Chapter 1 Anatomy of a Cyclone
Extra-tropical cyclone – an area of low pressure outside of the tropics
Other names for extra-tropical cyclones: Cyclone Mid-latitude cyclone Synoptic cyclone Frontal cyclone Storm system
Severe weather associated with extra-tropical cyclones: Rain Floods Mudslides Tornadoes Heavy snow
What are the atmospheric processes responsible for the formation and evolution of extra-tropical cyclones?
This is the main topic of ATOC 4720.
Describing the Atmosphere
SI (Système Internationale) Units
Length: meter (m) Mass: kilogram (kg) Time: second (s) Temperature: Kelvin (K)
(see Appendix 2 for additional derived SI units)
Atmospheric Temperature
Troposphere – lowest layer of the atmosphere, where temperature normally decreases with increasing altitude
Tropopause - the boundary between the troposphere and stratosphere Atmospheric Pressure
Horizontal and vertical variations in pressure give rise to atmospheric motions (which are the focus of ATOC 4720).
What is atmospheric pressure?
A molecular perspective…
SI Units for pressure
Pressure is a force per unit area:
From Newton’s second law: F=ma
Force has units of kg m s-2 (or Netwons – N)
Force per unit area has units of: kg m-1 s-2 = N m-2 (or Pascals – Pa)
Other commonly used units of pressure:
1 hPa = 100 Pa 1 millibar (mb) = 1 hPa
In the atmosphere the observed pressure is also proportional to the weight of air above the observation point.
Therefore, pressure decreases with increasing altitude in the atmosphere.
What is the rate of change of pressure with height in the lower atmosphere? Surface pressure – the actual air pressure measured at the surface of the earth
Mean sea-level pressure (MSLP) – surface pressure interpolated to zero elevation (sea level)
Why do meteorologists use MSLP instead of surface pressure?
Isobar – contour line of constant pressure
What is the pressure at point A (point B) on the sea level pressure map at the left?
Station Reports
What are the typical weather observations made at surface weather stations around the world?
Dew point temperature – the temperature to which a small volume of air must be cooled at constant pressure in order for that air parcel to become saturated
Dew point temperature indicates the amount of moisture contained in the air.
What units are used for temperature and dew point temperature reported on station models?
Significant weather
Cloud cover Wind direction – the direction the wind is coming from
Why do meteorologists indicate the direction that the wind is coming from?
Wind speed
Units for wind speed SI: m s-1 Meteorological convention: Knots (kts) 1 kt = 0.51 m s-1
Station model wind speed plotting convention: - Wind speed symbols shown in Figure 1.4 are additive - Actual wind speed is within ±2 kts of plotted wind speed
Sea level pressure
Decoding sea level pressure reported on station models
If coded SLP is greater than 500: Put a 9 in front of the 3 digit coded SLP Insert a decimal point between the last two digits Add units of mb Example: coded SLP = 956 Decoded SLP = 995.6 mb
If coded SLP is less than 500: Put a 10 in front of the 3 digit coded SLP Insert a decimal point between the last two digits Add units of mb Example: coded SLP = 052 Decoded SLP = 1005.2 mb
The normal range of sea level pressure is 950 to 1050 mb.
Record high sea level pressure: 1086 mb (Tosontsengel, Mongolia) Record low sea level pressure: 870 mb (Typhoon Tip, western Pacific)
Time and weather observations
UTC – Universal time coordinate GMT – Greenwich Mean Time Z – Zulu time
Quick facts about Universal Time Coordinate (UTC)
UTC is based on a 24 hour clock (so add 12 to any times after 12:59PM)
6AM UTC would be written as 06 UTC 12 noon UTC would be written as 12UTC 6PM UTC would be written as 18UTC
If UTC time is given as both hours and minutes it looks like this:
2:15AM UTC would be written as 0215 UTC 12:00 noon UTC would be written as 1200 UTC 10:20PM UTC would be written as 2220 UTC
UTC never switches from standard time to daylight savings time
This means we need to change how we convert between UTC and Mountain time depending on whether we are on standard time or daylight savings time
How do I convert from UTC to MST or MDT?
MST = UTC - 7 hours MDT = UTC - 6 hours
How do I convert from MST or MDT to UTC?
UTC = MST + 7 hours UTC = MDT + 6 hours
Air Masses and Fronts
Air mass – a large volume of the atmosphere with relatively uniform temperature and humidity
What conditions favor the formation of air masses?
What happens to an air mass when it moves away from its source region?
Front – boundary between differing air masses
Fronts are defined based on the thermodynamic differences across the front and the direction of movement of the air masses on either side of the front.
Surface Weather Maps
Upper Level Weather Maps
Since pressure always decreases with height, and above any given spot on the earth each height has a unique pressure, we can use pressure as a vertical coordinate.
Weather data on upper level weather maps are plotted on constant pressure surfaces rather than constant height surfaces.
Pressure surface – an imaginary surface above the ground where the pressure has a constant value
One of the key properties meteorologists are interested in when looking at a constant pressure map is the height of the constant pressure surface.
The height of a constant pressure surface varies with the temperature of the column of air below the pressure surface.
Lower heights correspond to a colder air column.
Therefore, we expect (and do) find lower constant pressure heights near the poles and higher heights in the tropics.
Commonly Used Constant Pressure Maps Pressure Approximate Approximate Level Altitude (ft) Altitude (km) 850 mb About 5,000 ft About 1.5 km 700 mb About 10,000 ft About 3.0 km 500 mb About 18,000 ft About 5.5 km 300 mb About 30,000 ft About 9.0 km 250 mb About 35,000 ft About 10.5 km 200 mb About 39,000 ft About 12.0 km
Upper Air Station Model
What are the differences between surface and upper air station models?
Trough – region of low heights on a constant pressure map
Ridge – region of high heights on a constant pressure map
Shortwave – a small ripple in the height field
Longwave – a large ripple in the height field
How does the height of the 500 mb surface vary from south to north on this map?
What is the relationship between winds and height contours on an upper level constant pressure map?
Does this relationship vary between the Northern and Southern hemispheres?
What wind direction should we expect to find in the mid-latitudes if lower constant pressure surface heights are found near the poles and higher heights are found in the tropics?
Isotherm – contour line of constant temperature
Baroclinic – temperature varies on a constant pressure surface Barotropic – temperature is constant on a constant pressure surface
The Structure of a Typical Extra-Tropical Cyclone
Extra-tropical cyclone characteristics: Size Pressure Winds
Polar front – boundary between warm tropical and cold polar air masses
Stages in the life cycle of an extra-tropical cyclone
What physical process causes the surface pressure to increase or decrease?
Convergence – accumulation of atmospheric mass Divergence – removal of atmospheric mass
Divergence associated with the shortwave shown in Figure 1.9a leads to the formation of a low pressure center at the surface of the earth.
What is the direction of circulation around this area of low pressure?
How does this circulation alter the distribution of temperature?
What types of fronts form in response to this circulation?
Warm sector – wedge of warm air ahead of an advancing cold front and behind a warm front
How does the height of the 500 mb constant pressure surface change in response to the changes in the distribution of temperature near the surface? Mature stage of a mid-latitude cyclone
Where are the upper level ridge and trough located relative to the surface low pressure center during the mature stage of the cyclone’s life cycle?
What determines how much the surface pressure decreases (or increases)?
Where are the clouds and precipitation located relative to the fronts in this cyclone?
How does the speed of movement of the cold and warm fronts differ?
What happens when the cold front catches up to the warm front?
Occluded front – a boundary that separates two cold air masses at the surface with warm air aloft
How does the position of the upper level trough relative to the surface low pressure center change once the cyclone has occluded?
What causes the cyclone to weaken and dissipate?