Chapter 3 - Cal State LA
Download
Report
Transcript Chapter 3 - Cal State LA
Chapter 3: Air Temperature
Daily Temperature Variations
Maximum temperature recorded late afternoon
Minimum temperature recorded just before sunrise
Incoming radiation stops around late afternoon
Afternoon temperature recorded around
• Later during the summer
• earlier during the winter
All of this, of course, depends on
• Cloud cover and
• Local effects such as
Santa Ana winds and ‘offshore wind effects’
Daily Temperature Range
Daily temperature range
Difference between the daily maximum and daily
minimum temperatures
Daily range in temperatures is much larger
on clear days than on cloudy days
Daily Temperature Range Can depend on
Cloud cover
Humidity
Annual Temperature Range
Difference between the average temperature of the
warmest and coldest months
Warmest part of day late afternoon
Radiation Cooling
Occurs at night
Creates a ‘radiation inversion’
When ground is cooler than air above
Can observe fog at ground on after a storm
Cold temperatures
At night
Warm daytime
Temps
Clouds help
To keep in temps
Radiation cooling
Causes valleys to
Be cold at bottom
Special Topic
Record high temperatures
Record low temperatures
When it comes to temperature, what is
normal?
A thousand degrees and freezing to death
Controls of Temperature
Latitude
Equator
Polar regions
Land and water
Beaches
Mountains
Deserts
Ocean currents
California current/Gulf stream
Elevation
Valleys/mountains/coast
Specific Heat
Amount of heat needed to raise the
temperature of one gram of a substance by
one degree Celsius
Takes more heat to raise temperature of
oceans than to raise temperature of land.
This explains why our ‘oceans’ have memory
of heat stored and can determine climate
over ‘decades’.
Mean Average Temperature
This is the average temperature of any
weather station for the entire year
Average is just a fancy name for ‘normal’
What is normal temperature for L.A. for this
time of year?
This can be applied to the rainfall total for
this time year
Tables to look at….
Wind Chill Table……3.2
How cold the wind makes us feel
The ‘feels like’ temperature
Measuring air temperature
Instrument Shelter
Liquid glass thermometer
Maximum Thermometer
Minimum Thermometer
Instrument shelter must be at
Least several feet from the ground
Automation of Weather Instruments
Automated Surface Observing Systems
(ASOS)
Electronic weather stations
End of Chapter 3
Key Terms
Questions for review
1, 2, 3, 5, 6, 8, 9, 10, 14ab, 15
Questions for thought…..
1, 2, 5, 7, 8