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Weather Thunderstorms Snow / Rain storms Mid-latitude cyclones Tropical cyclones Types of Severe Weather • Thunderstorms • Snow / Rain storms • Mid-latitude cyclones – Blizzards – Tornadoes • Tropical cyclones – Typhoons in the western Pacific – Cyclones in the Indian Ocean – Hurricanes in the U.S. Stages in the development of a thunderstorm Thunderstorms • How Lightning Works Thunderstorms Lightning Varieties cloud-to-ground Blue jets Cloud discharge Red sprites Ball lightning Elves (NOVA: Science Now – Lightning http://www.pbs.org/wgbh/nova/sciencenow/3214/02.html) Lightning Varieties Volcanic Lightning Nuclear Lightning Triggered Lightning (NOVA: Science Now – Lightning http://www.pbs.org/wgbh/nova/sciencenow/3214/02.html) Severe weather types • Tornadoes – How a Tornado Forms • Moist air from Gulf of Mexico • Fast moving cold, dry air mass from Canada • Jet stream moving east at 150 mph • Sets up shearing conditions Severe weather types • Tornadoes – How a Tornado Forms • Warm moist Gulf air releases latent heat, creates strong updraft • Updraft sheared by polar air, then twisted in a different direction by jet stream Tornado Wind Patterns Severe weather types • Tornadoes – Why do some thunderstorms spawn tornadoes while others do not? – Super Cell Thunderstorms Severe weather types • Tornadoes – The Fujita-Pearson Scale • The size of a tornado is not necessarily an indication of its intensity! Tornadoes • “Tornado Capitol of the World” – CNN’s “10 deadliest U.S. tornadoes” Source: cnn.com Tornadoes • Why don’t tornadoes strike large cities? – Occur over large regions – Cities are relatively small targets – Oklahoma City Tornado (1999) Mid-latitude Cyclones • Idealized weather – Middle-latitude cyclones move eastward across the United States • First signs of their approach are in the western sky • Require two to four days to pass over a region – Largest weather contrasts occur in the spring Mid-latitude Cyclones Mid-latitude Cyclones • Blizzards – Form when a long cyclone brings • Cold 60 km/hr winds • Freezing temperatures • Lots of snow – Can travel very slowly – Storm itself usually doesn’t kill • Shoveling snow, auto accidents, etc. Mid-latitude Cyclones • Ice Storms – Formation: • Falling snow and ice melt, change to rain, then freeze again as they reach the ground • Sleet • Freezing rain Hurricanes • Only natural disaster that is given a human name • Actually large tropical cyclones • Convert heat in the ocean into winds • Exports excess heat from the tropics to the midlatitudes Hurricanes • How a Hurricane Works – Tropical disturbance • Low pressure zone develops and draws in clusters of thunderstorms and winds Hurricanes • How a Hurricane Works – Tropical disturbance – Tropical depression • Surface winds strengthen, move about the center of the storm • Central core funnels warm moist air up towards stratosphere • Air cools, vapor condenses, latent heat released • Fuels more updrafts, cycle repeats, storm grows Hurricanes • How a Hurricane Works – Tropical disturbance – Tropical depression – Tropical Storm • Storm has sustained surface wind speeds of +39 mph Hurricanes • How a Hurricane Works – Tropical disturbance – Tropical depression – Tropical Storm – Hurricane • Surface winds consistently over 74 mph Hurricanes • How a Hurricane Works – Tropical disturbance – Tropical depression – Tropical Storm – Hurricane – The Eye • As wind speed increases, winds are spiraled upwards prior to reaching the center • A distinctive clear “eye” is formed • Strongest winds are located on the walls of the eye Hurricane Wind Patterns Hurricane Origins • Form in the tropics ~ 5° and 20 ° latitude • Cannot form at the equator (Coriolis effect = 0) Hurricanes • Hurricane Damages – Storm Surges • Large mound of water builds up beneath the eye • Reaches land as a surge of water Hurricanes • Hurricane Damages – Storm Surges • Wind speed varies depending upon which side of the hurricane you’re on • Amount of damage on the coastline will vary accordingly Hurricanes • Hurricane Damages – Heavy Rains – Mudflows and Debris Avalanches – Flooding Hurricanes • Hurricane paths – Curves due to Coriolis affect – Storms must go around high • Strong and large – storms to Atlantic seaboard • Small and to the north – storms may miss the U.S. Hurricane Paths Forecasting the Hurricane Season • Frequency of hurricanes in the North Atlantic is affected by climate – Wet Sahel region in Africa = more thunderstorms – Warm SST = more energy for tropical depressions – Low atmospheric pressure in Caribbean = more cyclones Forecasting the Hurricane Season • The La Nina / El Nino Connection – La Nina present in Pacific = more winds to move storms – El Nino present in the Pacific = less winds, disrupts storms El Niño Normal conditions in the tropical Pacific Ocean • Surface winds move from east to west • From high pressure in S. America to low pressure in Australia • Drags water westward • Warm water pools in the western Pacific Every 3 – 8 years, system reverses • Called the Southern Oscillation • Trade winds weaken or reverse • Warm water migrates from Australia to S. America • Arrives in time for Christmas – Corriente del Niño El Niño and La Niña What is El Niño? • Basically, it's a giant puddle (or pod) of heated water that sloshes across the Pacific Ocean • Similar to an iceberg – Bulge on the surface – Most of “pod” beneath the surface – Due to difference in density • National Geographic’s Model ENSO - El Niño-Southern Oscillation • Typically lasts 1 year • May last up to 3 • In multi-year events, first year not as affected • Affects both hemispheres Recognizing an El Niño • Sea Surface Temperatures (SST) • Normal: 6-8° C warmer in the western tropical Pacific than in the eastern tropical Pacific • Check SST to see if in “normal” range La Niña • Return to “normal” conditions from an El Niño • strong Produces: – Strong currents – Powerful upwelling – Chilly and stormy conditions along S. American coast • Eastern Pacific cools rapidly, Western Pacific • warms rapidly Renewed Trade Wind activity spreads the cooler eastern Pacific waters westward