Chapter 12 Air Masses and Fronts Theme of
- Slides: 112
Chapter 12 – Air Masses and Fronts
Theme of Chapter 12: Air Masses are Important! • Air mass – a large region of air (thousands of square miles) having similar temperature, pressure, and moisture characteristics
Theme of Chapter 12: Air Masses are Important! • Air mass – a large region of air (thousands of square miles) having similar temperature, pressure, and moisture characteristics • Air masses move and strongly influence the changing of the weather, making them very important to understand
Theme of Chapter 12: Air Masses are Important! • Air mass – a large region of air (thousands of square miles) having similar temperature, pressure, and moisture characteristics • Air masses move and strongly influence the changing of the weather, making them very important to understand • Fronts – boundaries between air masses
Formation of Air Masses • Air masses attain their characteristics from the part of earth’s surface over which they exist
Formation of Air Masses • Air masses attain their characteristics from the part of earth’s surface over which they exist Simple Examples - air sitting over tropical ocean becomes warm and moist - air sitting over a desert will be warm and dry
Formation of Air Masses • Source region – an area of earth where air masses form
Formation of Air Masses • Source region – an area of earth where air masses form - Source regions are very large
Formation of Air Masses • Source region – an area of earth where air masses form - Source regions are very large - Source regions occur at high and low latitudes (mid-latitudes are too variable)
Air Masses • Air masses are classified according to their temperature and moisture characteristics: 1) Based on moisture – continental (dry) or maritime (moist)
Air Masses • Air masses are classified according to their temperature and moisture characteristics: 1) Based on moisture – continental (dry) or maritime (moist) 2) Based on temperature – tropical (warm), polar (cold), or arctic (very cold)
Air Masses • There are 5 different types of air mass: 1) Continental arctic 2) Continental polar 3) Continental tropical 4) Maritime polar 5) Maritime tropical
Continental Polar Air Mass • Continental polar air masses are dry and cold
Continental Polar Air Mass • Continental polar air masses are dry and cold • Form over high-latitude land surfaces (including ice)
Continental Polar Air Mass • Continental polar air masses are dry and cold • Form over high-latitude land surfaces (including ice) • In winter, very little solar radiation causes net cooling of air mass
Continental Polar Air Mass • Continental polar air masses are dry and cold • Form over high-latitude land surfaces (including ice) • In winter, very little solar radiation causes net cooling of air mass • Extremely dry since cold air cannot contain much water vapor
Water Vapor in Cold Air
Continental Polar Air Mass • Continental polar air masses are dry and cold • Form over high-latitude land surfaces (including ice) • In winter, very little solar radiation causes net cooling of air mass • Extremely dry since cold air cannot contain much water vapor • Typically clear and cloudless
Continental Polar Air Mass • Continental polar air masses are dry and cold • Form over high-latitude land surfaces (including ice) • In winter, very little solar radiation causes net cooling of air mass • Extremely dry since cold air cannot contain much water vapor • Typically clear and cloudless • Very stable (resists vertical motion)
Pressure (mb) Continental Polar Air: Very Stable Te profile Temperature (o. C)
Continental Arctic Air Masses • Continental arctic air masses are extremely dry, extremely cold versions of continental polar air masses
Continental Arctic Air Masses • Continental arctic air masses are extremely dry, extremely cold versions of continental polar air masses • The only difference: Continental arctic air masses are shallower than continental polar air masses
Continental Arctic vs. Continental Polar Continental polar air Continental tropical air Continental arctic air
Maritime Polar Air Masses • Maritime polar air masses are moist and cool
Maritime Polar Air Masses • Maritime polar air masses are moist and cool • Form over oceans (not ice) at high latitudes
Maritime Polar Air Masses • Maritime polar air masses are moist and cool • Form over oceans (not ice) at high latitudes • Cool and moist due to contact with cold ocean water
Maritime Polar Air Masses • Maritime polar air masses are moist and cool • Form over oceans (not ice) at high latitudes • Cool and moist due to contact with cold ocean water • Generally cloudy
Continental Tropical Air Masses • Continental tropical air masses are dry and warm
Continental Tropical Air Masses • Continental tropical air masses are dry and warm • Form over low-latitude land surfaces
Continental Tropical Air Masses • Continental tropical air masses are dry and warm • Form over low-latitude land surfaces • Hot and dry due to contact with hot land surfaces with little moisture
Continental Tropical Air Masses • Continental tropical air masses are dry and warm • Form over low-latitude land surfaces • Hot and dry due to contact with hot land surfaces with little moisture • Generally cloud-free
Continental Tropical Air Masses • Continental tropical air masses are dry and warm • Form over low-latitude land surfaces • Hot and dry due to contact with hot land surfaces with little moisture • Generally cloud-free • Fairly unstable due to heating from below (but dryness inhibits cloud formation)
Maritime Tropical Air Masses • Maritime tropical air masses are
Maritime Tropical Air Masses • Maritime tropical air masses are moist and
Maritime Tropical Air Masses • Maritime tropical air masses are moist and warm
Maritime Tropical Air Masses • Maritime tropical air masses are moist and warm • Form over warm ocean (tropical) waters
Maritime Tropical Air Masses • Maritime tropical air masses are moist and warm • Form over warm ocean (tropical) waters • Unstable conditions (moist warm air at surface)
Maritime Tropical Air Masses • Maritime tropical air masses are moist and warm • Form over warm ocean (tropical) waters • Unstable conditions (moist warm air at surface) • Generally cloudy and partly cloudy
Maritime Tropical Air Masses • Maritime tropical air masses are moist and warm • Form over warm ocean (tropical) waters • Unstable conditions (moist warm air at surface) • Generally cloudy and partly cloudy • Responsible for daily showers/thunderstorms in the southeast U. S.
The Importance of Different Air Masses: The Pineapple Express • The Pineapple express – a weather phenomena that impacts the NW U. S.
The Importance of Different Air Masses: The Pineapple Express • The Pineapple express – a weather phenomena that impacts the NW U. S. • Constant flow of maritime tropical air into the NW U. S.
The Importance of Different Air Masses: The Pineapple Express • The Pineapple express – a weather phenomena that impacts the NW U. S. • Constant flow of maritime tropical air into the NW U. S. • Significant orographic (mountaininduced) rainfall
The Importance of Different Air Masses: The Pineapple Express • The Pineapple express – a weather phenomena that impacts the NW U. S. • Constant flow of maritime tropical air into the NW U. S. • Significant orographic (mountaininduced) rainfall • High freezing (and snow) levels
The Importance of Different Air Masses: The Pineapple Express • The Pineapple express – a weather phenomena that impacts the NW U. S. • Constant flow of maritime tropical air into the NW U. S. • Significant orographic (mountaininduced) rainfall • High freezing (and snow) levels • Causes destructive flooding
The Importance of Different Air Masses: The Pineapple Express
The Importance of Different Air Masses: The Pineapple Express
Summary of Air Masses
Air Mass Modification • Air masses can be modified as they move into new regions with different surface characteristics
Air Mass Modification • Air masses can be modified as they move into new regions with different surface characteristics Example: Continental polar air moves southward
Air Mass Modification
Air Mass Modification
Air Mass Modification
Fronts • Fronts – boundaries between different air masses
Fronts • Fronts – boundaries between different air masses • Cause significant changes in the weather (wind shift, temperature, moisture)
Fronts • Fronts – boundaries between different air masses • Cause significant changes in the weather (wind shift, temperature, moisture) • Usually associated with clouds, precipitation, and sometimes severe weather
Fronts • There are 4 different kinds of fronts: 1) Cold front – cold air advancing toward warm air
Fronts • There are 4 different kinds of fronts: 1) Cold front – cold air advancing toward warm air 2) Warm front – warm air advancing toward cold air
Fronts • There are 4 different kinds of fronts: 1) Cold front – cold air advancing toward warm air 2) Warm front – warm air advancing toward cold air 3) Stationary front – air mass boundary that isn’t moving
Fronts • There are 4 different kinds of fronts: 1) Cold front – cold air advancing toward warm air 2) Warm front – warm air advancing toward cold air 3) Stationary front – air mass boundary that isn’t moving 4) Occluded front – cold air advancing toward cool air
Cold Fronts • Cold fronts are at the leading edge of advancing cold air
Cold Fronts • Cold fronts are at the leading edge of advancing cold air Cold air Warm air
Cold Fronts • Cold fronts are at the leading edge of advancing cold air Cold air Warm air • A rapid decrease in temperature occurs behind the front
Cold Fronts Vital Stats • Move 0 -30 mph
Cold Fronts Vital Stats • Move 0 -30 mph • Lift the warm air into which its advancing
Cold Fronts Vital Stats • Move 0 -30 mph • Lift the warm air into which its advancing • Often produce brief, intense showers and thunderstorms
Cold Fronts Vital Stats • Move 0 -30 mph • Lift the warm air into which its advancing • Often produce brief, intense showers and thunderstorms • Often located in a pressure trough
Cold Fronts Vital Stats • Move 0 -30 mph • Lift the warm air into which its advancing • Often produce brief, intense showers and thunderstorms • Often located in a pressure trough • Usually are associated with a strong decrease in moisture as well as temperature
Cold Fronts Vital Stats • Move 0 -30 mph • Lift the warm air into which its advancing • Often produce brief, intense showers and thunderstorms • Often located in a pressure trough • Usually are associated with a strong decrease in moisture as well as temperature • 1: 100 vertical slope
Cold Fronts Vital Stats • Move 0 -30 mph • Lift the warm air into which its advancing • Often produce brief, intense showers and thunderstorms • Often located in a pressure trough • Usually are associated with a strong decrease in moisture as well as temperature • 1: 100 vertical slope • Wind shift is typically southerly to westerly
Cold Fronts
Cold Fronts
Cold Fronts
Cold Front Example Surface weather map February 17, 2008
Cold Front Example Surface weather map February 18, 2008
Cold Front Example Surface weather map February 19, 2008
Cold Front Example Surface weather map February 20, 2008
Cold Front Example Nighttime low temperatures past 24 hours February 17, 2008
Cold Front Example Nighttime low temperatures past 24 hours February 18, 2008
Cold Front Example Nighttime low temperatures past 24 hours February 19, 2008
Cold Front Example Nighttime low temperatures past 24 hours February 20, 2008
Warm Fronts • Warm fronts are at the leading edge of advancing warm air
Warm Fronts • Warm fronts are at the leading edge of advancing warm air Cold air Warm air
Warm Fronts • Warm fronts are at the leading edge of advancing warm air Cold air Warm air • A decrease in temperature occurs ahead of the front (less pronounced temperature gradient than with a cold front)
Warm Fronts Vital Stats • Move 0 -12 mph
Warm Fronts Vital Stats • Move 0 -12 mph • Warm air overruns cold air
Warm Fronts Vital Stats • Move 0 -12 mph • Warm air overruns cold air • Often produce long-lasting, steady, stratiform precipitation
Warm Fronts • • Vital Stats Move 0 -12 mph Warm air overruns cold air Often produce long-lasting, steady, stratiform precipitation Often located in a pressure trough
Warm Fronts • • • Vital Stats Move 0 -12 mph Warm air overruns cold air Often produce long-lasting, steady, stratiform precipitation Often located in a pressure trough Usually are associated with an increase in moisture as well as temperature
Warm Fronts • • • Vital Stats Move 0 -12 mph Warm air overruns cold air Often produce long-lasting, steady, stratiform precipitation Often located in a pressure trough Usually are associated with an increase in moisture as well as temperature 1: 200 vertical slope
Warm Fronts • • Vital Stats Move 0 -12 mph Warm air overruns cold air Often produce long-lasting, steady, stratiform precipitation Often located in a pressure trough Usually are associated with an increase in moisture as well as temperature 1: 200 vertical slope Wind shift is typically easterly to southerly
Warm Fronts
Warm Fronts: Vertical Structure
Warm Fronts
Stationary Fronts • Stationary fronts are located at a boundary between air masses that isn’t moving Cold air Warm air
Occluded Fronts • Occluded fronts form when a cold front catches up with a warm front (traditional explanation) Cool air Cold air • Cold air advancing toward cool air = cold-type occlusion
Occluded Fronts • Occluded fronts form when a cold front catches up with a warm front (traditional explanation) Cold air Cool air • Cool air advancing toward cold air = warm-type occlusion
Occluded Fronts: The Traditional Explanation
Occluded Fronts: The Traditional Explanation
Occluded Fronts: The Traditional Explanation
Occluded Fronts: Recent Findings • Occluded fronts form when centers of low pressure are stretched
Occluded Fronts: Recent Findings • Occluded fronts can also form when the cold front advances along the warm front, forming a “T-bone” structure
Drylines • Drylines exist at a boundary between a dry and moist air mass (without a temperature gradient)
Drylines • Drylines exist at a boundary between a dry and moist air mass (without a temperature gradient) • Advancing drylines act like cold fronts since dry air is more dense than moist air
Drylines • Drylines exist at a boundary between a dry and moist air mass (without a temperature gradient) • Advancing drylines act like cold fronts since dry air is more dense than moist air • Drylines are very common in the South Plains (due to local geography)
Drylines • Drylines exist at a boundary between a dry and moist air mass (without a temperature gradient) • Advancing drylines act like cold fronts since dry air is more dense than moist air • Drylines are very common in the South Plains (due to local geography) • Severe weather is common along drylines
Drylines • Drylines exist at a boundary between a dry and moist air mass (without a temperature gradient) • Advancing drylines act like cold fronts since dry air is more dense than moist air • Drylines are very common in the South Plains (due to local geography) • Severe weather is common along drylines • Drylines can both retreat and advance
Drylines
Drylines
Cold Front or Dryline? Cloudy Clear • Cold fronts and drylines are sometimes difficult to discern due to dirurnal effects like daytime heating/nighttime cooling
Issues Identifying Fronts/Drylines on Weather Maps • Fronts/drylines are plotted on weather maps using observations, and are sometimes hard to locate because:
Issues Identifying Fronts/Drylines on Weather Maps • Fronts/drylines are plotted on weather maps using observations, and are sometimes hard to locate because: 1) Observations are sparse
Issues Identifying Fronts/Drylines on Weather Maps • Fronts/drylines are plotted on weather maps using observations, and are sometimes hard to locate because: 1) Observations are sparse 2) Local variations in: - terrain - weather (i. e. showers)
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