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ATM OCN 100 - Summer 2002 LECTURES 32 & 33. THUNDERSTORMS: MESOSCALE CONVECTIVE SYSTEMS A. INTRODUCTION Practical Questions What is a thunderstorm? Why do thunderstorms occur? Definitions (where...). MADISON’S CURRENT WEATHER. Madison Weather at 1000 AM CDT
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ATM OCN 100 - Summer 2002LECTURES 32 & 33 THUNDERSTORMS:MESOSCALE CONVECTIVE SYSTEMS A. INTRODUCTION • Practical Questions • What is a thunderstorm? • Why do thunderstorms occur? • Definitions (where...)
MADISON’S CURRENT WEATHER Madison Weather at 1000 AM CDT WED AUG 8 2001 Updated twice an hour at :05 and :25 Sky/Weather: SUNNY Temperature: 83 F (28 C) Dew Point: 71 F (21 C) Relative Humidity: 67% Wind: W7 MPH Barometer: 30.04F
A. INTRODUCTION (con’t.) • Definitions • A thunderstorm - contains thunder; • A thunderstorm day - a day with thunder. • A Mesoscale Phenomenon
Thunderstorm Hazards-Lightning Lightning is a killer(with more than 80 deaths in US per year)!
Thunderstorm Hazards-Lightning Lightning is a killer(with more than 80 deaths in US per year)!
New Conceptual Model of Charge Structure in Deep Convection from Balloon Data
Thunderstorm Hazards-Flash Floods Flash Flooding is a killer(with more than 120 deaths in US per year)!
Thunderstorm Hazards-Tornadoes Tornadoes are killers(with more than 60 deaths in US per year)!
Funnel Cloud When funnel clouds touch the ground they become…….
B. THUNDERSTORM GENESIS • Essential Ingredients • Low Level Moisture • Unstable Atmospheric Lapse Rate • Trigger (or Kicker) • Initial Setting & Initiation Processes • Free Convection • Forced Convection
STABLE CONDITIONSCompare Environment with DALRColder parcel sinks & returns to start
ABSOLUTELY STABLE CONDITIONSCompare Environment with SALR & DALRColder parcel sinks & returns to start
UNSTABLE CONDITIONSCompare Environment with DALRWarmer parcel continues upward
ABSOLUTELY UNSTABLE CONDITIONSCompare Environment with SALR & DALRWarmer parcel continues upward
If STABLE CONDITIONS for DryCompare Environment with DALRColder parcel sinks & returns to start
But UNSTABLE CONDITIONS for HumidCompare Environment with SALRWarmer parcel continues upward
CONDITIONALLY STABLE CONDITIONSCompare Environment with SALR & DALR
STABILITY CRITERIA • Absolutely Stable • Layer lapse rate less than saturation adiabatic lapse rate. • Absolutely Unstable • Layer lapse rate greater than dry adiabatic lapse rate. • Conditionally Unstable • Layer lapse rate lies between dry & saturation adiabatic lapse rates.
STATIC STABILITY (con’t.) • Processes which change static stability (instability) • Cool below, but warm above (stabilize) • Warm below, but cool above (destabilize) • Visual stability indicators
Mammatus These pocket clouds form from sinking air ahead of the most severe thunderstorms. If you see these….run for cover!!!!
THE “TRIGGER” • Free Convection • Air ascends due to destabilization; • Heat surface and/or cool aloft. • Orographic Lifting • Air ascends mountain slopes. • Frontal Lifting • Air ascends along cold front. • Dynamic Lifting • Upper level motions induce lifting.
C. THUNDERSTORM TYPES • Single-Cell Thunderstorms • “Air Mass” Thunderstorms • Orographic Thunderstorms • Frontal Thunderstorms • Squall-Line Thunderstorms • Mesoscale Convective Complexes (MCC) • Multiple-Cell Thunderstorms
D. THUNDERSTORM CLIMATOLOGY • Geographical & Seasonal Distribution • Time of Day • Duration of Thunderstorms • Reported Thunderstorm Intensities
Thunderstorm ClimatologySee Fig. 13.9, Moran & Morgan (1997)
E. CHARACTERISTICS OF THUNDERSTORMS • The Thunderstorm Cell Model • Life Cycle of a Non-Severe Thunderstorm Cell • Where…
Cumulus Stage in thunderstorm life cycleSee Fig. 13.2a, Moran & Morgan (1997)
Mature Stage in thunderstorm life cycleSee Fig. 13.2b, Moran & Morgan (1997)
Dissipating Stage in thunderstorm life cycleSee Fig. 13.2c, Moran & Morgan (1997)
F. SEVERE THUNDERSTORMS • Official Criteria for Severe Weather • Large hail(3/4 inch or large diameter); • and/or • Damaging Winds(surface wind gusts of 58 mph or greater). • Unofficial Criteria for Severe Weather • Tornadoes, Heavy Precipitation, Flash Flooding, Deadly Lightning
Vertical Cross section of Severe ThunderstormSee Fig. 13.11, Moran & Morgan (1997)
Ingredients for severe thunderstorm episodeSee Fig. 13.13, Moran & Morgan (1997)
F. SEVERE THUNDERSTORMS (con’t.) • Types of Severe Thunderstorms • Structure of Severe Thunderstorms • Synoptic Situations Favoring Severe Thunderstorm Weather • Movement of Severe Thunderstorm Cells
NWS Watches & Warnings • Severe thunderstorm watch • Issued by National Weather Service to alert public that conditions are favorable for development of severe thunderstorms (large hail &/or high winds). • Severe thunderstorm warning • Issued by National Weather Service to warn public that a severe thunderstorm has been sighted by storm spotters or has been indicated by radar.