist}}		{{reflist}}
	[[Category:Uploaded]]		[[Category:Uploaded]]

J.williams: 1 revision imported

2015-08-26T21:30:57Z

1 revision imported

← Older revision	Revision as of 21:30, 26 August 2015
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J.williams at 16:53, 12 August 2015

2015-08-12T16:53:00Z

New page

[[category:done 2014-08-16]]
<onlyinclude>Convection is the motion of a fluid driven by temperature differences across that fluid. When a fluid is heated, the region in closest contact with the heat source becomes less dense due to increased [[kinetic energy]] in the particles</onlyinclude>. The portion of fluid that is less dense then rises, while the denser portion of fluid sinks. The process repeats itself because the less dense fluids cool down as they move away from their heat source, making them sink, while the denser fluids heat up as they near the heat source, making them rise. This creates convection currents.

Convection, along with [[thermal conduction]]<ref name=Knight>R. D. Knight, "Work," in ''Physics for Scientists and Engineers: A Strategic Approach,'' 2nd ed. San Francisco: Pearson Addison-Wesley, 2008, ch. 11, pp. 325–327</ref>, [[radiant energy]]<ref name=Knight/> and [[evapotranspiration]]<ref>R. Wolfson, "High-Energy Society," in ''Energy, Environment and Climate,'' 2nd ed. New York: Norton, 2012, ch. 12, pp. 333</ref>, is one of the fundamental ways that heat is [[Heat transfer mechanisms|transferred]].
<br />

[[File:Convection cell atmos labeled.gif|framed|left|Figure 1. Air over land heats faster than air over water, leading to convection which feels like a cool ocean breeze<ref name=Book1>”Properties of Matter Reading Selection: Density Creates Currents.” [Online]. Available: http://www.propertiesofmatter.si.edu/Density_Creates.html</ref>. ]]
Convection plays a large role in wind patterns and in passive ventilation. The movement of wind across the globe is dependent on various spots where warm air rises and cool air sinks, creating large wind currents that affect weather. For example, air over land will typically get heated up by the sun during the day, while air over the sea will remain cool. The hot air over land will rise in the atmosphere. As it rises, it also cools down and becomes denser, causing it to sink once more. This concept is illustrated in Figure 1.<br />
<br />

==Forced convection==
::''[[forced convection|main article]]''
[[File: Convection cell room labeled.gif|framed|left|Figure 2. Convection warming a room is quiet and energy efficient<ref name=Book1/>.]] Similar to how convection works in the atmosphere, convection also causes passive ventilation (natural air movement) in a room, as shown in Figure 2.While natural convection can be used inside houses, [[forced convection]] is more common. This is where air currents are forced through a room by a fan. Forced convection can achieve the same effects as natural convection, the process is simply aided through devices like fans. If your house has heating vents on the bottom of your walls, this is an example of forced convection.

<br />

==References==
{{reflist}}
[[Category:Uploaded]]