ATM OCN (Meteorology) 100
ATMOSPHERIC TEMPERATURE:
A FUNDAMENTAL WEATHER ELEMENT
Summer 2000
Lecture #3 Scheduled for:
14 JUN 2000 (W)
Recommended Readings from Moran and Morgan (1997):
pages 69-73 (left column); 24-25 (left column); 78-83; 102-105.
Today's Lecture 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 typical 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 from appropriate 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 ranging from the earth's surface to a height of several hundred kilometers, using the traditional temperature based nomenclature.
- To describe the general characteristics of the layers in the earth's atmosphere based upon the vertical variation in air 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
- Historical Background
- The Three Temperature Scales: Fahrenheit, Celsius and Kelvin
- Temperature Scale Conversions
C. THE CLIMATOLOGY OF NEAR-SURFACE AIR TEMPERATURE
- Temporal Variation in Air Temperature
- Diurnal cycle
- Annual cycle
- Spatial Variation in Observed Atmospheric Temperature
- North-south
- Continent-ocean
- 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 boundaries or "pauses"
- Reasons for the observed vertical temperature structure
- Implications of the vertical temperature structure
Links to Other References:
- A set of background documents for meteorological instruments, to include thermometers, at several levels of difficulty appear as Digital Library in the EarthLab Project , at a level intended for the general public. See other demonstrations entitled Weather Tools and Displays .
- Educational resource unit (K-12) on air temperature from Nebraska Earth Science Education Network (NESEN):
- All-time temperature extremes by state (from NCDC).
Last revision 15 June 2000 (0450 UTC)
Produced by Edward J. Hopkins, Ph.D.
Department of Atmospheric and Oceanic Sciences
University of Wisconsin-Madison Madison, WI 53706
hopkins@meteor.wisc.edu
URL: aos100/lectures/0003tmp.html
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