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Extreme Events in Climatology. Hurricanes Thunderstorms Tornadoes Droughts Glaciations. Glaciations 1-30 kyrs. Extreme events in the atmosphere rival those in the geosphere They are much more mobile than events like earthquakes affect large geographical areas
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Extreme Events in Climatology Hurricanes Thunderstorms Tornadoes Droughts Glaciations
Extreme events in the atmosphere rival those in the geosphere They are much more mobile than events like earthquakes affect large geographical areas and have dramatic consequences on the biosphere severe storms or perturbations in “normal” patterns Can cause extreme hardship on living things Can lead to widespread alteration of other natural systems soil loss, increased soil development, weathering, flooding, landslides, erosion…
Tropical cyclones (Hurricanes or Typhoons) Occur in the tropics Are cyclones - circulation around a low pressure center Counter clockwise rotation in Northern hemisphere driven by coriolis force Require warm temperatures and adequate air motion to generate
Hurricane paths note the absence along the equator
Thunderstorm types Severe = <58 MPH wind, hail, and tornadoes Non-severe = >58 MPH wind, lightning, rain
Multicell thunderstorms- cellular Multicell thunderstorms- linear
Squall lines and Thunderstorms Squall lines are a line of severe thunderstorm cells, associated with a cold front. Direction of line movement
Tornadoes, Waterspouts, Landspouts (aka Dustdevils) All involve rotational motion Some waterspouts and landspouts can come from the ground (water) up Tornadoes and some waterspouts come from the cloud down The US leads the world in tornadoes averaging 1000 per year
Dust Devils Caused by intense heating
Droughts By definition, a deficit in the water budget for a given region Can be related to global circulation, regional circulation, or local conditions Ground dries out, soil blows away, nothing grows Example “The Dust Bowl” in the 1930’s
Glaciation Driven by Milankovitch orbital variations Eccentricity, Obliquity and Precession Facilitated by feedback loops in Earth’s atmosphere and hydrosphere oceanic and atmospheric circulation patterns change, making things colder Results in snow and ice lasting the year Lasts 10’s of thousands of years a lot of retreats and advances Last glaciation was called the Wisconsinan occurred from 60-15 kya
Glaciers, droughts, and tropical storm frequency all have identifiable effects on the natural world rivers adjust soils erode or form vegetation changes lakes form or dry up These meteorological features are extremely sensitive This makes them good things to study for identifying elements of past, present and future climate change