The Atmosphere, Weather and Climate
Transcription
The Atmosphere, Weather and Climate
Atmosphere, Weather and Climate Section 1: Atmosphere Atmosphere Atmosphere: a thin envelope of gases that surrounds the earth/planet Between 1650 and 1660 a scientist named Robert Boyle discovered that air contains a substance that is required for life. He called it “vital air.” We call it oxygen, or O2 In the 1750’s a scientist named Joseph Black discovered that limestone mixed with acid gives off a substance that quickly extinguished flames. He called it “fixed air.” We call it carbon dioxide, or CO2 In 1772, Daniel Rutherford preformed experiments that got rid of vital air and fixed air. What was left killed living things and extinguished flames. He called the substance that remained “noxious air.” We call it nitrogen or N2 * There are 6 major components of air: 1. Nitrogen 2. Oxygen 3. Carbon dioxide 4. Trace Gases 5. Water Vapor 6. Particles Which one(s) do you think is/are the most abundant in the air we breath? Nitrogen - N2 78% of the volume of the atmosphere and the air we breath Oxygen - O2 Comprises 21% of volume of the atmosphere Another form is called ozone – O3 Ozone - a form of oxygen that has 3 oxygen atoms instead of the normal 2 atoms Less stable than O2 (breaks down faster) Good in stratosphere (a portion of the upper atmosphere) absorbs UV radiation Not good at ground level a pollutant – irritates the linings of lungs Carbon Dioxide – CO2 Essential for life – photosynthesis Burning fuels releases CO2 A greenhouse gas Trace Gases Trace: tiny, very small amounts Includes gases such as: Argon (Ar), Neon (Ne), Helium (He), Methane (CH4), Krypton (Kr), and Hydrogen (H2) Water Vapor Water vapor: water in the form of a gas Invisible (generally, except for clouds) Very important to weather and climate Particles/Particulates Not gases actual pieces of “things” in the air Includes: dust smoke salt chemicals sand * Why Is The Atmosphere So Important? 1. 2. 3. 4. 5. * Contains O2 and other gases required for respiration Contains CO2, O2 and other gases required for photosynthesis Keeps surface of earth warm enough to keep H2O in liquid form (requirement for life) Protects us from harmful UV radiation Protects us from meteoroids slows them down burns them up Properties of Air 1. Mass 2. Density 3. Pressure Mass Mass: the amount of matter contained in an object Anything that consists of gases and particles has mass If we know that air has mass, what else might it have that is related to mass? Density Density: the amount of mass in a given volume Density = mass volume g/ml or 3 g/cm more molecules = higher density Pressure Pressure: pushing force on a surface or area Air pressure: the pressure caused by the weight of a column of air pushing down on a surface Why don’t we get crushed by the air pressure? Because air is pushing in all directions (up, down, sideways, etc.) - it is balanced Air pressure changes day to day, hour to hour Denser air (more molecules) has higher air pressure Pressure is measured by a barometer Barometer: an instrument used to measure air pressure There are 2 types of barometers Mercury barometer (now called a liquid barometer) Aneroid barometer Units for both types: inches of mercury or millibars 1 in ~ 33.87 mb * Mercury Barometer Mercury is a restricted metal (new ones are not being made anymore) • water can be used too - hence the alternate name, liquid barometer • the tube is a minimum of 84 cm tall (for accuracy) • 1 atmosphere = 760 mm Aneroid Barometer air-tight metal chamber, usually made of copper and beryllium, making it sensitive to changes in air pressure • an increase in air pressure: chamber walls go in (causing a dial to move) • a decrease in air pressure: chamber walls bulge out (causing a dial to move in the opposite direction) * Altitude and Air As you go farther away from Earth: mass, pressure, density and temperature changes Mass • decreases as you go higher • still has the same amount of all of the gases, but the gases are more widely dispersed, or spread out as you go higher Density • decreases as you go higher in altitude Density = mass volume • if volume stays the same but mass decreases, then density must also decreases Pressure • decreases with increasing altitude • the farther you get away from the earth’s core, the less gravity affects objects, so pressure decreases (pressure deals with weight, which is a function of gravity ). Temperature • does not change on a linear scale • temperatures do not steadily increase or decrease throughout the atmosphere • layers of the atmosphere are categorized by temperature changes Layers of the Atmosphere a. b. c. d. Troposphere Stratosphere Mesosphere Thermosphere Troposphere Tropo = changing Troposphere: layer of the atmosphere where the Earth’s weather occurs • sea level to about 18-20 km high 9 km at poles, 18-20 km at equator • where we live • area of most weather occurrence • conditions are the most variable than all other layers • contains almost all of the mass of the atmosphere • temperature steadily decreases as you go higher • in upper regions of the troposphere, temperature is around -60C (-76 F) • on average, for every 1 km increase in altitude temperature decreases by 6.5C (almost 12 ) Stratosphere Strato = spread out, layer Stratosphere: layer of the atmosphere that contains a large amount of ozone • found from around 18-20 to 50 km above sea level • where many airplanes fly • as altitude increases, temperature increases recall ozone is absorbing UV radiation! • temperature ranges between - 60 C to –2 C Mesosphere Meso = middle Mesosphere: the layer of the atmosphere that protects the earth from meteoroids • found from 50 – 80 km above sea level • as altitude increases, temperature decreases • temperature ranges between -2C to - 80C (contains fewer ozone and other gas molecules) Thermosphere Thermo = heat Thermosphere: the outermost layer of the earth’s atmosphere that contains the ionosphere and exosphere • found from 80 km to space (blends gradually, no definite edge) • as altitude increases, temperature increases • temperature ranges between -90C to +1800C • temperature increases due to solar radiation hitting this layer first and heating up the molecules found there. • does not feel hot because there are not a lot of molecules hitting you (or the thermometer) even though they are moving very fast. Thermosphere divided into 2 layers: 1. Ionosphere 2. Exosphere Ionosphere • lower portion of the thermosphere • found between 80 km – 400 km • energy from sun causes gas molecules to become electrically charged (called ions) • radio waves bounce off these ions and back to Earth’s surface • the aurora borealis occurs in the ionosphere • particles from the sun enter the ionosphere near the poles and hit molecules that causes the molecules to glow! Exosphere Exo = outer • upper portion of the thermosphere • found from about 400 km out to outer space (thousands of kilometers wide) • Earth’s satellites for phone, television and weather are located in this area Air Quality Natural sources of air pollution: 1. Forest fires: dust, smoke, CO2, NO2 2. Soil erosion 3. Sand storms 4. Erupting volcanoes Air Quality Man-made sources for air pollution: 1. Farming 2. Construction 3. Burning fossil fuels such as coal, gas, methane and oil which causes: Smog: air that is polluted with particulates from the burning of fossil fuels Acid rain: rain that contains more acid than normal due to the burning of high-sulfur fossil fuels, especially coal 4. Cars 5. Man-made fires 6. Gas Stations Atmosphere, Weather and Climate Section 2: Weather Factors – Wind, Humidity, Precipitation Weather - Quick Background The movement of heat in the atmosphere is a major factor of weather it can affect temperature, wind, rain * Heat comes from the sun in the form of electromagnetic waves Most is visible light and infrared radiation (long wavelength), and a small amount is UV radiation (short wavelength) Much of the UV radiation is absorbed by ozone in stratosphere Not all reflected sunlight makes it out into space: The warm gases make a “blanket” around the Earth keeping it warm Incoming sunlight: • 50% is absorbed by surfaces and becomes heat • 25% is reflected back into space by clouds • 20% is absorbed by gases and particles in air (remember O3) • 5% reflected back into space by water Some things to remember/memorize: • hot/warmer air rises • cold/cooler air sinks • warmer air can hold more moisture than cooler Weather Factors A. Wind B. Humidity C. Precipitation A. Wind Air is fluid, so it moves from place to place wind: the horizontal movement of air from a region of high pressure to a region of low pressure Remember: warm air rises - if warm air rises, that means that it is less dense warm air is less dense = warm air has a lower air pressure cold air molecules do not move much - more dense air = higher air pressure SO . . Wind is caused by differences in air pressure Wind How do you measure wind? You measure both direction and speed To measure direction - use a wind vane Wind swings the vane so that one end points into the wind, Wind vanes indicate where the wind is coming from To measure speed - use an anemometer Think pinwheel on its side 3-4 cups attached to an axel and can spin freely A gauge/meter on the axel calculates wind speed Wind Another part of wind is how it feels Wind-chill Factor: a measure of cooling, due to a combination of wind and temperature. Wind blowing across skin will “pull” body heat out of you (heat moves from areas of high heat to areas of lower heat) The stronger the wind, the faster the wind moves, the cooler you feel Great when it is warm out – cools you off ! Can be deadly when it is already cold outside. Local Winds Form only where large scale winds are weak Only travel/blow over short distances Caused by the unequal heating of the Earth’s surface within a small local area Local Winds There are 2 types of local winds: sea breeze land breeze Both occur near large bodies of water Local Wind - Sea Breeze Sea breeze: a local wind that blows in from a sea or lake onto the land (also called lake breeze) Occurs along the shore of a large body of water (i.e. sea/ocean, gulf, Great Lakes) Land heats up faster than water, so the warm air over the land rises, allowing the cool air over the water to come blowing in Generally occurs during the daytime. Local Wind - Land Breeze Land breeze: a local wind that blows from the land over a sea or lake Occurs along the shore of a large body of water Land cools faster than water (cooler air = higher pressure) • wind moves from higher pressure to lower pressure • wind now blows from the land to the water! Generally occurs at night Global Winds Global wind: a wind that blows steadily over a long distance from a specific direction Created by the unequal heating of the Earth’s surface Middle of the day: Sun hits most directly at Equator, heating that area a lot! Sun hits the poles at an angle, spreading out over a wide area, heating the surface less Temperature difference between poles and equator creates a giant convection current Warm air rises at the equator (lower pressure) Colder air sinks at the poles (higher pressure) Difference causes the winds to blow from the Poles to the Equator Winds do not blow in a straight line from the poles to the equator because the Earth rotates and is tilted. The rotation of the Earth causes winds to curve. This is called the Coriolis Effect. Global winds in Northern hemisphere generally blow from east to west Global winds in the Southern hemisphere generally blow from west to east Do not have one large temperature current. Warm air will travel a limited distance before cooling and then sinking. Global Wind Belts Earth has a total of six (6) global wind belts: 3 in Northern hemisphere 3 in Southern hemisphere From poles to the equator, they are named: (The same name is used in both hemispheres) ( 90˚ to 60˚ N/S) Polar Easterlies Polar Front (60˚ N/S) Prevailing Westerlies (30˚ N/S to 60˚ N/S) Horse Latitudes (30˚ N/S) Tradewinds (0˚ to 30˚ N/S) Doldrums (0˚) Open up your agendas to the world map! 90° 60° N 30° N 0° 30° S 60° S 90° Polar Easterlies global wind belt found between 60 N or S and the Pole cold air at the Pole sinks and flows back toward lower latitudes Coriolis effect twists these winds in a westerly direction so winds blow from the east meets the Prevailing Westerlies around 60 N or S in a region called the polar front the meeting of the warm and cold air along this front greatly effects the U.S. weather *Remember: Air temperature is relative to position on Earth Prevailing Westerlies global wind belt found between 30 N or S and 60 N or S does not blow directly towards the north due to the Coriolis Effect pushes the winds from west to east, therefore blows or comes from a SW direction important to U.S. weather Tradewinds a global wind belt found between 0° to 30° N/S named because sailors depended on these winds to get to trading countries around the world Warm air rising from the equator, causing low pressure, cooler air travels from N/S to the equator, warming, etc. Blow from the Horse Latitudes (~ 30 N/S) to the equator from a NE direction due to the Coriolis Effect 2 areas of relative calm or weak winds: • doldrums (warm air rises) • horse latitudes (cooler air sinking) where air is either rising or descending there is little wind movement (horizontal movement) Doldrums an area of calm winds located right around the equator, 0 steady rising of warm air (creates low pressure) cooler air rushes in but is quickly warmed by the sun and rises before it can move too far. therefore, the wind near the equator is weak. Horse Latitudes an area of calm winds located around 30 N or S upper air stops moving towards poles and sinks – high pressure (it gets cooler) Why is it called the “horse” latitudes? Jet Stream Recent discovery (1940’s) when WWII jets began flying higher located around 10 km above sea level • high speed winds 200-400 kmph • very wide (100 km), but shallow (1-2 km) • move in a slow wavy pattern from W to E (following Earth’s rotation) B. Humidity Recall the water cycle Humidity: a measure of the amount of water vapor in the air Humidity Generally recorded as “relative humidity” Relative humidity: percentage of water vapor actually in the air compared to the maximum amount of water vapor the air can hold at a given temperature Ex: 10C air can hold 8g water vapor/m3 If humidity was 8g water vapor, then: relative humidity = 8g/8g = 100% i.e. saturated If humidity was 4g water vapor, then: relative humidity – 4g/8g = 50% Humidity Humidity is measured using a psychrometer Psychrometer: device used to measure relative humidity Has 2 thermometers: a wet bulb and a dry bulb Wet bulb: cloth covers bulb; this cloth can be and is moistened with water Dry bulb: no covering over thermometer bulb Relative humidity is found by comparing the temperatures of the dry bulb to the wet bulb The psychrometer is “slung” around its handle for about 30-45 seconds • Air blows over both thermometers • The wet-bulb thermometer is cooled to a lower temperature than the dry-bulb due to evaporation of water from the wet cloth • If humidity is high – little evaporation on the cloth occurs, so the difference between the two thermometers is small • If humidity is low – lots of evaporation on the cloth occurs, causing the wet-bulb thermometer to read a much lower temperature than the dry-bulb thermometer Cloud Formation Clouds form when water vapor condenses to form liquid water or ice crystals Condensation requires two (2) conditions: 1. Cooling of the air Remember - cooler air holds less water vapor 2. Presence of particulate Surface for condensation to occur upon Most particulates are: salt crystals from oceans dust from the soil smoke bacteria Clouds are classified by: Shape Altitude Capability to produce precipitation Cloud Classification - Shape There are three (3) basic shapes: Cirrus Cirrus = curl of hair • Look wispy, feathery, mare’s tail • Only form in high altitudes (above 6 km) • Made of ice crystals Cumulus Cumulus = heap, mass • Look like fluffy, rounded piles of cotton • Form less than 2 km above the ground but can grow to extend up to 18 km tall! Stratus Stratus = spread out • Flat layers, generally dull, grey color • Cover a lot, if not all, of the sky • Low level clouds Cloud Classification - Altitude Alto alto = high Clouds that form 2-6 km above the ground (middle level clouds) or above the level that the shape is usually found Cirro Clouds that usually form in very high altitudes, generally above 8 km Cloud Classification - Moisture Moisture/Precipitation Ability Nimbus or nimbo – Cloud that can produce rain or snow Naming Clouds Cloud terms: cirrus cumulus stratus alto cirro nimbus/nimbo Now lets put these terms into actual cloud names – 10 to be exact – and what kind of weather may be indicated when you see them! Cloud Names Cirrus – wispy, “mare’s tails” *fair weather Cirrocumulus – look like rows of cotton balls or fish scales *storms are probably on the way Cirrostratus – very thin clouds that cause halos around the sun or moon *precipitation may follow in 12-24 hours Altocumulus – slightly higher than normal and more cumulus clouds *thunderstorms may occur by the late afternoon Altostratus – spread out clouds higher than normal *often form ahead of a storm that will produce a steady rain/snow Cumulus – cotton balls *indicates fair weather until they get big enough to become: Cumulonimbus – huge towering clouds with flat tops *produce thunderstorms , sometimes violent Stratocumulus – cumulus clouds in a steady layer *can indicate a coming storm Nimbostratus - uniformly grey clouds in a steady layer *can produce constant drizzling rain/ light snow Stratus – “cloudy day” cloud; fog *sometimes can indicate rain/snow Cloud Type and Altitude Cirrus Cirrocumulus Cirrostratus Altocumulus Altostratus Cumulus Stratocumulus Nimbostratus Stratus High clouds 5-13 km Mid-level clouds 2-7 km Low clouds 0-2 km Cumulonimbus C. Precipitation There are 5 types of precipitation: Rain Sleet Freezing Rain Snow Hail Liquid water (droplets) or ice crystals need to be big enough and heavy enough to fall through the air and touch the ground to be considered precipitation cloud droplet = 0.002 mm Average time from evaporation of a single water molecule to precipitation is 9 days Rain • Most common form of precipitation • Must be at least 0.5 mm in diameter Smaller diameter liquid water is called drizzle Smallest is mist and usually comes from stratus clouds Sleet • Rain that has fallen through a layer of air that is below 0C (below 32F) Rain drop freezes on its way to the earth’s surface! • Smaller than 5 mm in diameter • OR. . . . Freezing Rain • Rain that has fallen through cold air that is located very near to the ground Not enough time to freeze in the air (like sleet), but freezes as soon as it touches a cold surface • Also called an ice storm Snow • Water vapor that has turned directly into an ice crystal inside a cloud (recall sublimation) • Called snowflakes • Cloud needs to be a cold cloud, below 0C, for snow to form Hail • Round pellets of ice larger than 5 mm in diameter • Can form inside cumulonimbus clouds during a thunderstorm • Requires strong updrafts of vertical wind inside the cloud to keep “flinging” the ice pellet back into the cloud, further coating it in ice The longer a pellet is in the cloud, the bigger the hail Atmosphere, Weather and Climate Section 3: Weather Patterns Weather Patterns Recall from previous lessons: • Warmer air rises – less dense • Cooler air sinks – more dense • Warm air holds more moisture than cooler air Today’s weather can be influenced by the air 1,000 or more kilometers away! Air Masses and Fronts Air mass: a large body of air that has similar temperature, humidity and pressure at any given height large =1,000,000 km2 and 10 km deep! We will learn: Types of fronts Types of air masses Movement of air masses Fronts Front: boundary where air masses meet Fronts do not readily mix when they meet There are four main types of fronts: • Cold front • Warm front • Stationary front • Occluded front Cold front: rapidly moving cold air mass runs into a slower moving warm air mass Colder air moves under the less dense warm air, pushing the warm air upwards As the warm air moves upwards, it cools - the now cooling warm air reaches its dew point Dew point: temperature at which water vapor condenses into droplets of water or ice crystals • cloud formation • if there is enough moisture in the warm air then rain, snow or a thunderstorm may occur Behind the cold front: • cooler temperatures, drier air • clear skies (why?) • shift in wind (direction and speed) On a weather map depicted as: • blue line with triangles • triangles point in the direction the cold front is moving towards (why?) Warm front: a faster moving warm air mass overtakes a slower moving colder air mass less dense, warm air moves over the denser cold air • if warm air is humid: warm air slowly rises over the cold air, cools, and may release its water vapor in the form of light rain or snow • if the warm air is dry: scattered clouds occur Warm fronts move slowly, which makes it possible to have rainy or cloudy weather for days Behind warm front: Warm, humid or dry weather WHY? Warm Front On a weather map: • red line with half circles • semicircles point in direction that the warm air mass/front is moving * Stationary front: two air masses, one warm and one cold, face each other in a “stand off” • fronts cannot move each other • water vapor condenses into rain, snow, fog or clouds where the two air masses meet • precipitation can fall for days • very little, if any, wind in this region On a weather map: • blue + red line with blue triangles and red half circles • blue points in the direction that the cold front is trying to move • red points in the direction that the warm front is trying to move Occluded front: warm air mass is caught between • • • • two cooler masses, one colder than the other denser, colder air masses push under the warm air mass, pushing the warmer air mass up warm air is cut off from the ground (occluded= cut off) temperatures cool weather may turn cloudy with rain or snow On a weather map: • purple line with alternating purple triangles and hemispheres • point in the direction that the colder air mass is moving Types of Air Masses So far we have been talking about cold and warm air masses. We can actually define them a bit more! Air masses are classified by two characteristics: • temperature (temperature affects air pressure) • humidity Words to know: Tropical: warm air masses that formed in the tropics (0-30) Polar: colder air mass formed above 50N or 50 S Maritime: humid air mass that formed over the oceans Continental: dry air mass that has formed over land Now we can put these 4 words together like we did with the clouds words how many will there be if you can only put one humidity word with one temperature word? Maritime Tropical (mT) Warm, humid air mass formed over the tropical oceans tropical oceans near the US: Gulf of Mexico, Southern Atlantic, Southern Pacific Travel into SE U.S., then get pushed to the N and NE into Central and Eastern U.S. (nor’easter) Summer hot, humid weather Winter heavy snow or rain Maritime Polar (mP) Cool, humid air mass formed over the North Pacific and North Atlantic oceans in the U.S. Can effect West Coast much more than East Coast (why?) Summer/winter cooler temperatures with fog or rain Continental Tropical (cT) Hot, dry air mass formed generally in the summer over the SW and Northern Mexico • covers a smaller area • moves in a NE direction • brings hot, dry weather to Arizona, New Mexico, eastern Texas and the Great Plains Continental Polar (cP) Cold, dry air mass forming over Canada and Alaska Winter brings very cold, dry, and clear weather to North America Summer air mass is more mild, but still brings cooler temperatures Movement of Air Masses Two (2) major means to move air masses: • Prevailing Westerlies • major wind belt across the continental United States • generally push air masses from W to E • Jet Stream • bands of high speed winds starting at around 10 km above sea level • generally push air masses from W to E in an undulating pattern Weather Technology Meteorologist: a scientist who studies the causes of weather and predicts what weather will be like in certain areas Old methods of determining weather include: • Cloud types • Broken bones • Barometer readings Automated weather stations over 1700 surface stations in U.S. record: • temperature • pressure • relative humidity • rainfall • wind speed/direction New technologies are used to increase accuracy: Weather Balloons Carry instruments into upper troposphere to the lower stratosphere Measure: temperature, pressure, humidity Satellites • TRIOS-1 launched in 1960 was the first weather satellite • cameras show: • Earth’s surface • clouds (tops of) • storms • snow cover • instruments take readings in: • temperature • humidity • solar radiation • wind speed/direction Computer forecasts • collects large amounts of data • process data quickly • each forecast builds upon the previous forecast (as new data arrives, the forecast is updated) gives forecast for: 12 hours (most accurate) 24 hours 36 hours 5-10 days (least accurate) * Reading A Weather Map • many small weather stations across the U.S. and the world • data from weather stations in the US are gathered and assembled into weather maps at the National Weather Service From data collected, you can make: Isobars Isotherms Weather Station Symbols Isobars: lines joining stations that have the same pressure Listed with just the last three numbers in mb (millibars) Isotherms: lines joining stations that have the same temperature (F in the U.S.) Isobars and isotherms never cross each other – make wavy circles, ovals in areas Surface Temperature Map Surface Air Pressure Map Weather Station Symbols Not all symbols are given every hour, especially if there is no change in weather conditions Also depends on the site you use; some give all, some give just a few C A E F G I J Cyclones and Anticyclones Occur when air masses collide around large surface features like mountains, the jet stream or even other air masses Bends develop, air begins to swirl, forming a: • • • • Cyclone Anticyclone Tornado Hurricane Cyclone Air swirls counterclockwise, inward and up • low pressure system • clouds gather, gets windy (upward motion of air causes air to come rushing in to fill the void) • humid air Cyclones over water can become: • Hurricane (Atlantic, Pacific) • Typhoon (West Pacific) • Cyclone (Indian Ocean, Southern Hemisphere) Anticyclone Air swirls clockwise, outward and down • high pressure system • skies clear (air is not moving upward – required for condensation) • drier air • light to no wind Hurricane a tropical cyclone with winds of 74 mph or more that forms over an ocean (minimum 74 mph, max 157 mph) Conditions for a hurricane to form: • warm water • low pressure area • sand from Sahara Desert Hurricane Andrew’s Path (1992) Hurricane Isabel (2003) Hurricane Formation • warm air rises over an ocean forming clouds (a low pressure area) • more warm air is pulled into the system (winds move from high to low pressure areas) • causing more clouds to form, pulling more humidity out of the ocean (tropical disturbance forms) • winds spiral inward toward low pressure area causing a lowering of pressure, causing more winds, etc… “snowball effect” • hurricanes get their energy from warm ocean currents • once over land, the hurricane loses its energy source and loses strength • damage is due to winds, high waves, severe flooding and storm surges a “dome” of ocean water that sweeps across the coast in a wide area near where a hurricane comes onto land • due to the low pressure and high winds Hurricane Ratings categorized by sustained wind speeds Saffir – Simpson scale Category Wind Speeds (mph) Air Pressure (mb) Storm Surge (ft) 1 - minimal 74-95 above 980 3-5 2 - moderate 96-110 979-965 6-8 3 - extensive 111-129 964-945 9-12 4 - extreme 130-156 944-920 13-18 5 - catastrophic 157+ below 920 over 18 Tornados Tornado: a destructive storm of a rapidly rotating column of air that is in contact with both the earth’s surface and a cumulonimbus cloud a condensation funnel is what forms the tornado’s characteristic shape can reach speeds of 480 km/h (300 mph) Conditions for tornado formation: • warm, humid air mass from Gulf of Mexico (Maritime tropical) • cold, dry air mass from Central Canada (Continental Polar) • thick cumulonimbus clouds Tornado Formation: • warm, moist air is found under cumulonimbus clouds • cold, dry air comes in and forces the warm, moist air up into cumulonimbus clouds, forming a low pressure area inside the cloud • warm air begins to rotate in the cumulonimbus cloud as it meets winds blowing in different directions at different altitudes • Tornado forms when a part of the cloud descends to the earth (in a funnel-shape condensation tube) due to the rapidly rotating air Size of tornado does not always indicate intensity, very subjective • depends on how experienced the surveyor is • “terrible tornado” sounds good on TV but may not be actual intensity Fujita Scale • damage scale invented by Dr. T. Theodore Fujita, at the University of Chicago (1971) • tornado damage due to high winds and flying debris • rating based on damage, swirl patterns on the ground, radar tracking, photography (if available) and eyewitness testimony • how can you estimate rating if only occurred in a corn field? • ranged from F0 – F5 • updated in 2007 (EF Scale) • accounts for plant damage and differences in construction techniques • better technology EF0: Light damage • 104-137 kph (65-85 mph) • few shingles removed • tree branches broken (39%) EF1: Moderate damage 138-177 kph (86-110 mph) • roofing material peeled off (trusses still in position) • mobile homes pushed off foundation • moving autos pushed off roads (36%) EF2: Considerable damage • • • • • • 178-217 kph ( 111-135 mph) trees uprooted trusses off frame homes mobile homes demolished train cars/boxcars overturned high rise windows broken (19%) EF3: Severe damage • • • • • 218-266 kph (136-165 mph) entire trains derailed/overturned walls and roofs torn from well constructed homes trees in forests uprooted heavy cars thrown (5 %) EF4: Devastating damage • • • • 267-322 kph (166-200 mph) homes leveled weak foundations broken/blown cars propelled through air (1 %) EF5: Incredible damage • > 322 kph (> 200 mph) • steel reinforced concrete structures damaged • auto-sized missiles > 100 m • total destruction (> 0.1 %) Hypothesized F6: Inconceivable damage ? Tornados Hurricane • formed over ocean/sea • one air mass involved • lasts for days • max winds = 157 mph • damage due to wind and storm surge • hundreds of miles wide • average of 10-15 per year • days to weeks warning • can spawn tornadoes Tornado formed over land two air masses involved lasts for minutes max winds = 200+ mph damage due to wind and flying debris less than a mile wide over 1200+ per year minutes to hours warning cannot spawn a hurricane • rating/category based on wind speed • produce rain, winds • cyclones (low pressure areas) Atmosphere, Weather and Climate Section 4: Climate Climate the average, year-after-year, conditions of temperature, precipitation, winds and clouds in an area Microclimate – a small area with climate conditions different from that around it Examples: riparian area vs. surrounding desert irrigated neighborhoods next to non-irrigated 2 main factors describe climate: Temperature Precipitation * What influences temperature? 1. Latitude 2. Altitude 3. Distance from large bodies of water 4. Ocean currents Latitude: distance from the Equator in degrees 3 main zones: Tropical An area that receives direct or almost direct sunlight all year round • straddles Equator (23.5 N/S) • almost all of Trade Wind belt • warm and humid Polar An area where the sunlight hits the surface at an angle (indirectly) • 66.5 N/S to 90 N/S • cold Temperate An area where the sun is more direct in the summer than the winter • between tropical and polar • 23.5 N/S – 66.5 N/S • Summers warm, winter cold * Altitude the distance above sea level Supersedes latitude when figuring out temperature i.e.: can have very cold mountain tops in tropical zone For every 1km above sea level, temperature drops 6.5 C Ex: Mount Kilimanjaro ~ 6 km above sea level 6 x 6.5 = 39 C difference in temperature between Serengeti Plain and top of Mt. Kilimanjaro Distance from large body of water oceans moderate temperature extremes of nearby land recall: water heats up/cools off more slowly than land Wind blowing from oceans to land tends to prevent extremes Ex: West Coast vs. Great Plains West Coast maritime climate mild winters, cool summer Great Plains continental climate cold winters, warm/hot summer Ocean Currents streams of water within the oceans that move in regular patterns • Cold water flows from the poles towards the equator • bring cold/cooler air • can keep some southern latitude countries cold • East Coast of South America • West Coast of Africa (southern regions) • Warm water from the tropics flows towards the poles • bring warm/warmer air • can keep some northern latitude countries warm • Gulf Stream/North Atlantic Drift: England, Ireland, Sweden (mild, humid air) • (El Niño and La Niña) Precipitation What influences precipitation? 1. Wind 2. Mountain Ranges 3. Seasonal Winds Winds Amount of water vapor in an air mass – influences how much precipitation will fall Amount of water vapor in air masses – depends on where these winds come from i.e. Maritime or Continental In the U.S., most air masses are moved by the Westerlies and the jet stream Mountain Ranges Need to be large, cover a big area Ex: Rockies, Sierra Madres, Cascades not South Mountain, but it can be a microclimate Creates what is called a rain shadow: an area having relatively little precipitation due to the effect of a large barrier causing the prevailing winds to lose moisture before reaching the area Rain Shadow • winds are forced to rise up and over mountains (draw diagram) As air rises, it cools: • cool air cannot hold as much moisture • clouds form on the windward side • precipitation falls before the winds finish going over the mountains • winds continue to travel across mountains, but are now drier • winds descend on downward or leeward side • warms up • soaks up any available moisture and keeps it! (warm air holds more moisture) Seasonal Winds a change in wind direction between summer and winter Summer: land generally warmer than water • caused air to rise • low pressure to form (over the land) • more wind comes in from the ocean • wind moves form an area of high pressure to and area of low pressure • increased humidity in the air • potential increase in precipitation Winter: land generally cooler than water • more wind from land to ocean • drier air • things in AZ a bit different!! Seasonal Changes in Climate • climate conditions are not static • change with the changing seasons: summer, winter, fall, spring What causes seasons? • seasons change as the amount of energy from the sun changes • due to • Earth’s tilted axis Earth’s tilted axis • at an angle of 23.5 • axis always points in same direction, no matter where it is in the Earth’s orbit • tip of axis is pointed at the sun for part of its orbit (year) and away in another part of its orbit • when northern end of axis is tilted at the sun: • summer in the Northern hemisphere winter in the Southern hemisphere • when southern end of the axis is tilted at the sun: • winter in the Northern hemisphere summer in the Southern hemisphere Short-term climate change El Niño and La Niña short term changes in the tropical Pacific Ocean sea surface temperatures (SST) due to changes in the currents and trade wind strength Figure A - normal conditions Figure B – El Niño conditions El Niño short-term change in the Pacific Ocean where SST are warmer than normal • generally begins in November/December • occurs every 2-7 yrs and can last 1-2 yrs • trade winds weaken – • do not blow from the east as strong • warmer water begins to travel west towards South America • warmer water causes the surface water temperature off the coast of South America to rise by as little as 0.5 C or as much as 3.5 C • disrupts: nutrient flow, weather • warmer water = warmer maritime winds = more precipitation La Niña short-term change in the Pacific Ocean where SST are colder than normal • opposite of El Niño • trade winds strengthen, forcing more cold water into tropics and west across the Pacific Ocean towards the Australia, Indonesia, etc. • good for nutrient cycle in ocean brings up nutrients from far below the ocean surface strong weak Climate: Global Warming • the Earth’s atmosphere holds in heat from the sun (keeps water in a liquid state) • different types of molecules/gasses trap or hold heat in the atmosphere and are called greenhouse gases any gas found in the atmosphere that can hold heat • most common greenhouse gases: • water vapor (H2O) • methane (CH4) • carbon dioxide (CO2) • nitrous oxide (N2O) • CFCs Chlorofluorocarbons; man-made chemicals that trap heat in the atmosphere and break down ozone Possible effects of a warmer Earth: Warmer ocean waters • increase in hurricane strength • change of ocean currents • increased glacier ‘calving’ Increased land temperatures: • plant crops in new regions • plant more than one crop per season in some areas • reduced crop land • rising ocean waters due to melting of glaciers Climate: Ozone Depletion In the 1970’s, discovered the ozone layer over Antarctica was thinning • more UV radiation was reaching the Earth’s surface in the area Cause: • Increase in amount of CFCs escaping into the stratosphere • used in many applications: • refrigerants, cleaners, aerosols, etc. WHY? Thinning ozone layer = • increased eye problems • increase in number and types of skin cancers Protection against UV radiation: • apply sunscreen of at least spf 30 • wear hats, long sleeves and sunglasses • reduce exposure to midday sun