Weather Patterns and Severe Storms 20.1 Air Masses Air Masses • Weather patterns result from a movement of a large body of air. • Characterized by a similar temperatures and amounts of moisture at any given altitude. • Could take several days for an air mass to move across an area = constant weather Movement of Air Mass • When the air mass moves out of the region it formed in ---- it takes the temp and moisture with it. • The air mass changes as it moves as well. Classifying Air Mass • Source Region – the area that an air mass gets it characteristics properties of temp and moisture. • Polar (P) and Tropical (T) – describe temperatures • Continental (c) and Maritime (m) – where they form and moisture characteristics Weather in N. America • Majority of weather is influenced by the cP and mT air masses. – Form in Alaska/N. Canada, and the Gulf of Mexico • cP (continental polar) – uniformly cold and dry in winter, can cool and dry in summer. – Lake – effect snow = when the temp of the lake and land are extremely different causing heave and unstable air, leads to heavy snow (precipitation) • m(T) – warm, loaded with moisture, usually unstable – Responsible for most of the precipitation in the eastern US – In summers brings high temps and humidity • m(P) – originate off the coast of eastern Canada – Can bring with it heavy snow/rain (from Siberia to western coast of US) – Nor’easter = snow and cold temperatures as low pressure center passes, going counterclockwise • c(T) – least influence on the weather in NA – Hot dry air masses begin in the southwestern US and Mexico during summer – Cause extremely hot, droughtlike conditions in the Great Plains in the summer – Indian Summer – mild weather in the Great Lake region (unseasonably warm and mild) 20.2 Fronts Formation of Fronts • When two air masses meet, from a front, a boundary that separates two air masses. • Fronts are narrow, associated with precipitation, usually acts as a barrier that travels with an air mass, classified according to the temp of the advancing front. Warm Front • When warm air moves into an area formerly covered by cooler air. – Gradual slope as warm air rises it produces clouds leads to precipitation – Slow moving front – Light to moderate precipitation • Shown by red lines and semicircles on a weather map that point towards the cooler air. Cold Front • Forms when cold dense air moves into a region occupied by warmer air. – Becomes a steep slope, advance rapidly – Violent weather (heavy downpours, gusty wind) – Behind a cold front weather is dominated by a cold air mass • Shown by a blue line with triangles that point toward the warmer air mass Stationary Front • When the surface position of the front does not move – The flow of air is neither toward the cold air mass or the warm air mass – Gentle to moderate precipitation can occur • Shown by blue triangles on one side and red semicircles on the other of the front. Occluded Front • An active cold front overtakes a warm front – The cold air mass wedges the warm front upward – Complex weather (due to warm air going up) – Can make its own light precipitation • Shown on a weather map by blue triangles and red semicircles on the same side of the front line. Middle Latitude Cyclones • Main weather producers in the country – Centers of low pressure that generally travel from west to east, cause stormy weather – Move in a counterclockwise direction (toward the center of the low) – Most have a cold front – lifting causes the formation of clouds and abundant precipitation • Low pressure systems shown on a map by a “L” How do they form? 1.) Development of a front (two air masses with different temps move in opposite directions) 2.) Front takes on a wave shape 3.) Warm air moves towards Earth’s poles, cold air moves toward the equator 4.) The change in airflow near the surface is associated with a change in pressure (resulting in a counterclockwise direction) 5.) Occluded front forms – storm gets stronger 6.) When all the warm air is gone the friction of the air and the surface slows the airflow and it “dies” The Role of Airflow Aloft • More often then not, air high up in the atmosphere fuels a middle latitude cyclone. • Usually can find anticyclones and cyclones next to each other. 20.3 Severe Storms Thunderstorms • Vertical movement of warm unstable air can lead to a thunderstorm. • Generates lighting and thunder, produce gusty winds, heavy rain, and sometimes hail • Could be a single cumulonimbus cloud or a large stretch along a cold front. • Greatest number of thunderstorms occur in the tropics – due to warm, moisture rich, and unstable air • Development – when warm, humid air rises in an unstable environment (lifespan about 2hrs) – 1.) Strong upward movements of warm moist air – 2.) Mature Stage – amount and size of precipitation due to the updraft is to large to be supported (most active stage) – 3.) Dissipating Stage – when the downdrafts dominate, cooling effect of the falling precipitation causes the storm to die Tornadoes • Violent windstorms that take the form of a rotation of air called a vortex that extends downward. • Tornado Season = April through June (December and January less frequent) • Form with severe thunderstorms • Mesocyclone – important to form a tornado, a vertical cylinder of rotating air that develops in the updraft Tornado Intensity and Safety • Wind speed is measured by the Fujita Scale – winds cannot be measured directly so determined by the amount of damage done. • Tornado Watch – the possibility of a tornado (favorable conditions) • Tornado Warning – tornado has actually been see in the area or on the weather radar Hurricanes/Typhoons/Cyclones • Tropical cyclones that produce winds of at least 119 km/hr • Most powerful storm on Earth • Can bring to shore strong winds, storm surge, and flooding • A higher threat now that more people live and work near the coastline Development of a Hurricane • A heat engine that is fueled by the energy given off when huge quantities of water vapor condense • Develop most often in the late summer when water temps are warm enough to provide heat and moisture to the air • Tropical disturbance to a category 5 hurricane – Eye – wall – is formed and usually helps to sustain the hurricane (strongest wind gusts are here) Hurricane Safety • Intensity measured by the Saffir – Simpson Scale • Storm Surge – water that precedes the hurricane and sweeps onto the shore/land. • Hurricanes weaken as they move over colder water (adequate heat and moisture) or land (due to friction and lack of moisture) 21.3 Climate Change Climate Change • Climate is always changing (short-term or long-term) • Natural Process that change climate – Volcanic Eruptions – Ocean Circulation – Solar Activity – Earth Motions Volcanic Eruptions • Emits large amounts of ash and dust into the atmosphere • Aerosols in the air increase solar radiation reflected back into the space – lowering the atmosphere temperature (Volcanic winter) Ocean Circulation • El Nino is the change in ocean circulation • Short term climate fluctuations Ex.) An area that usually has a lot of rain could experience a drought during an El Nino Solar Activity • Changes in the output of the solar energy • Sunspots = warm periods in Europe and North America • Short term Effects • No long term variations due to solar activity exist (yet) Earth Motions • Most are long-term changes • Tectonic plate movement – change in position on land and ocean • Shape of orbit and tilt of the Earth on the axis – Smaller the tilt the smaller the temperature difference between summer and winter Human Impact on Climate Change • Greenhouse Effect – a natural warming of both Earth’s lower atmosphere and surface – Major gasses involved – water vapor and CO2 – Makes life possible on Earth – Human impact has increased CO2 levels in the atmosphere (burning of fossil fuels and clearing of forest) • Global Warming – a result of the increases in CO2 and other gases ---- global temperatures have increases • Sea level rising, flooding, heat waves, droughts, more water vapor in the air, temperature increase across the globe.