ATM OCN (Meteorology) 100
THERMODYNAMICS:
BEHAVIOR OF GASES IN THE ATMOSPHERE
Summer 2000
Lecture # 6 Scheduled for:
20 JUN 2000 (T)
Recommended Readings from Moran and Morgan (1997):
pages 120-121; 136-138, 147-149 (skim).
Today's Lecture Objectives:
-
To qualitatively apply the gas law (equation of state) to atmospheric processes.
-
To explain an adiabatic process as it pertains to motions in the atmosphere.
-
To determine the temperature changes experienced by a vertically moving
air parcel using the adiabatic process lapse rate.
-
To identify the various lifting processes operating with the atmosphere.
-
To explain how atmospheric stability influences vertical motion of air.
Outline:
A. INTRODUCTION
B. KINETIC THEORY OF MATTER
-
Definitions
-
Historical
-
Assumptions for gases
-
Variables describing the molecular state of a gas
-
Molecular Diffusion
C. THE GAS LAWS
-
Classical approach to Ideal Gas Law (or Equation of State)
-
Atmospheric application of Ideal Gas Law
-
Dalton's Laws of Partial Pressures
-
Atmospheric application of Dalton's Laws of Partial Pressures
D. THE THERMODYNAMIC LAWS
-
Introduction
-
First Law of Thermodynamics
-
Atmospheric application of the First Law of Thermodynamics
-
Adiabatic Processes
E. THE VERTICAL MOTION PROBLEM
-
Response of an air parcel
-
Specification of the parcel response - The adiabatic lapse rate
F. STATIC STABILITY
-
Importance
-
Stability - Instability Concept
-
Response of the atmospheric environment
-
Criteria for Static Stability (Instability) Determination
-
Processes which change static stability (instability)
-
Visual stability indicators
-
Graphical Analysis: The Thermodynamic Diagram
Last revision 6 June 2000
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/0006gas.html