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Showing posts with label physical. Show all posts
Showing posts with label physical. Show all posts
Tuesday, March 22, 2016
Physical Principles: Electricity in the Atmosphere
Understanding Weather and Climate (7th Edition) (MasteringMeteorology Series) by Edward Aguado, James E. Burt
Physical Principles: A Closer Look at Divergence and Convergence
Understanding Weather and Climate (7th Edition) (MasteringMeteorology Series) by Edward Aguado, James E. Burt
Physical Principles: Vorticity and the Maintenance of Rossby Waves
Understanding Weather and Climate (7th Edition) (MasteringMeteorology Series) by Edward Aguado, James E. Burt
Labels:
angular,
climate,
earth,
maintenance,
meteorology,
momentum,
physical,
principles,
relative,
rossby,
vorticity,
waves,
weather
Friday, March 18, 2016
Physical Principles: What Causes El Ninos and La Ninas?
Understanding Weather and Climate (7th Edition) (MasteringMeteorology Series) by Edward Aguado, James E. Burt
Labels:
breakdown,
cause,
climate,
el nino,
ENSO,
la nina,
meteorology,
physical,
principles,
weather
Physical Principles: The Dishpan Experiment
Understanding Weather and Climate (7th Edition) (MasteringMeteorology Series) by Edward Aguado, James E. Burt
Labels:
climate,
dishpan,
eddies,
experiment,
meteorology,
physical,
principles,
rossby,
rotation,
turbulent,
wave,
weather
Physical Principles: The Movement of Rossby Waves
Understanding Weather and Climate (7th Edition) (MasteringMeteorology Series) by Edward Aguado, James E. Burt
Labels:
atmospheric,
climate,
meteorology,
movement,
physical,
principles,
rossby,
speed,
wave,
waves,
weather,
wind
Physical Principles: Maintaining General Circulation
Understanding Weather and Climate (7th Edition) (MasteringMeteorology Series) by Edward Aguado, James E. Burt
Labels:
atmosphere,
atmospheric,
circulation,
climate,
engine,
exchange,
general,
global,
heat,
maintaining,
meteorology,
momentum,
motion,
physical,
principles,
weather
Physical Principles: The Effect of Hail Size on Damage
Understanding Weather and Climate (7th Edition) (MasteringMeteorology Series) 7th Edition by Edward Aguado (Author), James E. Burt (Author)
Labels:
climate,
damage,
effect,
energy,
hail,
hailstones,
kinetic,
meteorology,
physical,
principles,
size,
weather
Physical Principles: Why Cloud Droplets Don't Fall
Understanding Weather and Climate (7th Edition) (MasteringMeteorology Series) by Edward Aguado, James E. Burt
Physical Principles: The Surprising Composition of Clouds
Understanding Weather and Climate (7th Edition) (MasteringMeteorology Series) by Edward Aguado, James E. Burt
Labels:
climate,
cloud,
composition,
meteorology,
physical,
principles,
water,
weather
Physical Principles: The Varying Value of the Saturated Adiabatic Lapse Rate
Understanding Weather and Climate (7th Edition) (MasteringMeteorology Series) by Edward Aguado, James E. Burt
Labels:
adiabatic,
climate,
lapse,
meteorology,
physical,
principles,
rate,
saturated,
value,
varying,
weather,
wet
Physical Principles: Adiabatic Lapse Rates and the First Law of Thermodynamics
Understanding Weather and Climate (7th Edition) (MasteringMeteorology Series) by Edward Aguado, James E. Burt
Labels:
adiabatic,
car,
combustion,
compression,
engine,
exhaust,
first,
intake,
lapse,
law,
meteorology,
physical,
piston,
principles,
rate,
thermodynamics
Physical Principles: The Coriolis Force
Understanding Weather and Climate (7th Edition) (MasteringMeteorology Series) 7th Edition by Edward Aguado (Author), James E. Burt (Author)
Labels:
acceleration,
atmosphere,
coriolis,
force,
meteorology,
physical,
principles,
rotation,
speed,
vertical,
weather,
wind
Physical Principles: The Hydrostatic Equation
Understanding Weather and Climate (7th Edition) (MasteringMeteorology Series) by Edward Aguado, James E. Burt.
► Hydrostatic Balance = if the net upwards force is equal to the downward force
─ For an atmosphere in hydrostatic balance, the balance of forces
in the vertical requires that…
► Or, the Hydrostatic
Equation:
─ The negative sign ensures that the pressure decreases with
increasing height
─ Because
we can rearrange the hydrostatic equation to
give…
► Above a fixed point on Earth…
─ That is, the pressure at height z is equal to the weight of
the air in the vertical column of unit cross-sectional are lying about that
level.
Hydrostatic
Equilibrium
► Pressure gradient force causes wind to flow from high to
low pressure
► Air pressure rapidly decreases with altitude
► Gravity pulls all mass, including the atmosphere, downward.
► Hydrostatic Equilibrium = vertical pressure gradient force and the force of
gravity are normally of nearly equal value and operate in opposite directions
─ When, gravitational force = vertical pressure gradient
force in magnitude à no vertical
acceleration occurs
─ When, gravitational force > vertical pressure gradient
force à downward motion
When, gravitational force < vertical pressure gradient force Ã
updrafts can develop that are associated with powerful thunderstormsPhysical Principles: Variations in Density
Understanding Weather and Climate (7th Edition) (MasteringMeteorology Series) by Edward Aguado, James E. Burt
Physical Principles: Velocity, Acceleration, Force, and Pressure
Understanding Weather and Climate (7th Edition) (MasteringMeteorology Series) by Edward Aguado, James E. Burt
Labels:
acceleration,
force,
gravity,
law,
Newton's,
physical,
pressure,
principles,
second,
speed,
velocity
Physical Principles: Earth's Equilibrium Temperature
Understanding Weather and Climate (7th Edition) (MasteringMeteorology Series) by Edward Aguado, James E. Burt
Physical Principles: The Sun
Understanding Weather and Climate (7th Edition) (MasteringMeteorology Series) by Edward Aguado, James E. Burt
Labels:
chromosphere,
convection,
disk,
flares,
fusion,
granules,
interior,
layers,
nuclear,
photosphere,
physical,
principles,
radiation,
solar,
sun,
sunspots,
zone
Physical Principles: The Nature of Radiation, Absorption, and Emission
Understanding Weather and Climate (7th Edition) (MasteringMeteorology Series) 7th Edition by Edward Aguado (Author), James E. Burt (Author)
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