Heat Transfer: Conduction, Convection And Latent Heat
Heat Transfer: Conduction, Convection and Latent Heat In addition to radiation, energy can also be transferred in the form of heat. There are three ways this can happen:
Heat Transfer: Conduction, Convection and Latent Heat In addition to radiation, energy can also be transferred in the form of heat. There are three ways this can happen: When heat simply diffuses through an object, passing from molecule to molecule, that's called conduction conduction of heat along a metal rod
Heat Transfer: Conduction, Convection and Latent Heat In addition to radiation, energy can also be transferred in the form of heat. There are three ways this can happen: When heat simply diffuses through an object, passing from molecule to molecule, that's called conduction As it turns out, air is actually very poor at diffusing heat through conduction.that is, air is a very poor conductor (- Equivalently, air is a very good insulator) As a result, conduction is really only important right next to the ground.over the lowest few cm, really
When heat is moved from place to place due to warm and cold air masses moving around, that's called convection a rising warm air bubble transfers heat by convection
When heat is moved from place to place due to warm and cold air masses moving around, that's called convection Some terminology: - Heat transfer due to vertical air motions is always referred to as convection.but - Heat transfer due to horizontal air motions is often called advection instead In the atmosphere, convection / advection is the main way of moving heat from place to place - Convection is much, much more efficient at transferring heat than conduction
Depending on the temperature, water in the air can exist in any of three phases: liquid, solid or gas (aka vapor). And. Transformations between these phases (referred to as phase changes) are accompanied by either the release or the absorption of heat, referred to generally as latent heating. Why do we care?
Depending on the temperature, water in the air can exist in any of three phases: liquid, solid or gas (aka vapor). And. Transformations between these phases (referred to as phase changes) are accompanied by either the release or the absorption of heat, referred to generally as latent heating. Why do we care? - If heat is released, it warms the surrounding air - If heat is absorbed, it cools the surrounding air
If water goes from. vapor to liquid liquid to solid vapor to solid solid to liquid liquid to vapor solid to vapor that's called. and the effect on the surrounding air is.
If water goes from. that's called. vapor to liquid condensation liquid to solid vapor to solid solid to liquid liquid to vapor solid to vapor and the effect on the surrounding air is.
If water goes from. that's called. vapor to liquid condensation liquid to solid freezing vapor to solid solid to liquid liquid to vapor solid to vapor and the effect on the surrounding air is.
If water goes from. that's called. vapor to liquid condensation liquid to solid freezing vapor to solid deposition solid to liquid liquid to vapor solid to vapor and the effect on the surrounding air is.
If water goes from. that's called. vapor to liquid condensation liquid to solid freezing vapor to solid deposition solid to liquid melting liquid to vapor solid to vapor and the effect on the surrounding air is.
If water goes from. that's called. vapor to liquid condensation liquid to solid freezing vapor to solid deposition solid to liquid melting liquid to vapor solid to vapor evaporation and the effect on the surrounding air is.
If water goes from. that's called. vapor to liquid condensation liquid to solid freezing vapor to solid deposition solid to liquid melting liquid to vapor evaporation solid to vapor sublimation and the effect on the surrounding air is.
If water goes from. that's called. and the effect on the surrounding air is. vapor to liquid condensation warming liquid to solid freezing warming vapor to solid deposition warming solid to liquid melting liquid to vapor evaporation solid to vapor sublimation
If water goes from. that's called. and the effect on the surrounding air is. vapor to liquid condensation warming liquid to solid freezing warming vapor to solid deposition warming solid to liquid melting cooling liquid to vapor evaporation cooling solid to vapor sublimation cooling
So water vapor in the atmosphere is thus a hidden form of heat, with the heat realized once condensation (or freezing, or deposition) occurs condensation and freezing in clouds releases latent heat to the surroundings, thus warming the air
Now, over most of the atmosphere, shortwave radiation from the sun passes straight through, without being absorbed - Exceptions: UV absorption in the stratosphere (by ozone) and X-ray and gamma-ray absorption in the thermosphere (by O 2 ) Question: If not the sun, then where does the atmosphere get its energy from?
Now, over most of the atmosphere, shortwave radiation from the sun passes straight through, without being absorbed - Exceptions: UV absorption in the stratosphere (by ozone) and X-ray and gamma-ray absorption in the thermosphere (by O 2 ) Question: If not the sun, then where does the atmosphere get its energy from? Answer: Most of the atmosphere's energy comes from from the Earth below
Now, over most of the atmosphere, shortwave radiation from the sun passes straight through, without being absorbed - Exceptions: UV absorption in the stratosphere (by ozone) and X-ray and gamma-ray absorption in the thermosphere (by O 2 ) Question: If not the sun, then where does the atmosphere get its energy from? Answer: Most of the atmosphere's energy comes from from the Earth below (Of course, the Earth gets its energy from the sun, so ultimately it does all come from the sun.just not directly)
Warming the Atmosphere from Below Step 1: Shortwave passes through and is absorbed by the ground, causing the ground to warm (radiation)
Warming the Atmosphere from Below Step 1: Shortwave passes through and is absorbed by the ground, causing the ground to warm (radiation) Step 2: Air in the lowest few cm is warmed by contact with the ground and moistened by evaporation
Warming the Atmosphere from Below Step 1: Shortwave passes through and is absorbed by the ground, causing the ground to warm (radiation) Step 2: Air in the lowest few cm is warmed by contact with the ground (conduction) and moistened by evaporation
Warming the Atmosphere from Below Step 1: Shortwave passes through and is absorbed by the ground, causing the ground to warm (radiation) Step 2: Air in the lowest few cm is warmed by contact with the ground (conduction) and moistened by evaporation (hidden heat)
Warming the Atmosphere from Below Step 3: Warm air rises, transferring heat upwards
Warming the Atmosphere from Below Step 3: Warm air rises, transferring heat upwards (convection)
Warming the Atmosphere from Below Step 3: Warm air rises, transferring heat upwards (convection) Step 4: As air rises it cools, leading to condensation.
Warming the Atmosphere from Below Step 3: Warm air rises, transferring heat upwards (convection) Step 4: As air rises it cools, leading to condensation, which brings latent heat release
Warming the Atmosphere from Below Of course, we also have absorption of radiation. it's just IR from the Earth instead of shortwave from the sun.
Warming the Atmosphere from Below Putting it together: Warming from below
Now for the details: The input energy stream Of the solar energy reaching the Earth. Roughly 30% is scattered or reflected back to space Another 19% is absorbed directly by the atmosphere (think ozone, O2, etc.)
Now for the details: The input energy stream Net result: Roughly 51% of the incoming solar radiation gets absorbed by the Earth's surface.
Now for the details: The total energy budget That 51% absorbed by the ground then gets distributed throughout the atmosphere.
Now for the details: The total energy budget .which can be pretty complex. But it's the same processes we've already discussed: radiation, conduction, convection and latent heat.
Heat Transfer: Conduction, Convection and Latent Heat In addition to radiation, energy can also be transferred in the form of heat. There are three ways this can happen: When heat simply diffuses through an object, passing from molecule to molecule, that's called conduction As it turns out, air is actually very poor at diffusing heat
Boiling water CONDUCTION CONVECTION RADIATION 43. Frying a pancake CONDUCTION CONVECTION RADIATION 44. Heat you feel from a hot stove CONDUCTION CONVECTION RADIATION 45. Moves as a wave CONDUCTION CONVECTION RADIATION 46. Occurs within fluids CONDUCTION CONVECTION RADIATION 47. Sun’s rays reaching Earth CONDUCTION CONVECTION RADIATION 48.
describe how heat moves by conduction, convection, and radiation. give examples of heat transfers that occur in every day situations. Vocabulary conduction: the transfer of heat through a material by direct contact. convection: the transfer of heat in a fluid (gas or liquid) as a result of the movement of the fluid itself.
the voltage applied and resistance of the heat source respectively, then using the energy balance, the net heat transfer (Q net) within the enclosure is given by- QQ Q Qnet conduction convection radiation ( 2 net Q V R ) The conduction heat transfer (Q conduction) at the enclosure side walls is determined as- wall conduction wall wall wall .
Chapter 5 Principles of Convection heat transfer (Text: J. P. Holman, Heat Transfer, 10th ed., McGraw Hill, NY) 5-1 INTRODUCTION We now wish to examine the methods of calculating convection heat transfer and, in particular, the ways of predicting the value of the convection heat-transfer coefficient h. Our discussion in this chapter will
Both temperature and heat transfer can change with spatial locations, but not with time Steady energy balance (first law of thermodynamics) means that heat in plus heat generated equals heat out 8 Rectangular Steady Conduction Figure 2-63 from Çengel, Heat and Mass Transfer Figure 3-2 from Çengel, Heat and Mass Transfer The heat .
(ignoring external natural convection), conduction through the wall, and natural convection and radiation to the interior wall. An important factor in the selection of this project was that it included all three major heat transfer mechanisms: conduction, convection, and radiation. It also included both major types of convection: forced and .
convection, pure solutal convection, heat transfer driven flows, and mass transfer driven flows were taken into account. Mobedi et al.,8,9 analyzed double diffusive convection in partially heated cavities. Nikbakhti and Rahimi10 studied numerically the flow, heat and mass transfer in
continue to meet with strategy groups and conduct shared reading and guided reading groups with a focus on print strategies and fluency based on students [ needs. **Although the unit details 22 sessions, this unit could easily utilize 6 weeks of instruction within the reading workshop.
