ATM OCN (Meteorology) 100 - Lecture 3
ATMOSPHERIC TEMPERATURE:
A FUNDAMENTAL WEATHER ELEMENT
Fall 1997
Lecture #5 Scheduled for:
12 SEP 1997 (F)
Recommended Readings from Moran and Morgan (1997):
pages 69-73 (left column); 24-25 (left column); 78-83; 102-105.
Objectives:
- To distinguish between temperature and heat.
- To list and describe the four commonly used thermometers.
- To discuss the factors that are necessary to obtain an accurate
air temperature reading.
- To compare and contrast the Celsius, Fahrenheit and Kelvin
temperature scales and perform conversions between each scale,
given a selected temperature reading.
- To list the usual values and the observed extreme ranges of
surface air temperature.
- To compute the daily mean, daily range, monthly mean, annual
mean and annual range of temperature at a locale from a provided
data set.
- To calculate heating- and cooling- degree day units given
the proper data and relate these calculations to expected fuel
consumption.
- To recognize the influence of the major controls of temperature
upon the world temperature distribution.
- To label the salient features of a typical vertical temperature
profile of the earth's atmosphere, using the traditional temperature
based nomenclature.
- To list and describe the general characteristics of the layers
in the earth's atmosphere based upon the vertical variation in
temperature.
- To identify the causes responsible for this temperature profile.
Outline:
A. BACKGROUND
- Definitions Temperature, Heat, Internal Energy
- Human Significance of Temperature
B. THERMOMETRY
- The Science of Thermometry
- Types of Thermometers
- Liquid-in-glass thermometers
- Maximum recording thermometers
- Minimum recording thermometers
- Deformation thermometers
- Electrical thermometers
- Radiation thermometers (radiometers)
- Measurement Requirements
- Temperature Scales
C. THE CLIMATOLOGY OF NEAR SURFACE AIR TEMPERATURE
- Temporal Variation in Atmospheric Temperature
- Spatial Variation in Observed Atmospheric Temperature
- Average Daily Temperatures and Degree Day Units
D. VARIATION OF OBSERVED AIR TEMPERATURE WITH HEIGHT
- Temperature lapse rates
- Layer nomenclature
- isothermal, inversion, lapse
- The Standard Reference Atmosphere
- The Temperature Spheres
- The pauses or boundaries
- Reasons for the observed vertical temperature structure
- Implications of the vertical temperature structure
Links to Other References:
Last revision 10 September 1997
Produced by Edward J. Hopkins, Ph.D.
Department of Atmospheric and Oceanic Sciences
University of Wisconsin-Madison Madison, WI 53706
hopkins@meteor.wisc.edu