Скачать презентацию The atmosphere is very thin The Atmosphere rrier Скачать презентацию The atmosphere is very thin The Atmosphere rrier

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The atmosphere is very thin The Atmosphere rrier! se ba opopau Tr Earth radius The atmosphere is very thin The Atmosphere rrier! se ba opopau Tr Earth radius 6, 370 km (3, 981 miles) The atmosphere extends upward to 500 km (321 miles), HOWEVER, 99% of all atmosphere gasses are below 32 km (20 miles) Therefore Although the entire atmosphere = 8% of earth’s solid radius 99% of gasses 0. 005 = 0. 5% (one half of one percent) of earth’s radius Cloud charts, radiosonde. instruments Troposphere

For Wet Air add water vapor (up to 7% in moist hot tropics) 4% For Wet Air add water vapor (up to 7% in moist hot tropics) 4% is more typical around here. Dry Air Two common gasses, N 2 (78%) and O 2 (21%), make up 99% of dry air. Other gasses, e. g. CO 2 CH 4 NO 2 and water vapor H 2 O also play an important role by keeping the atmosphere warm, the “greenhouse effect”.

Solar Heating • The equator receives 2. 5 times more sunlight (insolation [photons / Solar Heating • The equator receives 2. 5 times more sunlight (insolation [photons / m 2 ]), incoming solar radiation, than the poles. • Highest average annual ocean surface temperatures (~27 o. C) at equator • Lowest 0 o. C at high latitudes • Diff. drives density/pressure Differences => wind DEMO flashlight and globe 23. 5

P = r. RT Density falls off with altitude; pressure is caused by impacts, P = r. RT Density falls off with altitude; pressure is caused by impacts, dense air has more impacts

Pressure differences cause WIND Winds flowing into low pressure = low density areas are Pressure differences cause WIND Winds flowing into low pressure = low density areas are said to Flow in response to the Pressure Gradient Force.

Heat vs. Temperature • Atoms in air are in constant motion, the energy of Heat vs. Temperature • Atoms in air are in constant motion, the energy of their motion is known as kinetic energy. Kinetic energy increases as the speed of atomic motion increases. Ek = 1/2 mv 2 (identify symbols) • Heat energy is the total kinetic energy of all the atoms in a substance. The more atoms present, the greater the heat. • Temperature represents the average kinetic energy of the atoms in a substance. A few atoms with rapid motion will have a higher temperature than many atoms with slow motion.

1. Atmosphere Layers w/ Pauses 3. Tropopause higher at equator 2. Pressure the weight 1. Atmosphere Layers w/ Pauses 3. Tropopause higher at equator 2. Pressure the weight of air above Ozone layer equator poles 4. 75% of gasses In Troposphere 6. Note change of sign of lapse rate at Tropopause (next slide) 5. lapse rate 6. 5 o. C/km

Coriolis Effect Air masses at rest above the equator are moving much faster than Coriolis Effect Air masses at rest above the equator are moving much faster than air masses at rest over us in NJ. Both must rotate once per day, but the equatorial air goes much further.

Equatorial Air has faster spin it still has it , so it is As Equatorial Air has faster spin it still has it , so it is As it moves toward poles faster than land below Coriolis Effect: Flowing winds appear to turn due to earth’s rotation Coriolis Effect Air in Northern Hemisphere deflects to the right, reverse in Southern H. DEMO: Coriolis Clip

Earth’s rotation appears to turn winds flowing along a pressure gradient Winds blowing parallel Earth’s rotation appears to turn winds flowing along a pressure gradient Winds blowing parallel to isobars are called geostrophic winds This 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

Coriolis “turns” them LOW HIGH Polar Cell Ferrel Cell Hadley Cell LOW The major Coriolis “turns” them LOW HIGH Polar Cell Ferrel Cell Hadley Cell LOW The major wind cells If Earth did not rotate, there would be one cell in each hemisphere. Note the formation of Ocean Current Gyres

Horizontal temperature differences Temperature effects density and pressure: P = r R’ T so Horizontal temperature differences Temperature effects density and pressure: P = r R’ T so T = P /r R’ If you heat something it expands and gets less dense A 500 millibar pressure level is much higher in hot air. Hotter air has lower density and greater volume 500 mb 700 mb 850 mb Warm 1000 mb Cold Psurface

Polar Jet Formation Steep gradients of Pressure cause higher velocity geostrophic winds. This is Polar Jet Formation Steep gradients of Pressure cause higher velocity geostrophic winds. This is the trigger for jet stream flow.

More polar air is denser, so it wedges under the low density warm air. More polar air is denser, so it wedges under the low density warm air. Rotation causes an eddy to form 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

Subtropical Deserts +/- 30 o latitude Highs where Hadley/Ferrel Cells descend Subtropical Deserts +/- 30 o latitude Highs where Hadley/Ferrel Cells descend

“water vapor” Water only compound in three states (liquid, gas, solid) on Earth’s surface. “water vapor” Water only compound in three states (liquid, gas, solid) on Earth’s surface. Heat energy is transferred through the atmosphere as water changes from one state to another. The atmosphere’s heat is absorbed by water in processes such as melting, sublimation, and evaporation. Evaporation puts moisture (water vapor Condensation releases heat to air & gas) into the atmosphere and cools the air forms cloud droplets “ “ These two transfer the most energy, are less common, don’t cause

Lifting a moist air mass results in condensation, liquid droplets are clouds, coalescence yields Lifting a moist air mass results in condensation, liquid droplets are clouds, coalescence yields precipitation Figure 1 -4 b

Orographic Lifting Windward Rain Forest Leeward Rain-Shadow Desert Rain also on the high Leeward Orographic Lifting Windward Rain Forest Leeward Rain-Shadow Desert Rain also on the high Leeward drainage sometimes Flash floods on dry plateau

Ocean-Current Desert Ocean-Current Desert

Also Interior and Polar Deserts Also Interior and Polar Deserts

Frontal Lifting • Frontal lifting occurs when two large air masses of contrasting density Frontal Lifting • Frontal lifting occurs when two large air masses of contrasting density (temperature, moisture content) meet. • The boundary between the air masses is termed a front and may be 10 to 150 km (6 -94 miles) across and hundreds of kilometers in length.

http: //www. met. tamu. edu/cl ass/Metr 304/Dirsurface/surface. html~ c. P m. T http: //www. met. tamu. edu/cl ass/Metr 304/Dirsurface/surface. html~ c. P m. T

AT THE SURFACE Friction turns surface winds back toward the pressure gradient. Near the AT THE SURFACE Friction turns surface winds back toward the pressure gradient. Near the surface, winds almost move from High to Low pressure They spiral counterclockwise into a Low in Northern Hemisphere

Buoyancy Lifting (heated atoms speed up paddle board analogy) Start area density floor Local Buoyancy Lifting (heated atoms speed up paddle board analogy) Start area density floor Local Heat Hot Air Expands Dense air falls into low density hot molecules bounce off the high Atoms close together (dense, high pressure) “fall into” the nearly empty (low pressure) ar bounce up

Define Lapse Rate Figure 1 -4 a Define Lapse Rate Figure 1 -4 a

Latent Heat of Condensation Figure 1 -3 c Latent Heat of Condensation Figure 1 -3 c

Hurricanes Table 1 -3 Hurricanes Table 1 -3

Hurricanes &Typhoons (Tropical Cyclones) When extremely hot ocean surface temperatures (>26 o. C) cause Hurricanes &Typhoons (Tropical Cyclones) When extremely hot ocean surface temperatures (>26 o. C) 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

Hurricanes are fueled by Latent Heat of Condensation release. One day equals the energy Hurricanes are fueled by Latent Heat of Condensation release. One day equals the energy production of US for a year

Jeanne Hurricanes need hot moist air as fuel. This is why they weaken over Jeanne Hurricanes need hot moist air as fuel. This is why they weaken over land

Trapped in House, swept away Storm Surge Trapped in House, swept away Storm Surge

Storm Surge Storm Surge

Freshwater (rain) floods cause most fatalities Freshwater (rain) floods cause most fatalities