chapter 5 air pressure - #1 element of weather prediction
TRANSCRIPT
Air Pressure
Air pressure is a measure of the force that air exerts on a surface
Weight per unit area of the column of air above that location– Weight = mass * acceleration due to gravity
Average air pressure at sea level – 1.0 kg/cm2
– 14.7 lb/in2 – The air pressure at any point is the same in all
directions
Mercurial Barometer
More accurate than aneroid Invented by Torricelli in 1643 One meter (39 inches) long glass
tube sealed on one end Open end is inverted in pool of
mercury Height of mercury changes as
pressure changes Adjustments are required for
temperature and latitude
Aneroid Barometer
Flexible evacuated chamber with a spring inside
As pressure changes allow the chamber to flex
This causes movement in gears which display the pressure
Air Pressure Tendency
The change in air pressure with time– Rising: continuing fair or clearing weather– Falling: approaching inclement weather– Steady: no change
Barograph– An instrument that provides a continuous trace of
air pressure with time Altimeter
– An aneroid barometer that is calibrated to measure altitude or elevation
Air Pressure Meteorologists often express altitude in terms of
pressure (850mb map) Worldwide range in air pressure averages
between 970mb and 1040mb Lowest: 870mb (25.69in Hg) in Typhoon Tip
near Guam (Peak Winds of 190 mph)
Highest: 1083.8mb (32.01in Hg) in Siberia
Variations in Air Pressure With Altitude
The maximum air density is at the surface
Number density: the number of gas molecules per unit volume– Decreases with altitude
Thinning of the air with altitude is associated with decline in air pressure
50% atmosphere’s mass below 3 miles 99% atmosphere’s mass below 20
miles
The Standard Atmosphere: a model of the real atmosphere averaged across all latitudes for all seasons characterized by
1. Sea level air temperature of 15oC
2. Sea level pressure of 1013.25mb
Variations in Air Pressure With Altitude
Denver (mile high city) has an average air pressure 83% less than Boston– Altitude sickness– Lexington is about 900 feet above sea
level, so actual pressure is less than “fixed” pressure
In very sparse air (thermosphere) temperature is very high, but heat transfer is low
Horizontal Variations in Air Pressure On a surface weather map, variations in
pressure due to altitude are removed by determining what the pressure would be at that point if that point were at sea level
Easier to observe variations in pressure from one place to another by day and hour
Influence of Temperature and Humidity Generally, temperature has a greater
influence on density and pressure than water vapor
Air pressure drops more rapidly with altitude in cold (more dense) air than warm (less dense) air
Dry air is more dense that humid air!!
Influence of Temperature and Humidity Cold, dry air masses are more dense
and produce higher surface pressures than warm, humid air masses
Change in air pressure is usually accompanied by a change in air mass
The Gas Law (Equation of State)
Variables of State: temperature, pressure, and density
p = ρRT– Pressure (p)– Density (ρ)– Gas Constant (R)– Temperature (T)
In the atmosphere these 3 variables are constantly changing
The Gas Law
P = ρRT Pressure is held constant
– If T increases then ρ decreases– If ρ increases then T decreases
Temperature and Pressure are inversely proportional
The Gas Law
P = ρRT Density is held constant
– If T increases then P increases– If P increases then T increases
Temperature and Pressure are directly proportional
The Gas Law
P = ρRT Temperature is held constant
– If P increases then ρ increases– If ρ increases then P increases
Density and Pressure are directly proportional