Intro pt. 2a Flashcards
Global Atmospheric Composition &
Circulations: Water Vapor & Clouds
Atmospheric water
Most common transport: ______
High evaporation heat (2501 J/g at 0C)
Evaporation and condensation: important in ______ in the atmosphere
evaporation & precipitation
energy budget
Global Atmospheric Composition & Circulations: Water Vapor & Clouds
collectively: “evapo-transpiration”
Evaporation from a given surface depends on 4 things
FRWP
Flux of energy
Relative humidity
Wind movements
Properties of the surface
under properties of the surface, which refers to increased transport to the atmosphere as evaporation though the stomata of plants
Vegetation
Global Atmospheric Composition &
Circulations: Water Vapor & Clouds
Condensation in the free atmosphere does not always lead to precipitation…stops at
formation of clouds
3 main types of clouds:
Stratus
Cumulus
Cirrus
_____ Clouds with vertical development (above 50k ft)
_____ Middle clouds 6,500 – 20,000 ft.
_____ Low clouds, surface up to 6,500 ft.
_____ High clouds 20,000 ft and above
Cumulonimbus clouds
Altocumulus clouds
Nimbostratus clouds
Cirrus clouds
_____– formed by large-scale vertical movements (cm/s), lifetime: 1 day over oceans
____– bubble formed clouds, formed locally, due to heating of the Earth’s surface, rising velocity in m/s, lifetime – about 1 hour
____ – Tread-formed thin clouds, formed at larger heights (> 5 km), consists of ice particle
Stratus
Cumulus
Cirrus
- _____= physical condition of the atmosphere (particularly the troposhere) at a specific time and place with regard to wind, temperature, cloud cover, fog and precipitation
- _____= collective word for rain, hail, snow, etc.
- _____, highly variable and somewhat unpredictable
- _____= longer term view of the weather patterns of a particular locality
weather
precipitation
weather
climate
The energy that drives processes in the atmosphere: _____
Radiation from a black body
Incoming solar radiation
Albedo and angle of incidence
Outgoing long wave radiation
Heat balance
Solar energy
______ - Large gaseous globe; mainly hydrogen and helium
Kept warm by internal nuclear fusion
process.
Outer 1000 km of the sun’s surface: _____ (radius: 0.7 million km from center)
sun
photosphere
What happens to an incident electromagnetic radiation?
______- fraction of the incident radiation that
is reflected
______- fraction of the incident radiation that
is absorbed
______- fraction of the incident radiation that is transmitted
Reflectivity
Absorptivity
Transmissivity
A body that absorbs all electromagnetic radiation that falls on it is called a _____.
“perfect absorber” - _____
Neither transmits nor reflect any of the radiation that they intercept
black body
idealization
Realization of a black body:
An insulated enclosure with a ____ , through which light can pass through. The incident light is reflected to the internal surface (big surface
compared to the tiny hole).
very little of the reflected light can
pass back through the _____.
nearly all incident light is absorbed by the internal surface of the enclosure.
tiny hole
Realization of a black body:
A ___ often modeled as a black body, and electromagnetic radiation emitted from these bodies as black-body radiation.
The emitted light of a _ is generated in the photosphere, within which the photons of light interact with the materials in it and achieve a common temperature T that is maintained over a long period of time.
star or planet
star
A _____ is also a perfect radiator (emitter), i.e., the relative intensities of the different frequencies that it radiates are dependent only on its temperature.
black body
Radiation: ____ is a function
of Temperature
energy flux
_____: The wavelength of the peak radiance [lambda (max)] decreases linearly as the temperature increases, where c is a constant:
_____: intensity of radiant energy emitted at a given wavelength
and temperature T (shape of the curve)
_____ gives the power As , the total energy emitted as a function of temperature T. This power is calculated by adding up the areas under the curve of intensity vs. T. Sigma is the Stefan-Boltzman constant.
Wein’s Law
Planck’s Law
Stefan-Boltzmann Law
Radiation: ____ from a non-
black body
Energy flux
____– the ratio of the amount of radiative power emitted by a non- black body to that of a blackbody at the same temperature.
Emissivity
Radiation from the Sun
____: distribution of the emitted spectrum.
The ____is considered to behave as a black body having a surface temperature of ca. 6000 K.
At this temperature the radiation emitted (solar radiation) reaches a maximum intensity in the visible part of the electromagnetic part of the spectrum.
Solar spectrum
sun
Solar Radiation
___% Reflected, ___% absorbed
The Earth intercepts about 0.002% of the total
electromagnetic output of the Sun.
The Earth also emits radiation.
36%
64%
Solar vs. Earth’s Radiation
The _____ is not a perfect absorber nor a perfect emitter (radiator).
Its emission is less than that of a black body at the same temperature (294 K).
Earth and its atmosphere
Earth’s Radiation
____ is not smooth unlike that of a black body of the same temperature. There are deep throughs.
The atmosphere contains trace elements that absorb specific parts of the IR spectrum, particularly CO2, H2O and CH4.
The deep through in the emission spectrum at 15 myu m: due to CO2
None of the 15 myu m radiation escapes into space - warming the atmosphere.
The Earth’s atmosphere acts as a blanket keeping the surface warm - ____
Terrestrial spectrum
Greenhouse effect
The Earth’s surface temperature (ca. 294 K at the tropopause) is ___ than that of the Sun. - It emits radiation in the infrared range (IR).
Long-wave radiation vs solar radiation - short wave radiation.
much lower
___ - incoming solar radiation
___ - radiated out to space
Short-wave
Long-wave Terrestrial radiation
Radiation and Energy Budget
_ of the total radiation absorbed by the Earth is absorbed by the Earth atmosphere system. - warming of the Earth’s atmosphere
this energy warms the air and drives the atmospheric motion
73%
Radiation and Energy Budget
Over sufficiently long period, the energy budget of the Earth is balanced.
K = L
where
K is the total energy absorbed as the radiation from the sun.
L total energy emitted as radiation from the earth
if :
K = L: no net warming nor cooling
K > L: Earth would ____
K < L: Earth would ____
warm up
cool down
Radiation and Energy Budget
Radiation budget is not in balance at a local level.
- Near the ____: K > L
- Near the ____: K < L
There must be a mechanism that moves the energy from the equator to the poles.
equator
poles
Radiation and Energy Budget
Mechanism that moves the energy from the equator to the poles:
Circulatory movement of matter in both the lower atmosphere and the oceans.
Together, these _____ are responsible for many of the features of the global climate.
There is an overall decrease in the mean surface temperature with increasing latitude (from equator to pole)
circulatory systems
Variability in the intensity of sunlightat the surface of earth is due to the ____ of solar radiation
incident angle