ATM OCN (Meteorology) 100 - Lecture 3
FORMATION OF CLOUDS, FOG, DEW & FROST
Fall 1997
Lecture #11 Scheduled for:
26 SEP 1997 (F)
Recommended Readings from Moran and Morgan (1997):
pages 136-146; 297-299; 153-164.
Objectives:
- To explain how the water vapor content of air is quantified
and define the following moisture parameters
- dewpoint temperature
- wet bulb temperature
- vapor pressure
- mixing ratio
- relative humidity
- To describe the relationship between temperature and the capacity
of air to hold water vapor.
- To explain the temperature dependency of relative humidity.
- To perform simple calculations involving moisture parameters.
- To list the mechanisms involved in cooling air to saturation.
- To identify the various lifting processes operating with the
atmosphere.
- To explain the types of cloud formation processes.
- To describe the condensation processes within a cloud.
- To distinguish between cloud condensation nuclei and ice forming
(or freezing) nuclei.
- To distinguish between warm clouds and cold clouds in both
composition and appearance.
- To compare and contrast the physical characteristics of fog
and clouds.
- To describe the various processes that result in fog development.
- To explain how dew and frost form
- To compare and contrast the physical characteristics of dew
and frost.
Outline:
A. INTRODUCTION
- What are clouds
- Why are clouds important
B. REQUIREMENTS FOR CLOUD FORMATION
- Statement of the Practical Problems
- The Need for Saturation Conditions
- The Role of the Condensation Process in Cloud Formation
- Mechanism for Condensation
- Supersaturation
- Cloud Condensation Nuclei
C. MECHANISMS FOR CLOUD FORMATION
- Formation Options
- Evaporation Mechanisms
- Cooling Mechanisms
- Expansional Cooling
- Evaporative Cooling
- Advection Cooling - Horizontal Transport
- Radiative Cooling
- Expansional Cooling Specifics
- Review of adiabatic processes
- Dry adiabatic lapse rate
- No phase change of water or R.H. less than 100%
- Rate is 10 Celsius
degrees per 1000 m (or 5.5 Fahrenheit degrees per 1000 ft)
- Saturation (moist) adiabatic lapse rate
- Phase change of water or R.H. = 100%
- Rate is 6 to 7 Celsius degrees per 1000 m (or 3 Fahrenheit
degrees per 1000 ft)
- Ways to lift for Expansional Cooling
- Dynamic Lifting --
- In surface low pressure systems
- Along fronts
- Lifting by Convection -- Localized heating
- Mechanical Lifting -- Over mountain barriers (orographic lifting)
D. LOW LEVEL SATURATION PROCESSES & PHENOMENA
- Fogs
- Definition
- Comparison between clouds and fog
- Fog Formation Mechanisms
- Cooling to Saturation
- Addition of moisture
- Significance
- Types of Fog
- Fog Types Classification by temperature:
- Warm fog
- Cold fog
- Ice fog (or ice crystal fog)
- Fog Type Classification by formation process:
- Radiation fog
- Upslope fog (or mountain fog)
- Frontal fog
- Advection fog
- Steam fog (also known as sea smoke)
- Rain fog
- Dew and Frost
- Definitions
- Formation
- Comparison and Contrasts
- Significance
Last revision 30 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