1 MET 112 Global Climate Change MET 112 Global Climate Change - Lecture 3 The Earth’s Energy...
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Transcript of 1 MET 112 Global Climate Change MET 112 Global Climate Change - Lecture 3 The Earth’s Energy...
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MET 112 Global Climate Change - Lecture 3
The Earth’s Energy BalanceDr. Eugene Cordero
San Jose State University
Outline Energy Solar and terrestrial radiation Absorption and scattering Global energy balance
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Earth’s Energy BalanceEarth’s Energy Balance
Energy entering top of atmosphere
Energy entering the Earth’s surface
= Energy leaving top of atmosphere= Energy leaving top of atmosphere
= Energy leaving Earth’s surface= Energy leaving Earth’s surface
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There are three modes of energy There are three modes of energy transmission in the atmosphere.transmission in the atmosphere.
Conduction: the transfer of energy in a substance by means of molecular excitation without any net external motion.
Convection: the transfer of energy by mass motions within a fluid or gas, resulting in actual transport of energy.
Radiation: the propagation of electromagnetic waves through space.
Energy transmissionEnergy transmission
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ConvectionConvection
Electromagnetic radiation
Radiation is the transfer of energy by rapid oscillations of electromagnetic fields.
The most important general characteristic is its wavelength (), ____________________________.
Radiation travels through space at the speed of light (3 x 108 m s-1).
Defined as the crest-to-crest distanceDefined as the crest-to-crest distance
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Radiation
What emits radiation?– All objects with a temperature greater than 0°K emit
some type of radiation (energy) Examples:
Radiation laws:– Warmer objects emit more intensely than cold
objects. (Stefan-Boltzmann Law)– Warmer objects emit a higher proportion of their
energy at short wavelengths than cold objects. (Wien’s Law)
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Review questions
Considering the previous discussion– Which object would emit more (intensity) radiation:
Earth or Sun?
– If you were examining the radiation emitted by both the Sun and Earth, which would have a longer wavelength?
– What wavelength radiation are you emitting right now?
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Review questions
Considering the previous discussion– Which object would emit more (intensity) radiation:
Earth or Sun?
– If you were examining the radiation emitted by both the Sun and Earth, which would have a longer wavelength?
– What wavelength radiation are you emitting right now?
Sun
Earth
infrared
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Solar Radiation (Sunlight)
Sunlight is primarily made up of the following:– Visible Light (44%)– Infrared Radiation (48%)– Ultraviolet Radiation (7%)
Unit: 1 m =
0.000001 m
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Terrestrial or Longwave Radiation
Planets mainly emit infrared radiation Radiation emitted by
planets occurs mainly at wavelengths _____
than those contained in solar radiation
Solar Radiation (“Shortwave”)
Planetary Radiation (“Longwave”)
longer
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Solar vs. Terrestrial Radiation
The sun is much hotter than planets; therefore, sunlight consists of shorter wavelengths than planetary radiation;
Thus …
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Recap
______________ radiation comes from the sun and is composed of both ultraviolet and visible radiation
______________ radiation comes from the Earth and is composed of infrared radiation
Recall that everything (above a temperature of 0K) emits some type of radiation (energy) with a particular wavelength.
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Recap
______________ radiation comes from the sun and is composed of both ultraviolet and visible radiation
______________ radiation comes from the Earth and is composed of infrared radiation
Recall that everything (above a temperature of 0K) emits some type of radiation (energy) with a particular wavelength.
Shortwave or solar
Longwave or terrestrial
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Energy from the Sun
Obviously, the Sun provides the Earth with it’s energy. The question is, how much of the Sun’s energy does the Earth get?
Sun’s energy is either– Scattered (reflected away) or– Absorbed
Scattering happens by bouncing off – Particles in the atmosphere– Earth’s surface
Absorption happens when certain gases absorb the energy– The reality is the only certain gases absorb certain
wavelengths.
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Absorption of radiation
Absorption of shortwave radiation by atmospheric gas molecules is fairly weak; – most absorption of shortwave radiation
occurs at the Earth’s surface.
Most gases do not interact strongly with longwave radiation, however
– Greenhouse gas molecules absorb certain wavelengths of longwave radiation.
Absorption of Radiation in the Earth’s Atmosphere
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Incoming solar radiationIncoming solar radiation
Each ‘beam’ of incoming sunlight can be either:– Reflected back to space:
Clouds Atmosphere Surface
– Or absorbed; either by atmosphere (e.g. clouds or ozone) or Earth’s surface.
AlbedoAlbedo
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Longwave radiation is emitted from surface.
Some surface radiation escapes to space
Most outgoing longwave is absorbed in atmosphere (by greenhouse gases)
Greenhouse gases emit longwave upward and downward
Some atmospheric radiation escapes to space
Some atmospheric radiation is absorbed at the surface
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Greenhouse EffectGreenhouse EffectSequence of steps:
1. Solar radiation absorbed by earth’s surface.
2. Earth gives off infrared radiation.
3. Greenhouse gases absorb some of the Earth’s infrared radiation.
4. Greenhouse gases (water and CO2) give off infrared radiation in all directions.
5. Earth absorbs downward directed infrared radiation
Result: warmer surface temperature
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Energy Balance
Assume that the Earth’s surface is in thermodynamic equilibrium:
Thermodynamic Equilibrium: – The flow of energy
away the surface equals the flow of energy toward the surface Surface
Average surface temperature = 15°C
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Removal of greenhouse gases would decrease downward flow of energy; now energy away from surface is greater than energy toward surface.
Sudden Removal of all Greenhouse Gases
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Removal of greenhouse gases would decrease downward flow of energy; now energy away from surface is greater than energy toward surface.
Thus, average surface temperature starts to decrease.
Sudden Removal of all Greenhouse Gases
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As surface cools, emission of radiation decreases until balance is restored. At this point, cooling stops
Sudden Removal of all Greenhouse Gases
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As surface cools, emission of radiation decreases until balance is restored. At this point, cooling stops and equilibrium is restored.
Average surface temperature = -18°C
Result: A Very Cold Planet!
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Question
Start with the following diagram and assume the earth’s surface temperature is 15C and that the atmosphere has greenhouse gases.
Imagine that the concentrations of greenhouse gases were to increase by 50%. 1. Draw two more diagrams illustrating (with arrows) how the energy balance would change with the increase in greenhouse gases and explain why. 2. How would the average surface temperature change?
SurfaceAverage surface temperature = 15°C
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Earth’s Greenhouse Effect
Without the greenhouse effect, the surface temperature of Earth would be – Way Cold (-18°C)
Greenhouse gases play an important role in shaping climate.– More GHGs – warmer climate– Less GHGs – cooler climate
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Activity 2 Greenhouse Effect
Draw a diagram showing how the earth is heated by the Sun.
Include arrows and/or lines to indicate the ‘Energy Balance” of the earth.
Energy Balance – Energy coming in and energy going out.
Clouds, and reflected energy