ATMOSPHERE AND WEATHER AP Environmental Science Mark Ewoldsen, Ph.D. Dr. E

ORIGIN OF MODERN ATMOSPHERE original atmosphere surrounded the homogenous planet Earth and probably was composed of H and He second atmosphere evolved from gases from molten Earth H 2 O, CO 2, SO 2, CO, S 2, Cl 2, N 2, H 2, NH 3, and CH 4 allowed formation of oceans and earliest life modern Atmosphere evolved after Cyanobacteria started photosynthesizing oxygen produced did not reach modern levels until about 400 million years ago

DRIFTING CONTINENTS About 230 million years ago, all the Earth’s landmasses were joined in one super continent, Pangaea. As the continents moved toward their present-day locations, the sea level dropped, volcanoes erupted, and much of the Earth’s surface was pushed upward. The combined effect was a drop in temperature and precipitation all over the Earth. These changes were gradual.

EXTINCTION OF THE DINOSAURS The climate change caused by the drifting of the continents may have resulted in the extinction of the dinosaur. Many types of plants also became extinct. Dinosaurs that depended on these plants died. Meat-eating dinosaurs that depended on plant- eating dinosaurs died. Other scientists believe that dinosaurs became extinct as the result of a giant asteroid striking the Earth 65 million years ago. The climate change caused by the drifting of the continents may have resulted in the extinction of the dinosaur. Many types of plants also became extinct. Dinosaurs that depended on these plants died. Meat-eating dinosaurs that depended on plant- eating dinosaurs died. Other scientists believe that dinosaurs became extinct as the result of a giant asteroid striking the Earth 65 million years ago.

EARTH’S ATMOSPHERE Compared to the size of the Earth (10 4 km), the atmosphere is a thin shell (120 km). If the Earth was an orange, the atmosphere would be the pesticides on its peel

ATMOSPHERE LAYERS Exosphere Thermosphere (Ionosphere) Mesosphere Stratosphere Troposphere

STRATOSPHERE extends to 50 kilometers (31 miles) high dry and less dense temperature in this region increases gradually to -3 degrees Celsius, due to the absorption of ultraviolet radiation ozone layer absorbs and scatters the solar ultraviolet radiation ninety-nine percent of "air" is located in first two layers every 1000-m 11% less air pressure

TROPOSPHERE 8 to 14.5 kilometers high (5 to 9 miles) most dense the temperature drops from about 17 to -52 degrees Celsius almost all weather is in this region

COMPOSITION Nitrogen (N 2, 78%) Nitrogen Oxygen (O 2, 21%) Oxygen Argon (Ar, 1%) myriad of other very influential components are also present which include the Water (H 2 O, 0 - 7%), "greenhouse" gases or Ozone (O 3, %), Carbon Dioxide (CO 2, %),WaterOzone Carbon Dioxide

REVIEW QUESTIONS What gas was originally not in the atmosphere? A. Carbon dioxide B. Water C. Oxygen D. Methane

REVIEW QUESTIONS The gas that composes 78% of the gases in the atmosphere is: A. Oxygen B. Nitrogen C. Carbon Dioxide D. Ozone

REVIEW QUESTIONS The atmosphere layer in which most of the weather occurs is the: A. Troposphere B. Stratosphere C. Mesosphere D. Thermosphere E. Exosphere

SEASONAL CHANGES Occur because the earth’s axis is tilted Creates opposite seasons in the northern and southern hemisphere Factor that determines global air circulation patterns

SEASONS Seasons are short periods of climatic change. Seasons are short periods of climatic change. Because the Earth is tilted, certain areas of Earth receive changing amounts of radiation throughout the year. Because the Earth is tilted, certain areas of Earth receive changing amounts of radiation throughout the year.

Earth’s Seasons North Pole Earth When the north pole tilts toward the sun, it gets more radiation – more warmth during the summer SUMMER (Northern Hemisphere) South Pole WINTER (Southern Hemisphere) When the north pole tilts toward the sun, the south pole tilts away So when it’s summer in the north, it’s winter in the south Equator

Tilt of the Earth’s axis towards or away from the sun creates the seasons Earth’s Seasons Continued…. When the north pole tilts away from the sun, it gets less radiation – So it’s colder during the winter Earth WINTER (Northern Hemisphere) SUMMER (Southern Hemisphere) When the north pole tilts away from the sun, the south pole tilts toward it… When it’s winter in the north, it’s summer in the south North Pole South Pole Equator

OCEAN CURRENTS Sea-surface temperature influences air temperature as the ocean exchanges heat with the overlying atmosphere. Evaporation rates are generally higher where sea- surface temperature is higher

OCEAN CURRENTS OCEAN CURRENTS There are two type of Ocean Currents: 1. Surface Currents -- Surface Circulation These waters make up about 10% of all the water in the ocean. These waters are the upper 400 meters of the ocean.

OCEAN CURRENTS 2. Deep Water Currents These waters make up the other 90% of the ocean These waters move around the ocean basins by density driven forces and gravity. These deep waters sink into the deep ocean basins at high latitudes where the temperatures are cold enough to cause the density to increase.

OCEAN CURRENTS Ocean Currents are influenced by two types of forces 1. Primary Forces--start the water moving 1. Solar Heating 2. Winds 3. Gravity 4. Coriolis 2. Secondary Forces--influence where the currents flow

Ocean evaporation is higher where… A. Ocean temperature is lower B. Ocean temperature is higher C. It is the same amount everywhere

These forces start the water moving: A. Primary forces B. Secondary forces C. Tertiary forces

These forces influence where the currents flow: A. Primary forces B. Secondary forces C. Tertiary forces

Deep water Currents make up what percent of the ocean water? (A) 75% (B) 50% (C) 90% (D) 10%

LATITUDE Latitude is the measure of the distance north and south of the equator. Latitude is the measure of the distance north and south of the equator. Measured in degrees. Measured in degrees. Areas close to the equator, or 0 degrees latitude, receive the direct rays of the sun. These direct rays provide the most radiant energy. Areas close to the equator, or 0 degrees latitude, receive the direct rays of the sun. These direct rays provide the most radiant energy. Areas near the equator are warm. Areas near the equator are warm. Polar regions are cold. Polar regions are cold.

HIGH LATITUDES During the year, the high latitudes near the poles have great differences in temperature and daylight hours.

Review Question As latitude ________, the average annual temperature _________. 0° Latitude 90° Temperature A.increases; decreases B.decreases; increases

AIR TEMPERATURE As solar energy reaches the Earth, equatorial regions heat up more than the poles. As solar energy reaches the Earth, equatorial regions heat up more than the poles. Warm air and water at the equator travel poleward while cold air and water at the poles travel equatorward in an attempt to equalize this temperature contrast. Warm air and water at the equator travel poleward while cold air and water at the poles travel equatorward in an attempt to equalize this temperature contrast. It is the atmosphere's continual struggle for temperature balance that brings us our changing weather. It is the atmosphere's continual struggle for temperature balance that brings us our changing weather.

AIR PRESSURE air pressure is caused by the weight of the air pressing down on the Earth, the ocean and on the air below air pressure is caused by the weight of the air pressing down on the Earth, the ocean and on the air below the pressure depends on the amount of air above the measuring point and falls as you go higher the pressure depends on the amount of air above the measuring point and falls as you go higher air pressure changes with weather air pressure changes with weather

… AND WEATHER air in a high pressure area compresses and warms as it descends air in a high pressure area compresses and warms as it descends the warming inhibits the formation of clouds, meaning the sky is normally sunny in high-pressure areas the warming inhibits the formation of clouds, meaning the sky is normally sunny in high-pressure areas haze and fog might form haze and fog might form the opposite occurs in an area of low pressure the opposite occurs in an area of low pressure

You would most likely find clouds and rain in an area of: A. High Pressure B. Low Pressure

As you go higher in the atmosphere, air pressure ___ A. Rises B. Falls C. Stays the same

HUMIDITY relative humidity is the amount of water vapor in the air compared with the potential amount at the air's current temperature relative humidity is the amount of water vapor in the air compared with the potential amount at the air's current temperature expressed as a percentage expressed as a percentage depends on air temperature, air pressure, and water availability depends on air temperature, air pressure, and water availability the Earth has about 326 million cubic miles of water the Earth has about 326 million cubic miles of water only about 3,100 cubic miles of this water is in the air as water vapor > clouds > precipitation only about 3,100 cubic miles of this water is in the air as water vapor > clouds > precipitation

CLOUD COVER 40% moisture in the atmosphere forms clouds which cover an average of 40% of the Earth at any given time a cloudless Earth would absorb nearly 20 percent more heat from the sun clouds cool the planet by reflecting sunlight back into space. This is known as Albedo However clouds reduce the amount of heat that radiates into space by absorbing the heat radiating from the surface and reradiating some of it back down the process traps heat like a blanket “Cloud cloudlg.htmwww.nasm.si.edu/earthtoday/ cloudlg.htm -Dec :52:11 EST

PRECIPITATION Air containing water vapor cools in atmosphere and therefore condenses to form droplets of liquid water Rain : liquid, falls, d >0.5 mm (sphere) Freezing Rain : occurs when drop touches frozen surface Sleet : ice pellets, d < 0,5 mm, begins as rain but enters air below freezing Snow : water deposits in hexagonal nuclei below freezing Snow Pellets : grains of ice, d = 2-5 mm Hail : mm in diameter, concentric rings of ice

OTHER FACTORS THAT EFFECT PRECIPITATION: -Prevailing winds -Mountain ranges

REVIEW QUESTIONS Humidity depends on: Humidity depends on: A. air temperature B. air pressure C. water availability D. All of the above

WINDS horizontal wind moves from areas of high to low pressure horizontal wind moves from areas of high to low pressure vertical wind moves from low to high pressure vertical wind moves from low to high pressure speed is determined by differences in pressure speed is determined by differences in pressure Coriolis effect causes winds to spiral from high pressure zones and into low pressure zones Coriolis effect causes winds to spiral from high pressure zones and into low pressure zones Spring98/feature_story.htm

WINDS wind speed is detected by an anemometer direction is detected by a weather vane wind direction is based on where the wind is coming from: wind from the east is an easterly Beaufort Wind Speed Scale is has a range from 0 for calm to 12 for a hurricane with waves greater than 37 feet transcripts/1999/07/07.htm

FRONTS Warm Front separates warm air from the cooler air it moves into (6 mph, NE) separates warm air from the cooler air it moves into (6 mph, NE) rises over cool air masses rises over cool air masses develops clouds and light precipitation develops clouds and light precipitation

FRONTS Cold Front cold air advancing into warm (9 to 30 mph, SE) cold air advancing into warm (9 to 30 mph, SE) pushes under warm air – rising air just ahead of front pushes under warm air – rising air just ahead of front vertical movement strong and thus thunderstorms vertical movement strong and thus thunderstorms

SEVERE WEATHER - THUNDERSTORMS occur from equator to Alaska occur from equator to Alaska may have hail, strong winds, lightning, thunder, rain & tornadoes may have hail, strong winds, lightning, thunder, rain & tornadoes moist air rises due to frontal zone lifting causing loss of heat leading to cumulus clouds with updrafts moist air rises due to frontal zone lifting causing loss of heat leading to cumulus clouds with updrafts at 42,000 feet downdrafts and precipitation start at 42,000 feet downdrafts and precipitation start may last an hour may last an hour severe thunderstorms occur when cold front approaches warm front (which supplies moisture and energy) severe thunderstorms occur when cold front approaches warm front (which supplies moisture and energy) winds over 60 mph winds over 60 mph hail > 3/4 inch hail > 3/4 inch

Direction is detected by a(n) ______, wind speed is detected by a(n) _______ A. weather vane; anemometer B. anemometer; weather vane

A warm front: A. rises over cool air masses B. pushes under warm air

Which is not apart of a warm air front? (A) cold air advancing into warm (9 to 30 mph, SE) (B) develops clouds and light precipitation (C) separates warm air from the cooler air it moves into (6 mph, NE) (D) rises over cool air masses

SEVERE WEATHER - TORNADOES swirling masses of air with speeds of 300 mph+ swirling masses of air with speeds of 300 mph+ waterspouts occur over water waterspouts occur over water center of tornado is extreme low pressure which causes buildings to implode center of tornado is extreme low pressure which causes buildings to implode destruction is usually less than 0.5 miles wide and 15 miles long destruction is usually less than 0.5 miles wide and 15 miles long tornado alley is from Texas to Indiana (usually trailer homes) tornado alley is from Texas to Indiana (usually trailer homes) Wizard of Oz! Wizard of Oz!

SEVERE WEATHER - HURRICANES cause most property damage and loss of life cause most property damage and loss of life winds speeds greater that 74 mph at the center winds speeds greater that 74 mph at the center begin over warm oceans of the tropics begin over warm oceans of the tropics solar insolation (water >80 o F) provides energy for huge evaporation, cloud formation, and atmospheric lifting solar insolation (water >80 o F) provides energy for huge evaporation, cloud formation, and atmospheric lifting Thorpe, Gary S., M.S., (2002). Barron’s How to prepare for the AP Environmental Science Advanced Placement Exam

SEVERE WEATHER - HURRICANES stages stages separate thunderstorms over tropical ocean separate thunderstorms over tropical ocean cyclonic circulation which causes them to pick up more more moisture and heat energy from ocean cyclonic circulation which causes them to pick up more more moisture and heat energy from ocean winds speeds of 23 to 40 mph lead to Tropical Depression winds speeds of 23 to 40 mph lead to Tropical Depression Tropical Storms have lower pressure and higher wind speeds (40-75) Tropical Storms have lower pressure and higher wind speeds (40-75) center is called the eye center is called the eye rainfall may exceed 24 inches in 24 hours rainfall may exceed 24 inches in 24 hours

REVIEW QUESTIONS cyclonic circulation which causes them to pick up more more moisture and heat energy from ocean 1. cyclonic circulation which causes them to pick up more more moisture and heat energy from ocean 2. swirling masses of air with speeds of 300 mph+ 2. swirling masses of air with speeds of 300 mph+ 3. moist air rises due to frontal zone lifting causing loss of heat leading to cumulus clouds with updrafts 3. moist air rises due to frontal zone lifting causing loss of heat leading to cumulus clouds with updrafts A. Thunderstorms B. Tornados C. Hurricanes

THE EL-NIÑO SOUTHERN OSCILLATION (ENSO) Occurs every few years ENSO’s occur when the prevailing westerly winds weaken or cease and surface waters along the South and North American Coasts become warmer Upwellings of cold nutrient rich waters are suppressed Leads to declines in fish populations

ENSO events result from weakening of tropical Pacific atmospheric and oceanic circulation Climatic connections carry these climate effects throughout the globe (e.g., El Niño creates warm winters in AK and lots of rain in California) 2.19

LA NINA The opposite of el Nino is La Nina. The opposite of el Nino is La Nina. During La Nina, the winds blowing across the Pacific are stronger than normal and warm water accumulates in the western Pacific. The water near Peru is colder. During La Nina, the winds blowing across the Pacific are stronger than normal and warm water accumulates in the western Pacific. The water near Peru is colder. This causes droughts in the southern United states and excess rainfall in the northwestern Untied States. This causes droughts in the southern United states and excess rainfall in the northwestern Untied States.

REVIEW QUESTION What causes droughts in the southern United states and excess rainfall in the northwestern Untied States? What causes droughts in the southern United states and excess rainfall in the northwestern Untied States? A. La Nina A. La Nina B. El Nino B. El Nino During which do westerly winds weaken or cease and surface waters along the South and North American Coasts become warmer? -A. La Nina -B. El nino

CLIMATE Definitions: Average long term weather of an area Seasonal variations and weather extremes averaged over a long period (at least 30 years) 2 Main factors Temperature Precipitation amount distribution

CLIMATE CONTINUED… Factors that effect temperature: Latitude Elevation Closeness to large bodies of water

ELEVATION

Closeness to Large Bodies of Water Water moderates the temperature creating cooler summers and warmer winters

SHORT TERM CHANGES IN CLIMATE Some short-term changes may be the result of changes in ocean currents and global winds. Some short-term changes may be the result of changes in ocean currents and global winds. Ocean currents help transfer heat to the atmosphere. This process generates global winds. The global winds help move ocean currents. Ocean currents help transfer heat to the atmosphere. This process generates global winds. The global winds help move ocean currents. Any major change in an ocean current can cause a change in climate. El Nino is an example. Any major change in an ocean current can cause a change in climate. El Nino is an example.

THE RAIN SHADOW EFFECT

REVIEW QUESTION How does the Rain Shadow Effect affect climate? A. Windward side: warm and dry Windward side: warm and dry Leeward side: cold and moist Leeward side: cold and moistB. Windward side: cold and moist Windward side: cold and moist Leeward side: warm and dry Leeward side: warm and dry

Review question As elevation _________, the average annual temperature __________. Elevation Temperature A.increases; decreases B.decreases; increases