Unit 2: Chapters 5, 6, 7 Flashcards
Q's 1 - 86 are from the study guide. 87 - 115 are from the first video sheet and 116 - 134 are from the second video sheet. Let's get A's!
What is standard atmospheric pressure?
14.7 lbs per square inch
What are the four ways standard atmospheric pressure can be expressed?
14.7 lbs per square inch
1013.25 millibars / hectopascals
101.325 kilopascal
?
How is pressure gradient calculated?
It is the relative closeness of isobars, indicating the horizontal rate of pressure change; the slope
What is an isobar?
lines of equal pressure
What is the coriolis effect?
deflection acts at 90 degrees from the direction of movement – to the right in the Northern Hemisphere and the left in the Southern Hemisphere.
How does coriolis force affect circulation around Northern Hemisphere High Pressure?
circulates clockwise
How does coriolis force affect circulation around Northern Hemisphere Low Pressure?
circulates counterclockwise
How does coriolis force affect circulation around Southern Hemisphere High Pressure?
circulates counterclockwise
How does coriolis force affect circulation around Southern Hemisphere Low Pressure?
circulates clockwise
Where on earth is there no coriolis effect?
The Equator
Be able to locate the position of the major wind and pressure belts that make up global circulation.
from top to bottom: polar high polar easterlies polar low westerlies subtropical high trade winds equatorial low trade winds subtropical high westerlies polar low polar easterlies polar high
Name the pressure belts and wind systems starting at the North Pole and working towards the South Pole.
polar high polar easterlies polar low westerlies subtropical high trade winds equatorial low trade winds subtropical high westerlies polar low polar easterlies polar high
How do pressure gradients affect the strength of the wind?
Closer isobars = stronger winds. Pressure of high to low creates wind
What causes monsoons?
Winter shift in intertropical convergence zone produces shift in trade winds location
Why is it dry in India and SE Asia during the winter?
thermally induced systems, outblowing dry
Why is it very wet in India and SE Asia during the summer?
monsoons
Be able to explain the cause of land breezes.
Nocturnal cooling over the land causes high air pressure there, a condition that creates an offshore flow of air.
Be able to explain the cause of sea breezes.
Land rapidly heats during the day, heating the air above. Air expands and rises, creating low pressure that attracts surface breezes from over the adjacent water body.
Be able to explain the cause of mountain breezes.
at night, the heat is quickly los from the face of the slope and cooled air flows downwards
Be able to explain the cause of valley breezes
warned air rises, creating a low-pressure cell and cooler air flows into the low pressure area
What is a katabatic wind?
spilling of air downslope, originate in cold upland areas and cascade toward lower elevations under the influence of gravity
ex. antarctica whipping winds off of icy cliffs
What is a Santa Anas wind?
high speeds, high temp, extreme dryness
What is the hydrolic cycle?
evaopration, condensation, precipitation
Know how temperature affects evaporation
high temp = high evaporation
Know how humidity affects evaporation
warm air prompts evaporation
Know how turbulence affects evaporation
more wind = more evaporation
Be able to define absolute humidity
mass of water vapor in a g / m^3
Be able to define specific humidity
amount of water vapor per unit weight of air
Be able to define relative humidity
how dense air is, how filled is the air with water vapor. water vapor / water vapor capacity
Define the relationship between temperature and holding capacity for water vapor in the atmosphere
an inverse relationship as temperature increases the capacity decreases
As temperature increases, what happens to the holding capacity of the atmosphere?
warmer temperatures = increasing holding capacity
What does the saturation curve indicate?
as temperature increases, so does holding capacity
How does the relative humidity change with regard to daily changes in temperature?
as temperature increases, relative humidity increases
How is relative humidity computed?
( actual water vapor / capacity ) x 100
What information is needed in order to calculate relative humidity?
actual water vapor and capacity
What is meant by Condensation level?
altitude by which condensation begins
What is meant Dew Point?
temperature at which water droplets begin to form
What is an air mass?
a large, variable parcel of air that is distinct from others.
Know the origin and characteristics of a cT air mass
continental tropical - hot and dry
Know the origin and characteristics of a mT air mass
maritime tropical - hot and wet
Know the origin and characteristics of a cP air mass
continental polar - cold and dry
Know the origin and characteristics of a mP air mass
maritime polar - cold and wet
Know the origin and characteristics of a A air mass
arctic - cold and dry
What is albedo?
rate at which light is reflected
Be able to describe the characteristics of a warm front
warm air ascends over cold air with temperature decreasing as air rises
Be able to describe the characteristics of a cold front
advancing cold air, lower portion moves slower than upper portion
Be able to describe the characteristics of an occluded front
2 cold air masses meet and push warm air up
Be able to describe the characteristics of a stationary front
no precipitation neutral front - no displacement
Be able to diagram a typical mid-latitude cyclone with associated air masses and fronts
circular air masses, warm air rises from southeast, cold air comes from south and northeast and north and west
Be able to identify in a mid-latitude cyclone the warm sector
Approaching from the east, into occluded front
Be able to identify in a mid-latitude cyclone the cold air
Approaches from the west, completes circle
Be able to identify in a mid-latitude cyclone the cool air
Approaches from the North East
Be able to identify in a mid-latitude cyclone the area of low pressure
Be able to identify the circulation pattern around a N.H. High pressure cell.
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