modern day satellite photos geostationary operational environmental satellite (goes) program...
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Modern Day Satellite PhotosGeostationary Operational Environmental
Satellite (GOES) ProgramOperated by National Weather Service (NWS)
Weather Service began as part of the War Department
September 1, 1872
http://weather.msfc.nasa.gov/GOES/goeseastconuswv.html
http://www.cdc.noaa.gov/cgi-bin/db_search/SearchMenus.pl
Cloud charts, Thermometers, Wet Bulb shoelaces, Humidity charts. pinwheels
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Density falls off with altitude; pressure is caused by impacts, dense air has more impacts
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Buoyancy Lifting
Start Local Heat Air Expands Dense AirJiggles
Underneath(heated atoms
speed uppaddle board
analogy)forces warm
air up
Atoms close together (dense, high pressure) “fall into” the empty (low pressure) area
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Pressure differences cause WIND
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Wind is caused by differences in pressureWind is caused by differences in pressure
Pressure and Density of air are two aspects Pressure and Density of air are two aspects of the same thingof the same thing
Atoms close together (in dense, high Atoms close together (in dense, high pressure areas ) “fall into” the empty (low pressure areas ) “fall into” the empty (low pressure) areapressure) area
WINDWIND
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The greater the contrast in pressure the faster the wind.One atmosphere (pressure at surface) is about 1000 millibars These red isobars are lines of equal pressure
HL
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Pressure Gradients
Coriolis turning
Initially wind flows from high to lowbut Coriolis turns it nearly parallel to lines of equal pressure (isobars)
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Winds blowing parallel to isobars are called geostrophic windsThis occurs well above the surface where there is no friction
Notice pressure gradient force always from high to low pressure, but Coriolis perpendicular to actual flow direction
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Winds blowing parallel to isobars are called geostrophic winds
Winds Aloft, maybe 3 km upWind speed feathers on the “from” end. Winds named for the “from” direction
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Friction turns surface winds back toward the pressure gradient.Near the surface, winds almost move from High to Low pressureThey spiral counterclockwise into a Low in Northern Hemisphere
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Near the surface, winds almost move from High to Low pressure
They spiral counterclockwise into a Low in Northern Hemisphere
L
L lowest local pressure
Blue arrows PGF
Red arrows Coriolis
Black arrows wind path
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Ferrel Cell
Polar Cell
Hadley Cell
Since earth’s rotation turns air, flows are broken into 3 cells per hemisphere
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Horizontal temperature differences
Temperature effects density and pressure:
500 mb
700 mb
850 mb
Warm Cold Psurface
If you heat something it expands and gets less denseA 500 millibar pressure level is much higher in hot air. Hotter air has lower density and greater volume
1000 mb
P = R’ T so T = P /R’
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Polar Jet FormationPolar Jet Formation
Steep gradients of Steep gradients of Pressure cause Pressure cause higher velocity higher velocity geostrophic geostrophic winds.winds.
This is the trigger This is the trigger for jet stream for jet stream flow.flow.
LOW _____________________HIGH
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For the Polar Jet, the eddy is in the Ferrel cell on the upper polar side, and so air flows from the west to the east, the “Westerlies”
Since the pressure difference is great at the boundary, the jet is a very fast wind
Polar air is denser, so it wedges under the low density warm air. Rotation causes an eddy to form
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Air MassesAir Masses
An air mass develops when the atmosphere An air mass develops when the atmosphere is located above a relatively uniform land or is located above a relatively uniform land or water surface for several days. water surface for several days.
The lower atmosphere assimilates some of The lower atmosphere assimilates some of the properties of the underlying surface.the properties of the underlying surface.
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Air MassesAir Masses
Large regions (1,000s kmLarge regions (1,000s km22) of the lower ) of the lower troposphere with uniform characteristics troposphere with uniform characteristics (temperature, moisture content) originally (temperature, moisture content) originally defined by a source area.defined by a source area.
Labels refer to temperature (arctic vs. Labels refer to temperature (arctic vs. polar vs. tropical) and source area polar vs. tropical) and source area (continental vs. maritime). The source (continental vs. maritime). The source area determines the moisture content.area determines the moisture content.
Labels around here: cT cP mT mPLabels around here: cT cP mT mP
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http://www.met.tamu.edu/class/Metr304/Dir-surface/surface.html~
Polar air enlarges and moves further south during Polar air enlarges and moves further south during winter and retreats northward during summerwinter and retreats northward during summer..
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Heating (cP air moving south) will lead to instability (bouyancy) as warms.
Cooling (mT air movingnorth) has the opposite effect, because colder air cannot rise
Orographic Lifting forces maritime mP and mT air upward over mountain ranges in the western U.S., leading to condensation and precipitation that converts the formerly humid air to a much dryer air mass.
Typical Air Mass Changes
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Air Mass Interactions
• Weather in any region is influenced by the interactions between air masses. Recall that the boundaries between contrasting air masses are called FRONTS
cP
mT
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cPmT
Heavy rains can result from the interaction between the continental polar cP air mass and the maritime
tropical mT air mass
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ExtraTropical Cyclones are up to ExtraTropical Cyclones are up to 2,000 km across & 2,000 km across & control the weather control the weather for three days to a week.for three days to a week.
Winds circulate counter-clockwise (CCW) Winds circulate counter-clockwise (CCW) around the Low in Northern Hemis.around the Low in Northern Hemis.
Mid-latitude Cyclones
L
Def: Synoptic Scale: space and timescales of
mid-latitude depressions i.e. several thousand kilometers and
timescales of several days
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0. Maximumheat from
Sun
7. Mid-Latitude Cyclones are dominant where Ferrel meets Polar
1. ITCZLOW
HIGH
LOW
HIGH
2.
3. to E
4. Ferrel CellMid-Latitude Cyclones northDry south
5. 6. Gyre
8. Cold air sinks
Polar Cell
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Dishpan Experiment
Camera rotates with dishCold Center hot edgeLarge scale waves and eddies formThey flow CW & CCW
Rossby Waves
Why are the boundaries between cold and hot not straight?Cold mass is denser and forces its way under the warmer mass
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Mid-Latitude Cyclones
This clash between cP and mT air masses is the most common source of frontal systems in the U.S.
Weather conditions, and cloud types, change in a predictable sequence as warm and cold fronts pass over an area.
A front is a transition from one air mass air mass to another
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http://www.met.tamu.edu/class/Metr304/Dir-surface/surface.html~
cP mT
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DBZ is Decibels received back
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cP
mT
Map Symbols These show surface positions
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Warm Front• Ahead of a warm front, warm, humid air is
transported upward over a distance of approximately 1,000 km (625 miles).
• Rain may last longer than for a cold front because the warm front moves slowly and extends over a larger area.
Dangerous storms if cold air is very cold
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Warm Front Clouds and Winds• First sign of warm front is sequence of clouds
(cirrus, cirrostratus, altostratus). • If winds are right, up to 12 hours after the cirrus,
the higher clouds will be replaced by lower nimbostratus with associated light to moderate precipitation.
• Temperatures and humidity rise and winds typically shift direction (first from the south or southeast, then from the southwest) with the passage of the warm front.
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Warm Front Changes
Expect increasing Temperature and Humidity as the warm front passes
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Cold Frontchanges
Cold, dense continental polar air cP replaces moist, warm maritime tropical air mT across a cold front
Expect decreasing temperature and humidity and increasing atmospheric pressure with the passage of the cold front.
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Warm Air Rises
Warm wet air has lowest density, so it will always rise over cooler air.
Both the cold and warm fronts are inclined toward the warm air mass.
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Warm air is pushed up and over the advancing cold front, causingrelatively rapid cooling and condensation that results in thedevelopment of tall cumulonimbus clouds. They host heavy butrelatively short-lived precipitation
Approaching Cold Frontis behind Thunderstorms
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Cold Front cloud bands are narrowbecause cold front wedges are steep
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http://www.emc.ncep.noaa.gov/mmb/gmanikin/nas125/tstorm/squall1.gif
Cold Fronts are narrowCold Fronts are narrowbecause the edge of the because the edge of the cold air mass is steepcold air mass is steep
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A Cold Front Squall Line
Rapidly advancing cold fronts may be marked by the growth of a squall line of thunderclouds
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Cyclogenesis 1 – Stationary Front A small scale wave forms
mT
cP
Mid-Latitude Cyclones start as Stationary Fronts.
These persist if the air masses have equal pressureThen many small waves form, and storms are very frequent
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Cyclogenesis 2 – Warm and Cold Fronts
cP
mTIn the Ferrell cell, winds have a strong westerly component, and storms move East.As they mature and move, Warm Fronts pass over, followed by Cold Fronts.
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Cyclogenesis 3 – Occluded Front forms
Cold front catches warm, forcing warm air aloft. Broad precipitation area results.
cP
mT
Where the cold front catches up, they are called Occluded Fronts. Note symbol.
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Occluded Fronts• The cold front is faster than a warm front and will
eventually close the gap between the fronts, forcing the intervening warm air upward generating additional rain
Nimbostratus
cP
mT
Rain then covers a wide area
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Storm evolution
1. Surface map, so winds crossIsobars and spiral into the LOW
2. Wide precipitation bandmT
cP cPmT
Along the occluded front warm moist air is force aloft, resulting in a broad band of rain
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Thunderstorms
Thunderstorms form where warm, humid air is forced upward to altitudes of up to 15 km (20 for supercells).
Condensation occurs as the air cools, releasing latent heat and ensuring that the rising air remains unstable (warmer so less dense than surrounding air).
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Rising Warm air overshoots into stratosphere
Prevailing Wind Aloft
Freezing Line
CondensationLine
Surface
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All downdraftsDroplets coalesce
15 minutesOnly updrafts.
No rain.
Rain and Ice too heavy for updrafts Lasts 15 to 30 minutes
Rain, plus gusty winds caused by downdrafts
Type 1: Isolated Thunderstorms from unstable (hot, moist, low density) air
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Lightning
• Most dangerous frequently encountered weather hazard that people commonly experience each year.
• Second most frequent weather killer in the United States with nearly 100 deaths and 500 injuries each year,
after floods and flash floods
http://www.nssl.noaa.gov
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+ marks concentrations
of rising and falling ice
Ice often positive
Lightning equalizes large charge differences between storm levels and the ground
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2. Synoptically Forced Thunderstorms
Most of the cloud formation associated with a cold front is actually in the warm moist air mass
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Supercells Severe thunderstorms, or supercells, are
associated with frontal lifting along the cold front between the continental polar and maritime tropical air masses in mid-latitude cyclones. The lower portion of these storms, the mesocyclone, rotates. They often contain severe hail and sometimes tornadoes.
Most common during spring and early
summer, when the contrast in temperatures and moisture between air masses is greatest.
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Tropopause
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Tropopause
2. Strong updrafts pull in more air from below.
3. The strong updrafts lift falling ice and it gets covered with another layer of ice. If this happens enough times, large hailstones are the result.
Hail Formation
1. Condensation heats the moist air, which accelerates upwards
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Supercell Hail
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Tornadoes Funnel clouds that rotate at speeds
of up to 500 km/hr beneath supercells.
Ranked from F0 (weakest) to F5 (strongest) using the Fujita Intensity scale.
Most move to the east or northeast at an average speed of approximately 50 km/hr.
Develop in association with mesocyclones
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Wind Shear (different wind directions at different altitudes)causes rolling
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Updrafts can pick up the roll
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Jet Stream winds result from large pressure gradients at the boundary between mT and cP air, where a large difference in Tropopause height exists.
N
The jet stream and tornadoes: pressure differences in the extreme
The Jet Stream
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A strong tornado often is associated with rapid
removal of updraft air by the Jet Stream aloft
Tornados are narrow areas of extremely
fast updrafts
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The Dry LineThe Dry LinecT
cP
mT
Tornado Conditions
Jet Stream Aloft
Potential for wind shear with hot dry unstable cTSimilar temp but different density than mT which is moist and therefore “light”
Dry, so dense
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Multiple vortices in an F5
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May 3, 1999
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Stecker
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Supercell tops overshoot into stratosphere
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A Stecker, Oklahoma Home
http://www.nssl.noaa.gov/teams/swat/Cases/990503/A_images/stecker.gif
“Only” F3
May 4th, 1999
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A Perfect Hook
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Hurricanes &Typhoons (Tropical Cyclones)
When extremely hot ocean surface temperatures (>26oC) cause hot, moist surface air, huge clusters of thunderstorms develop at sea. If uplift gets extreme, these can organize into a gigantic Low with spiral storm lines, and winds exceeding 74 mph, a Tropical Cyclone, aka Hurricane
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Hurricanes are fueled by Latent Heat of Condensation release.One day equals the energy production of US for a year
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Jeanne
Hurricanes need hot Hurricanes need hot moist air as fuel. This moist air as fuel. This
is why they weaken is why they weaken over landover land
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Katrina
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Storm Surge
Trapped in House, swept away
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Storm Surge
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Freshwater (rain) floods cause most
fatalities
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