CH 1 Atm
CH 2 Stability
CH 4, 8, 9 Pressure, Airmasses, Fronts
100

Layers of the atmosphere from surface to space

Troposphere, Tropopause, Stratosphere, Stratopause, Mesosphere, Mesopause, Thermosphere, (Exosphere).

100

An inversion is a sign of what type of atmospheric stability?

Stable Air

100

1 millibar = ___ feet of elevation

30 feet. 

The pressure difference between a strong High pressure center (1030 mb) and an intense Low pressure center (970 mb) is 60 mb = 1800 ft

200

The atmosphere is always trying to restore _______?

Equilibrium

200

What is the leading cause of instability in the atmosphere?

Heating of the earth's surface

200

International Standard Atmosphere for Pressure in all 3 units (" Hg, mb, psi)?

29.92" Hg, 1013.25 mb, 14.7 PSI

300
What does meteorology mean?

The study of weather (p.1)

300

SLR, DALR, MALR values. Define ELR.

Standard LR: -2C/+1000 ft

Dry Adiabatic LR: -3C/+1000 ft

Moist (Saturated) Adiabatic LR: -1.5C/+1000 ft

Environmental LR = What the LR actually is for the day

300

What are the 5 airmasses that affect the Continental US?

cP, cT, cA, mT, mP


400

Percentage of water vapor in the air fluctuates from _____ to _____

0% - 4%

400

LCL - What is it and what happens?

Lifting Condensation Level. Height of cloud bases. Where OAT = Dewpoint so air parcel is fully saturated, and begins rising at MALR.

400

What initially causes the formation of a frontal depression?

An upper air feature (p.84: Stage I)

500

Atmospheric Circulation: On a global level because of _____ and on a local level because ____

Global: Solar incidence/Unequal heating of the earth by the Sun

Local: Different surfaces absorb, retain, and reflect solar rays differently

500

Name the cloud type, turbulence level, visibility, precipitation type, and position of warm air vs cold air in both Stable and Unstable atmospheres

Stable: Stratiform, Smooth, Poor, STEADY, Cold below Warm

Unstable: Cumuliform, Turbulent, Clear, SHOWERY, Warm below Cold

500

List 3 differences between High and Low pressure systems

High: 1. Cold air aloft sinking down, 2. Rotates CW from center outwards (divergence) in Northern Hemisphere, 3. Fair weather, calmer winds

Low-pressure: 1. Warm air at the surface rotates inward, CCW (convergence) in N. Hemi., 2. Air rises up (convection), 3. Synoptic/bad weather, strong winds

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