Weather and Climate

aos.wisc.edu

Weather and Climate

First attempt at analysis . . .


Weather and Climate(Lecture 26)Instructor: Prof. Michael C. MorganTeaching Assistant: Dianna N. Nelson


Questions from last lecture


Which of the following conditions isbest for air mass development?A. flat terrain, light winds, high pressure regionB. mountainous terrain, light winds, low pressureregionC. flat terrain, strong winds, low pressure regionD. mountainous terrain, strong winds, lowpressure regionE. flat terrain, strong winds, high pressure regioncontrasts, pressure change, changes in windspeed


What kind of air mass originates over Alaska?A. maritime polarB. maritime tropicalC. continental polarD. continental tropical


Fronts are best identified on a weather map byA. temperature contrasts, pressure change,changes in wind speedB. pressure changes, changes in moisturecontent, changes in cloud heightC. changes in wind speed, pressurechange, regions of precipitationD. temperature contrasts, pressure change,changes in wind direction


A front is identified on asurface weather map by:1. Sharp temperature change overa short distance2. Shifts in wind direction3. Pressure (trough) and pressurechanges4. Changes in air’s moisture content5. Clouds and precipitation patterns


Fronts


A front is identified on asurface weather map by:Temperature ChangeWind ShiftMoisture Change


A stationary frontA. acts as a boundary between polar andtropical air massesB. brings cold air into regions of warm airC. brings warm air into regions of cold airD. is an area of deep convection andintense


Madison, WI is located inA. the tropicsB. the sub-tropicsC. the mid-latitudesD. the subpolar regionE. the polar region


Map discussionhttp://weatherbonk.comhttp://aurora.aos.wisc.edu/~morgan/personal_links.htmlhttp://weather.cod.edu/analysis/analysis.raob.html


Fronts


Types of fronts• There are three basic types of fronts:1. Stationary front2. Cold front3. Warm front


Stationary front• This type of front has essentially no movement• The weather along the front may be quitevariable with respect to clouds and precipitation• If the air on either side starts to move, thestationary front will become a cold or warmfront.• Generally is a boundary between polar andtropical air


Cold front


Slow moving (15kt) vs. fastmoving (25kt) cold fronts• Fast moving cold fronts are steeper• Slow moving have a broad area ofprecipitation and cloud cover behind thefront.• In front of a fast moving cold front, squalllines may develop.– Squall lines are a lone of active showers andthunderstorms with heavy rain and gustywinds.


Warm front


Warm front


Warm front


Thunderstorms• A thunderstorm is a storm containinglightning and thunder.• Thunderstorms occur all over the world


Formation - Ingredients• Moisture (water vapor) in the lowest levelsof the atmosphere• Cold, dry air aloft (2-3 miles above thesurface)• Lifting mechanism


Air Mass (Single-Cell)Thunderstorms• Formed by uneven heating of the earth’ssurface• Brief, but well-defined lifespan with threestages– Cumulus Stage– Mature Stage– Dissipating Stage


Three stages


Mature Thunderstorms• The updraft can become so strong that itpenetrates into a region of stable air,resulting in a overshooting top.


Which is mature and which isdissipating?


Lifespan of a Thunderstorm• A single cell, consisting of an updraft anddowndraft, lasts 20 minutes.• But we have all observed thunderstormsthat appear to last longer than 20minutes….WHY?


Multicell storms• Sometimes when the cold downdraft reachesthe surface, it may force the warm, moistsurface air upward• This rising air can condense and build a newthunderstormMulticell clusterMulticell line (Squall Line)


Downdrafts


Gust fronts


Gust front


Downbursts


Straight-line winds• Associated with a cluster of severethunderstorms• May exceed 90 knots• If wind damage extends 250 milesalong storm path, it is called aderecho.


Tree damageWhat does it look like from adownburst vs. a derecho?


What makes a thunderstorm asevere thunderstorm?


Severe thunderstorm• Hail ¾” or greater• Winds in excess of 50 knots (57.5 mph)•Tornado


Severe thunderstorms


Supercell thunderstorms


Capping inversion• An important component of creating asevere thunderstorm is the strength ofthe boundary layer cap.– Too strong nothing develops– Too weak numerous cumulus clouds– Just righthelps to funnel the air into astrong updraft


Supercell thunderstormsRadarWeather and Climate


Squall line


Squall line


Tornadoes


Tornadoes


Tornadoes


Tornado alley


Photos courtesy of Ross Lazear


Photos courtesy of Ross Lazear

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