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April 10, 2012. Joe Halvorson, Chris MacIntosh, Tim Marquis. Severe Weather and Storm Chasing. What causes a storm, severe parameters, tools. Severe Weather Basics. The Basics. Thunderstorms need three things to develop: Moisture Instability Lift/Trigger
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April 10, 2012 Joe Halvorson, Chris MacIntosh, Tim Marquis Severe Weather and Storm Chasing
What causes a storm, severe parameters, tools. Severe Weather Basics.
The Basics • Thunderstorms need three things to develop: • Moisture • Instability • Lift/Trigger • Severe storms need one more ingredient: • Wind shear (directional, speed)
Storm Types • Single cell: “popcorn” storms • Usually not severe, short-lived • Multicell: group of cells moving together • Moderate severe, tornado potential • Squall line: line of storms • Moderate severe, low tornado potential • Supercell: storm with a rotating updraft (mesocyclone) • Very high severe potential • Main tornado producer
Multicell radar 4 cells
Parameters • CAPE/CIN(H) • Bulk Shear • Storm-Relative Helicity • Energy Helicity Index • Others • LCL Heights, LI, Lapse Rates. • Supercell Composite, Significant Tornado Parameter
CAPE • Convective Available Potential Energy • Ability that a parcel has to rise • Large CAPE usually means large vertical velocities • Different types: • Surface-based • Mixed-layer (Mean layer) • Most unstable • 0–3 km • “Skinny” and “Fat” CAPE • Skinny: weaker updrafts • Fat: stronger updrafts
“Fat” CAPE CAPE! “Skinny” CAPE CAPE!
CAPE • Thresholds (in J kg-1): • 1–1,000 : Marginally unstable • 1,000–2,500 : Moderately unstable • 2,500–3,500 : Very unstable • 3,500+ : Extremely unstable • For 0–3 km CAPE, 100+ J kg-1 best for tornadic environment
CIN (CINH) • Convective Inhibition • “Cap,” can prevent instability from being realized • Negative CAPE • Ways to overcome CIN: • Heating (daytime or warm air advection) • Moisture • Lift
CIN (CINH) • Thresholds (in J kg-1): • 0–50 : Weak cap • 50–200 : Moderate cap • 200+ : Strong cap • These values are negative on most model and mesoanalysis charts.
CAPE/CIN: 24 May 2011 Surface-based Mixed-layer
Bulk Shear • Change in wind direction and speed with height put into a single number • Most useful: 0–1 km, Effective • Effective accounts for storm depth (inflow base to equilibrium level) • Thresholds • 0–1 km : 15-20+ kts supportive of tornadoes • Effective : 25–40+ kts supportive of supercells
Bulk Shear: 27 April 2011 Effective 0–1 km
Storm-Relative Helicity (SRH) • Measure of the potential for a rotating updraft in a supercell • Higher numbers associated with a higher potential for tornadoes • Three types: • 0–1 km, 0–3 km, effective • Effective is most useful in discriminating between tornadic and nontornadic storms.
Storm-Relative Helicity (SRH) • Thresholds (in m2 s-2) • 0–1 km : 100+ • 0–3 km : 250+ • Effective : 100+
0–1 km SRH: Outbreaks 27 April 2011 24 May 2011
Hodographs Greensburg EF5 Parkersburg EF5
Energy Helicity Index (EHI) • Combination of CAPE and SRH • Two types: 0–1 km, 0–3 km • Thresholds • >2.5 : Favorable for tornadoes • Storms must develop for this to be useful • Can be skewed by high CAPE values
0–1 km EHI: Outbreaks 27 April 2011 24 May 2011
Other Parameters • LCL Heights • Lower heights (<1000 m) associated with tornadoes • Higher moisture available, keeping RFD warm • Lifted Index (LI) • Another stability index (taken at 500 mb) • The lower the number, the more unstable the atmosphere
Other Parameters • Supercell Composite • Significant Tornado Parameter • For these two, we shall play a game!
But first… MATH! Not scary Chen math, but still a nuisance.
The point of STP & SCP • These are best used to pinpoint a region that severe weather could occur on a given day. • Should never be used to make any other decisions without actually analyzing the environment.
More things to look at! • Jet Stream • Increases shear • Separates downdraft from updraft • Longer-lived storms • Low-level Jet (LLJ) • Brings in moisture and warmer temperatures, increases shear and helicity • Upper-Level Jet Streaks • Increased shear, upward motion to increase instability • Upward regions: right entrance, left exit
Upper Level Jet Streak Left Exit RightExit Left Entrance Right Entrance
More things to look at! • Frontal boundaries • Cold and warm fronts, dryline • Can enhance shear, helicity • Source of lift • Surface observations • Gives an idea of what is going on at this moment • Look for mesoscale features • Satellite Imagery • Look for clearing early, robust CU fields
More things to look at! • Water Vapor Imagery • Shows drying, moistening in the mid- and upper-levels • See where fronts/shortwaves are located
More things to look at! • Moisture • Storms won’t form without it • Td > 60°F for best environment • 700 mb temperatures • Good indicator of cap strength • < 12°C in the spring without a strong lifting mechanism • Can be slightly higher (<13°C) during summer months or with strong lift
More things to look at! • Theta-E • Measure of heat and moisture in the atmosphere • Look for theta-e advection/ridges • Increased instability, convergence • Could be area of convective development • Storm Motion • Calculated average direction and speed of storms • Gives an idea of how storms will move
Where Do We Look At This Stuff? • SPC Mesoanalysis • TwisterData • COD Analysis • AMS Model Animator • HPC • RAP Weather
How to chase safely and effectively. Storm Chasing Basics.
The Beginner’s Way • S/SE is safest place to be • Watch for right-turning • Avoid core-punching • Avoid rain-wrapped messes • Pull off on side roads, not main roads
What NOT to expect… • To see a tornado on your first time out… • or second… • or third… • Good chasers usually see a tornado about once in every seven chases. • Don’t let this deter you from chasing… • Can’t win the game if you don’t play!
What to expect… • LONG car rides • Sitting, waiting, wishing… football and frisbee! • Lots of gas station/fast food meals • Sketchy dirt roads • And in turn, few rest stops. • The beauty of the Plains • Awesome tunes! • THE TIME OF YOUR LIFE! Memories!
Tips • Wear real shoes or boots, not flip flops. • Watch the skies, not just the computer screen. • Only your eyes can tell you what’s actually happening around you. • Try to learn as much as possible, not just watch.
So we’re not held liable if you act stupid. Just kidding. But seriously. Storm Chasing Safety.
Safety Tips • CHASE WITH SOMEONE WHO HAS CHASED BEFORE. • Chase with a partner • Stay in the car as much as possible if there’s lightning nearby. • Have an escape route • Try to head south if you feel that you’re in danger. • If that’s not possible, head east until you can go south.