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Announcements

Announcements. Last lab group hand in kits Friday. If you were absent on Friday and have an excuse, see me ASAP to schedule a makeup exam. Second exam and first homework will likely be handed back after the election.

phillip-larsen
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Announcements

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  1. Announcements Last lab group hand in kits Friday. If you were absent on Friday and have an excuse, see me ASAP to schedule a makeup exam. Second exam and first homework will likely be handed back after the election.

  2. Survey question: Who is the head coach of one of the top five ranked college football teams in the BCS whose school colors are the same as my tie? • Mack Brown • Nick Saban • Joe Paterno • Bob Stoops • Pete Carroll

  3. NATS 101 Section 4: Lecture 22 Fronts

  4. Last time we talked about how air masses are created. When air masses meet, or clash, the transition zone is called a front.

  5. The concept of “fronts” in weather developed from the idea of the front line of battle, specifically in Europe during World War I

  6. Like the fronts in a war, weather fronts are where the air masses “battle it out” and they are the places where the exciting weather is usually found.Which air mass “wins” depends on what type of front it is.

  7. Four types of fronts COLD FRONT: Cold air overtakes warm air. B to C WARM FRONT: Warm air overtakes cold air. C to D OCCLUDED FRONT: Cold air catches up to the warm front. C to Low pressure center STATIONARY FRONT: No movement of air masses. A to B

  8. Fronts and Extratropical CyclonesFeb. 24, 2007 Case In mid-latitudes, fronts are part of the structure of extratropical cyclones. Extratropical cyclones form because of the horizontal temperature gradient and are part of the general circulation—helping to transport energy from equator to pole.

  9. Type of weather and air masses in relation to fronts: Feb. 24, 2007 case mP cP mT

  10. Characteristics of a front • Sharp temperature changes over a short distance • Changes in moisture content • Wind shifts • A lowering of surface pressure, or pressure trough • Clouds and precipitation • We’ll see how these characteristics manifest themselves for fronts in North America using the example from Feb. 2007…

  11. COLD FRONT Horizontal extent: About 50 km AHEAD OF FRONT: Warm and southerly winds. Cirrus or cirrostratus clouds. Called the warm sector. AT FRONT: Pressure trough and wind shift. Area of rain showers, which can be thunderstorms if the air ahead of the front is warm and moist enough. Unstable, vertically developed clouds. BEHIND FRONT: Rapid clearing and drying in the cold air. Pressure rises. Winds typically northerly or westerly.

  12. Fronts follow the pressure trough

  13. Note rapid change in dew point temperature and temperature in the vicinity of the cold front.

  14. Typically a line or lines of showers or thunderstorms on a cold front. These are called squall lines.

  15. ENHANCED IR SATELLITE IMAGE Very cold, highly vertically developed clouds along the cold front in Arkansas where the squall lines are. APPROXIMATE COVERAGE OF LITTLE ROCK RADAR

  16. WARM FRONT Horizontal extent: About 600 km AHEAD OF FRONT: Easterly to Southeasterly winds. Widespread precipitation from stable clouds like nimbostratus. May include fog. As get father north away from the front precipitation typically transitions because the cold air layer gets deeper rain  freezing rain and sleet  snow AT FRONT: Pressure trough and wind shift to the south. BEHIND FRONT: Warming, rising pressure and southerly winds.

  17. FREEZING RAIN STEADY RAIN

  18. Rain on a warm front is typically widespread and steady. It is also not typically very heavy, as with the thunderstorms on the cold front. Note the lack of the really strong radar echoes here (i.e. not a lot of orange and red colors).

  19. Freezing rain is occurring in Iowa where the radar reflectivity is highest (yellows)

  20. Far enough north and west of the warm front is typically where the snow happens because the cold air is deep enough. Radar color key RAIN FREEZING RAIN or SLEET SNOW L

  21. SNOW

  22. OCCLUDED FRONT Cold front “catches up” to the warm front, forming a wedge of warm air above the ground. At the occlusion, precipitation may range from widespread and steady to localized and heavy. Near the center of the low pressure.

  23. Occluded front in our example case extends from the center of the low pressure in central Kansas through southwest Missouri.

  24. L

  25. Tucson cold front passageThings to Note:Wind shifts (trees and smoke stack)Precipitation (squall lines)Temperature drop and lowering of cloud basesClearing at the end

  26. Summary of Lecture 22 AHEAD OF WARM FRONT Temp: Slow Warming Press: Falling Wind: E-SE Dew Pt: Rising Sky: Lowering Ceiling Wx: Steady Precip., Low Vis. AHEAD OF COLD FRONT Temp: Warm Press: Steady Wind: S-SW Dew Pt: High Sky: Variable Wx: Showers and T-storms WARM SECTOR BEHIND COLD FRONT Temp: Rapid Cooling Press: Rapid Rising Wind: W-NW Dew Pt: Lowering Sky: Clearing Wx: Improving

  27. Reading Assignment and Review Questions Reading: Chapter 12 Chapter 11 Questions Questions for Review: 12,15,16 Questions for Thought: 6,7,8,9,10,11

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