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GHG Water vapor

Содержание

Structure of the AtmosphereThermosphereMesosphereOzone MaximumStratosphereTroposphereTemperature

Слайды и текст этой презентации

Слайд 1 GHG Water vapor

GHG Water vapor

Слайд 2Structure of the Atmosphere
Thermosphere
Mesosphere
Ozone Maximum
Stratosphere
Troposphere
Temperature

Structure of the AtmosphereThermosphereMesosphereOzone MaximumStratosphereTroposphereTemperature

Слайд 3Electromagnetic Spectrum
incoming
outgoing

Electromagnetic Spectrumincomingoutgoing

Слайд 41. Shorter, high
Energy wavelengths
Hit the earths
Surface

2. Incoming energy
Is

converted to heat

1. Shorter, highEnergy wavelengths Hit the earthsSurface2. Incoming energy Is converted to heat

Слайд 53. Longer, infrared
Wavelengths hit
Greenhouse gas
Molecules in the
atmosphere
4. Greenhouse gas
Molecules in

the
Atmosphere emit
Infrared radiation
Back towards earth

3. Longer, infraredWavelengths hitGreenhouse gasMolecules in theatmosphere4. Greenhouse gasMolecules in theAtmosphere emitInfrared radiationBack towards earth

Слайд 678% nitrogen

20.6% oxygen

< 1% argon

0.4% water vapor

0.036% carbon dioxide

traces

gases:
Ne, He, Kr, H, O3
Methane, Nitrous Oxide

78% nitrogen20.6% oxygen< 1% argon0.4% water vapor0.036% carbon dioxide traces gases:Ne, He, Kr, H, O3 Methane, Nitrous

Слайд 7Absorption Spectra of Atmospheric Gases
Anthes, p. 55
CH4
CO2
N2O
H2O
O2 & O3


atmosphere
WAVELENGTH (micrometers)
Infrared
Visible
UV

Absorption Spectra of Atmospheric GasesAnthes, p. 55 CH4CO2N2OH2OO2 & O3 atmosphereWAVELENGTH (micrometers)InfraredVisibleUV

Слайд 8Greenhouse gases absorb infrared radiation and prevent it from escaping

to space.

Carbon dioxide, methane, and nitrous oxide are very good

at capturing energy at wavelengths that other compounds miss




Greenhouse gases absorb infrared radiation and prevent it from escaping to space.Carbon dioxide, methane, and nitrous oxide

Слайд 9Climate Change - Greenhouse Gases
To be an effective greenhouse gas,

a molecule must:
- absorb light in the infrared region (must

have dipole moment for vibration mode)
- 3 modes of vibration for CO2 shown

O=C=O

O=C=O

O=C=O

Symmetric vibration not allowed

Climate Change  - Greenhouse GasesTo be an effective greenhouse gas, a molecule must:	- absorb light in

Слайд 10Earth’s Atmospheric Gases
Non- Greenhouse
Gases
99%
Greenhouse
Gases 1%

Earth’s Atmospheric GasesNon- GreenhouseGases99%GreenhouseGases 1%

Слайд 11Greenhouse Gases
Carbon Dioxide

Water

Methane

Nitrous Oxide

Greenhouse GasesCarbon DioxideWaterMethaneNitrous Oxide

Слайд 12 Greenhouse Gases
Molecules must absorb light in the right regions
-

roughly 7 to 25 μm region
- however, in some regions

(5 to 7 and 13 to 17 μm), essential no light from surface makes it to space due to current gases present
- for this reason, CO2 is less effective as a greenhouse gas (at least for additional CO2)
Greenhouse GasesMolecules must absorb light in the right regions	- roughly 7 to 25 μm region	- however,

Слайд 13 - Greenhouse Gases
Molecules absorbing light in the “IR window”

regions are more effective
Additional CO2 is not as effective as

additional N2O (absorbs at 7.5 to 9 μm) on a forcing per ppm basis

From Girard (old text)

- Greenhouse GasesMolecules absorbing light in the “IR window” regions are more effectiveAdditional CO2 is not

Слайд 14Selected Greenhouse Gases
Carbon Dioxide (CO2)
Source: Fossil fuel burning, deforestation


Anthropogenic increase: 30%
Average atmospheric residence time: 200 years
Methane (CH4)
Source:

Rice cultivation, cattle & sheep ranching, decay from landfills, mining
Anthropogenic increase: 145%
Average atmospheric residence time: 7-10 years
Nitrous oxide (N2O)
Source: Industry and agriculture (fertilizers)
Anthropogenic increase: 15%
Average atmospheric residence time: 140-190 years
Selected Greenhouse GasesCarbon Dioxide (CO2) Source: Fossil fuel burning, deforestation Anthropogenic increase: 30%Average atmospheric residence time: 200

Слайд 15Greenhouse Effect & Global Warming
The “greenhouse effect” & global warming

are not the same thing.
Global warming refers to a

rise in the temperature of the surface of the earth

An increase in the concentration of greenhouse gases leads to an increase in the the magnitude of the greenhouse effect. (Called enhanced greenhouse effect)
This results in global warming
Greenhouse Effect & Global WarmingThe “greenhouse effect” & global warming are not the same thing. Global warming

Слайд 16Global Energy Redistribution

Global Energy Redistribution

Слайд 17Radiation is not evenly distributed over the
Surface of the earth.

The northern latitudes have an energy deficit and the low

latitude/ equator has an excess. But the low latitudes don’t indefinitely get hotter and the northern latitudes don’t get colder.

Why?

The atmosphere and ocean transfer energy from low
latitudes to high

Radiation is not evenly distributed over theSurface of the earth. The northern latitudes have an energy deficit

Слайд 18The climate engine II
Since earth does rotate, air packets do

not follow longitude lines (Coriolis effect)
Speed of rotation highest at

equator
Winds travelling polewards get a bigger and bigger westerly speed (jet streams)
Air becomes unstable
Waves develop in the westerly flow (low pressure systems over Northern Europe)
Mixes warm tropical air with cold polar air
Net transport of heat polewards
The climate engine IISince earth does rotate, air packets do not follow longitude lines (Coriolis effect)Speed of

Слайд 19Atmospheric Pressure Decreases With Height Most of the energy is captured

close to the surface That energy drives climate and weather
50 percent

of mass of the atmosphere is within 6 km of the surface
Atmospheric Pressure Decreases With Height  Most of the energy is captured close to the surface

Слайд 20Cloud effects
Low clouds over ocean
more clouds reflect heat (cooling)
fewer clouds

trap heat (warming)
High clouds
more clouds trap heat (warming)

high: 5-14 km;

low < 2km

Cloud effectsLow clouds over oceanmore clouds reflect heat (cooling)fewer clouds trap heat (warming)High cloudsmore clouds trap heat

Слайд 21Fig. 19-10, p. 513

Fig. 19-10, p. 513

Слайд 22 - Greenhouse Gases
H2O as a greenhouse gas
- the molecule

responsible for the most greenhouse effect heating
- the third most

prevalent molecule in the atmosphere (on average, but composition is variable)
- direct anthropogenic sources are insignificant (at least outside of deserts and the stratosphere)
- also responsible for cooling through increasing albedo (in clouds) so normally kept separate from other greenhouse gases
- water vapor is important indirectly as planet heating increases water vapor (this is covered under feedbacks)
- Greenhouse GasesH2O as a greenhouse gas	- the molecule responsible for the most greenhouse effect heating	-

Слайд 23The sun plays a key role in the earth’s temperature
Researchers

think that atmospheric warming is not due to an increase

in energy output from the sun
Since 1975
Troposphere has warmed
Stratosphere has cooled

Warmer temperatures create more clouds
Thick, low altitude cumulus clouds – decrease surface temperature
Thin, cirrus clouds at high altitudes – increase surface temperature

The sun plays a key role in the earth’s temperatureResearchers think that atmospheric warming is not due

Слайд 24Water vapor is one of the most important elements of

the climate system. A greenhouse gas, like carbon dioxide, it

represents around 80 percent of total greenhouse gas mass in the atmosphere and 90 percent of greenhouse gas volume.
Water vapor and clouds account for 66 to 85 percent of the greenhouse effect, compared to a range of 9 to 26 percent for CO2. So why all the attention on carbon dioxide and its ilk? Is water vapor the real culprit causing global warming?
The answer is that water vapor is indeed responsible for a major portion of Earth’s warming over the past century and for projected future warming. However, water vapor is not the cause of this warming. This is a critical, if subtle, distinction between the role of greenhouse gases as either forcings or feedbacks. In this case, anthropogenic emissions of CO2, methane, and other gases are warming the Earth. This rising average temperature increases evaporation rates and atmospheric water vapor concentrations. Those, in turn, result in additional warming.
Water vapor is one of the most important elements of the climate system. A greenhouse gas, like

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