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Fundamentals of Physical Geography 1e Chapter 6: Air Masses and Weather Systems Petersen Sack Gabler Air Masses and Weather Systems Air Masses • Air Mass: large body of air whose temperature and moisture characteristics are similar • Source Region: m = Maritime (sea) c = Continental (land) E = Equatorial (very warm) T = Tropical (warm) P = Polar (cold) A = Arctic (very cold) Air Masses •Air Masses – Maritime Equatorial (mE) – Maritime Tropical (mT) – Continental Tropical (cT) – Continental Polar (cP) – Maritime Polar (mP) – Continental Arctic (cA) Air Masses Air Masses • Air Mass Modification and Stability – cP or cA moves over Great Lakes and picks up moisture, and may cause Lake effect snow. What two main factors contribute to increased precipitation caused by the lake effect? Air Masses • North American Air Masses – Continental Arctic (cA) – Continental Polar (cP) – Maritime Polar (mP) – Maritime Tropical (mT) – Continental Tropical (cT) Air Masses • Continental Arctic (cA): Dry and very cold – Occasionally impacts U.S. in the winter – Often produces record breaking cold • Continental Polar (cP): Dry and cold – May reach Gulf of Mexico in winter – Rarely affects west coast • Maritime Polar (mP): Moist and cool – Westerlies bring air mass to west coast, especially in winter – Occasionally affects eastern U.S. as Nor’easters Air Masses • Maritime Tropical (mT): moist and warm – May originates in Gulf of Mexico – Major impact on central and eastern U.S •T-storms in the summer •Clashes with cP • Continental Tropical (cT): dry and hot – Small source region (SW deserts and N. Mexico – Dry line – Smallest player in U.S. weather Air Masses Which air masses affect your location? Are there seasonal variations? Fronts • Fronts – Clash between air masses – Sloping boundary – Generally move with westerlies – 3-dimensional – Frontal uplift – U.S. and Canada in a zone between source regions Fronts • Cold Front: – Cold air moves in on warm air – Warm air (less dense) rises above cold air – Steep slope – Cumulonimbus – May form a Squall line – Sharp changes in temperature, pressure, and wind Cirrus anvil top Warm air mass Cumulonimbus Cold air mass Cumulus Stepped Art Fig. 6-3, p. 127 Fronts • Warm Front: – Warm air moves in on cooler air – Warm air (less dense) rises above cold air – Slope is not as steep – Light precipitation which may last longer – Usher in warmer conditions Warm air mass Cirrus Cirrostratus Altostratus Cool air mass Nimbostratus Stratus Stepped Art Fig. 6-4, p. 128 Fronts • Stationary Front – Boundary between air masses that is not moving – Extended period of light precip. and occasionally strong T-storms • Occluded Front – Cold air is overtaking warm air – Dying storm Four major frontal symbols used on weather maps Atmospheric Disturbances • Anticyclones and Cyclones – Atmospheric disturbance •Anticyclone •Cyclone •Wind and pressure gradient Where would be the strongest winds in this figure? Where would be the weakest winds? Atmospheric Disturbances • Anticyclone (H) – Move with path of westerlies – Divergence, sinking air – Sources: •Northern Canada and Arctic Polar outbreak •Subtropical High Dry and warmer weather Atmospheric Disturbances • Cyclones – Low pressure – Convergence and rising air – Clouds and precipitation Atmospheric Disturbances • Mapping pressure systems – Horizontal structure – Vertical Structure Atmospheric Disturbances • General Movement – Track of storms (mid-latitude cyclones) – What storm track influences your location? Atmospheric Disturbances • Middle-Latitude Cyclone – Also known as extratropical cyclones – Migrating storms – Clash between air masses •Ex: Cp vs. mT – Vary in intensity, longevity, speed of travel, wind strength, amount and type of cloud cover, the quantity and type of precipitation, and the area they affect. – Associated with polar front •Movement with the seasons Atmospheric Disturbances • Middle-Latitude Cyclone – Stages in the development of a mid-latitude cyclone – In (c), where would you expect rain to develop. Why? Atmospheric Disturbances • Cyclones and Local Weather Describe the front(s), temp, air mass type, wind direction, and precip. in Pittsburg and Detroit. Atmospheric Disturbances • Cyclones and the Upper Air Flow – Alternating pressure ridges (highs/divergent winds) and troughs (lows/convergent winds) Where would you expect storms to develop? Atmospheric Disturbances • Cyclones and the Upper Air Flow – Polar Jet Stream Analysis – Which country does most of this pattern occupy? Where is one trough? Atmospheric Disturbances • Hurricanes – Circular, cyclonic storm with wind speeds greater than 74 mph – Smaller than mid-latitude cyclone – Same air mass type – More destructive – Calm winds at center – Also called tropical cyclones – Require/fueled by warm water (80oF or more) Atmospheric Disturbances • Hurricane cross-section Atmospheric Disturbances • Major “Hurricane Alleys” Which coastlines seem unaffected by these tracks? Atmospheric Disturbances • Hurricane development – Warm water (>27oC or 80oF) – Most air – Coriolis force (does not form or survive near equator) • Stages of development – Tropical disturbance (easterly waves) – Tropical depression – Tropical storm (becomes named; 39-74 mph) – Hurricane (categorized by Saffir-Simpson Scale) – Dissipation (dies) over land or cool water Atmospheric Disturbances • Hurricane Intensities and Impacts – Storm surges – Saffir-Simpson Scale What can people who live in such regions do to protect themselves when a serious storm surge is threatening? Atmospheric Disturbances • Saffir-Simpson Hurricane Scale Atmospheric Disturbances • Hurricane Intensities and Impacts – 2004 was a record- breaking year • 3 in Florida – Hurricane Katrina in 2005 • New Orleans • Levee failure – Hurricane Ike in 2008 Atmospheric Disturbances • Snow storms and blizzards – Mid and high latitudes • Blizzard – Severe weather event – Heavy snow and strong winds (35 mph) – Visibility reduced Atmospheric Disturbances • Thunderstorms – Low and mid latitudes – Lightning: intense discharge of electricity – Thunder: sonic boom created by the expansion of air around the lightning bolt Atmospheric Disturbances • Types of Thunderstorms – Convective (thermal) – Orographic – Frontal Atmospheric Disturbances • Tornadoes – Occur almost anywhere but are most common in North America (Tornado Alley) – Small intense, cyclonic storm of low pressure, violent winds, and converging air Destruction caused by an F5 tornado in Greensburg, Kansas on May 16, 2007 Atmospheric Disturbances • Tornado – Typically small and short lived – 80% associated with thunderstorms – Temporal Variability •March to July •Late afternoon or early evening Atmospheric Disturbances • Doppler radar: – Improves tornado detection and forecasting – Able to determine wind speed and direction – Hook Echo is a signature of a tornado Atmospheric Disturbances • Fujita Scale (F-0 to F-5) • Enhanced Fujita Scale (EF-0 to EF-5) Weather Forecasting • Weather Forecasting – Doppler radar – Weather satellites (e.g. GOES East) – High speed computers – Improving! Is there cloud cover over your state on this day? Fundamentals of Physical Geography 1e End of Chapter 6: Air Masses and Weather Systems Petersen Sack Gabler