Meteo 300 -- Introduction to the Atmospheric Sciences
Study Sheet for the Final Exam
Study everything on this study guide. If you really understand
everything on this study guide, you have a very good chance of doing well
on the final exam. The exam with have one section of short answer
questions, definitions, and equations. The rest of the exam will
be questions that require somewhat longer answers and problems related
to those you have already done or seen. About a third of the exam
will be on the material not covered by the other two exams.
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Fraction of air that is nitrogen, oxygen, water vapor, and carbon dioxide.
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Variation of pressure with altitude: equation -- p = po exp(-z/H)
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Vertical temperature distribution: "spheres" amd "pauses".
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Ideal gas law: equation in any form -- for example, pV = nR*T.
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Avagadro's number: 6.02x1026 molecules per mole
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Dalton's law of partial pressures: concept.
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Virtual temperature: concept.
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Hydrostatic equilibrium: equation -- dp/dz = -g
r
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Geopotential: definition and concept.
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Hyposometric equation and thickness: concept and important variables.
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Relationship between thickness and average temperature of the layer.
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The First Law of Thermodynamics: equation -- du = dq - dw.
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Relationship between work and pressure and volume: equation -- dW
= p dV.
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Specific heat: constant pressure and constant volume: equations
and concepts -- du/dT = cv, for example.
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Latent heats; concepts for water vapor.
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Latent heats and change in air temperature.
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Dry adiabatic lapse rate: concept and rough value.
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Potential temperature: equation and concept.
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Water vapor mixing ratio: concept and equation.
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Relative humidity: concept and equation.
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Lifting condensation level: concept and method for determining.
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Saturated adiabatic lapse rate: concept and approximate value.
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Equivalent potential temperature: concept.
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Stability -- be able to identify stable, unstable, and neutrally stable
air.
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Second Law of Thermodynamics
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The Carnot Cycle: description
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Carnot Cycle Efficiency: concept
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Entropy: definition and examples of entropy increases
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First Law of Thermodynamics: equation with entropy in it
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Reversible and Irreversible processes: definition
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Clausius Clapeyron Equation: concept and equation
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Lifting Condensation Level in terms of adiabatic expansion and the Clausius
Clapeyron Equation
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Cloud types and their characteristics (thickness, LWC, vertical velocities,
lifetimes)
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Synoptically forced thunderstorms: characteristics
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Squall lines: characteristics
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Five Latin roots for clouds
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Aerosols: definition and types
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Supersaturation and subsaturation: definitions
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Homogeneous nucleation: concept
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Heterogeneous nucleation: concept
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Koehler Theory: How the Kelvin Effect and the Raoult Effect work to make
a cloud droplet
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Cloud growth by vapor deposition
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Cloud growth by collision-coalescence
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Cloud droplet growth and precipitation development in a warm cloud: the
big picture and the importance of each step
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Cloud drop growth and precipitation development in a cold cloud: the big
picture and the importance of each step
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Electromagnetic spectrum: relationship among frequencis, wavelengths, and
energies
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Absorption of a photon by a molecule: where the energy can be stored
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The order of energy for electronic excitation, vibration, rotation, or
translation of a molecule
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Solar zenith angle: concept
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Solar constant: dependence on distance from the sun and approximate value
for Earth
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Black-body radiation: concept and shape of the emission spectra
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Solar radiation absorbed by Earth: concept and equation
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Infrared radiation emitted by Earth: concept
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The Greenhouse Effect: concept
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Poleward energy flux: concept
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Four stages of cyclogenesis
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Converting x,y coordinates to r, latitude, longitude coordinates: know
Figure 8.1.
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Four vertical coordinates that are commonly used
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Two apparent forces - effective gravity and the Coriolis force - causes
and concepts
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Two real forces
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Geostrophic wind: concept
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Effects of friction on the wind: where is friction effective and what does
it do?
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The five primitive equations: list them
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Thermally driven circulation: concept