The transfer of heat by convection can be seen clearly by a simple example like heating a pot of water over a stove. When the stove is first turned on heat is transferred first by conduction between the element through the bottom of the pot to the water. However, eventually the water starts bubbling - these bubbles are actually local regions of hot water rising to the surface, thereby transferring heat from the hot water at the bottom to the cooler water at the top by convection. At the same time, the cooler, more dense water at the top will sink to the bottom, where it is subsequently heated. These convection currents are illustrated in the following figure.
Consider now two regions separated by a barrier, one at a higher pressure relative to the other, and subsequently remove the barrier, as in the following figure. These convection currents are illustrated in the following figure.
When the barrier is removed, material in the high pressure (high density) area will flow to the low pressure (low density) area. If the low pressure region was originally created by heating of the material, one sees that movement of material in this way is an example of heat flow by convection.
Convection in our daily lives...
1. Creation of breezes over land masses next to large bodies of water.
Water has a larger heat capacity than land, and subsequently holds heat better. It therefore takes longer to change its temperature, either upward or downward. Thus, during the day the air above the water will be cooler than that over the land. This creates a low pressure area over the land, relative to the high pressure area over the water, and subsequently one finds breezes blowing from the water to the land.
On the other hand, during the night water cools off more slowly than the land, and the air above the water is slightly warmer than over the land. This creates a low pressure area over the water relative to the high pressure area over the land, and breezes will blow from the land to the water. ![](https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEh-3ppZ72n1j5dP-0phqxkMsJwqDWhmkAPpbiXMczTnUOKGWK8osVLbsBQ-JePdkH6Eu4Cgc8lYg0NHesPF8ZPudSvxjpoEyzIhBW9gUceawDYnoUmO4bi9nALzrnWkmIeqbtUkqXstscI/s320/img121.gif)
2. Convection currents in the Earth's System
![](https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEh-3ppZ72n1j5dP-0phqxkMsJwqDWhmkAPpbiXMczTnUOKGWK8osVLbsBQ-JePdkH6Eu4Cgc8lYg0NHesPF8ZPudSvxjpoEyzIhBW9gUceawDYnoUmO4bi9nALzrnWkmIeqbtUkqXstscI/s320/img121.gif)
2. Convection currents in the Earth's System
Large convection currents in the aesthenosphere (70 ~ 250 km from surface of the Earth)transfer heat to the surface, where plumes of less dense magma break apart the plates at the spreading centers, creating divergent plate boundaries. As the plates move away from the spreading centers, they cool, and the higher density basalt rocks that make up ocean crust get consumed at the ocean trenches/subduction zones. The crust is recycled back into the aesthenosphere. Thus, convection currents are also part of the eruption of volcanoes and earthquakes.
![](https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhfIx-6tP4KTUW0Mbg6vC4qmDqgMrb1DQbktN7WN2qhrjPEZmDrpgVfp1NDWAuCt8ks0TcE5Vx-BP8VfQmSi7_IpVsGKXYrg4n-iH6ug-XAE9R2p8ecPvQob-KMXS9mmtsaP8RhPB7NOAU/s400/untitled.bmp)
*Fun experiment: the papers can be lifted above the warm radiator, due to rising convective air current
1. Convection Oven
In a convection oven, the air in the oven must circulate freely. Shape of food affects convection cooking. A long thin meat cooks faster than a bulky one of the same weight because more surface is exposed to moving hot air. Size of pan also must be considered. The same quantity of food cooks faster in two small pans than it does in one large pan since air can circulate more freely.
2. Water kettle
The heating coil of a kettle is always placed at the bottom of the kettle. This is to aid transfer of thermal energy in water by convection. When the power is on, the water nearest to the coil would heat up, making it expand and less dense. This heated water would then rise while the cooler water regions in the upper part of the water body would descend to replace this heated water. Thus, a convection current is set up.
3. Hot water systems
Procedure:
1. Water is heated in the boiler by the gas burners. This water expands and becomes less dense; causing it to rise and flow into the upper half of the cylinder.
2. To replace this hot water, cold water would come down from the cistern and into the lower portion of the cylinder, and then to the boiler. This is caused by the pressure difference.
3. The overflow pipe is attached to the cylinder lest the temperature of the water becomes too high and cuases a large expansion of the water.
4. The hot water tap (leads to the overflow pipe) must be lower than the cistern; so as to ensure that the pressure difference between the cistern and tap causes the water to flow out of the tap.