ES May 19 Air Pressure and Wind, Air masses, fronts, midlatitude cyclones, Severe Storms

Transcription

1 ES May 19 Air Pressure and Wind, Air masses, fronts, midlatitude cyclones, Severe Storms I. Pressure A lab./in 2, exerted in all directions: up, down, sideways B. Measuring air pressure with barometer 1. millibars standard sea-level pressure: mb 2. inches of mercury: a. rises in evacuated tube from pressure on open dish b. standard sea-level pressure: inches 3. aneroid barometer uses partly evacuated metal chamber a. high~fair b. low~storm c. overgeneralization 4. barograph records pressure continuously II. Wind A. Horizontal movement of air (advection) 1. flows due to pressure differences: Pressure Gradient Force a. from high to low b. created by unequal heating of Earth s surface 2. affected by surface friction 3. affected by Coriolis Effect B. pressure gradient force 1. maps drawn of pressure shown with isobars equal pressure lines 2. spacing of isobars shows the pressure gradient 3. wind blows more strongly with larger pressure gradients 4. initial direction from high pressure toward low pressure but C. Coriolis Effect begins to affect direction 1. general mechanism a. deflected to right of their path in Northern Hemisphere b. deflected to left of their path in Southern Hemisphere c. regardless of direction of travel d. not affected at equator 2. affect on wind flow a. changes direction at 90 O angle to wind flow b. does not affect wind speed c. wind speeds affect amount of Coriolis Effect 1) greater speeds: more deflection 2) slower speeds: less deflection D. friction of Earth s surface affects wind flow 1. upper levels of atmosphere not affected by friction a. wind flow follows isobars: b. geostrophic winds 2. slows wind speeds at lower levels of atmosphere a. reduces amount of Coriolis Effect pressure gradient prevails b. surface winds directed toward low pressure at angle across isobars c. surface roughness affects amount of surface friction III. High pressure and low pressure

2 A. Low pressure called a cyclone 1. northern hemisphere cyclones turn counterclockwise as winds blow inward toward low pressure and are deflected to right by Coriolis effect 2. southern hemisphere cyclones turn clockwise by same effect 3. flow inward results in surface convergence, a. creating uplift and storminess: due to expansion and cooling b. consequent divergence aloft may become stronger than surface convergence and intensify cyclone B. High pressure called anticyclone (the opposite of cyclone) 1. winds flow outward 2. surface divergence at center, a. convergence aloft where air drawn into area of divergence b. subsiding air precludes rainfall because it is compressed and warms C. these effects are the basis for fair and stormy indications on barometer D. isobar maps show high pressure ridges, and low pressure troughs IV. General circulation of the atmosphere A. Greatest heating in tropics creates uplift of rising air 1. flow from poles to equator would occur without Coriolis Effect or friction 2. these break single circulation into smaller cells, with surface directions B. Idealized global circulation 1. equatorial low created by Sun heating a. abundant precipitation b O N and S of equator c. Cooling aloft, and poleward flow 2. descending air about 30 O N and S of equator a. subtropical high pressure b. descending air does not rain desert belts across Earth 3. wind flow between equatorial low and subtropical high a. affected by Coriolis b. creates Trade Winds 4. poleward flow at surface from subtropical high deflected into Westerlies 5. cold dense air from Polar High converges with Westerlies to create subpolar low a. Polar easteries occur here b. Polar front is interaction of cold polar air and warmer midlatitudes air 6. Jet Streams are geostrophic winds created at the interaction of global circulation patterns a. Polar front jet stream at the polar front Rossby waves b. Subtropical jet stream between tropical and midlatitudes air

3 7. continents interfere with idealized global circulation a. result is closed, semi-permanent pressure cells b. high pressure 1) Pacific High persistent 2) Azores high seasonal winter 3) Siberian High seasonal winter a) Results in offshore winds from Asia to Indian Ocean dry b) Summer heating draws air off Indian Ocean wet Monsoon! 4) Bermuda High seasonal summer c. Low pressure seasonal winter: source of storms 1) Aleutian low 2) Icelandic low 8. Westerlies a. Coriolis Effect creates wind from west to east b. Interrupted by migrating cyclonic systems bringing weather 1) Cyclones driven by upper level wind flow 2) Upper level flow migrates seasonally a) Winter months allow storms further toward equator b) Summer month storms generally further poleward V. Local wind systems created by local temperature and pressure differences A. Land and Sea Breezes 1. heating land in daytime causes rising air 2. air drawn in off sea is a sea breeze 3. nighttime cooling of land leaves sea warmer 4. air drawn toward sea from land is land breeze B. Mountain and Valley Breezes 1. similar to Land and Sea Breezes, due to temperature changes 2. daytime heating of slopes results in a valley breeze, more predominant in summer 3. nighttime cooling of upper areas can chill air to descent slopes as mountain breezes, most predominant in winter C. downslope, strong, drying, warm winds have local names: Chinook, Santa na, Mistral VI. Measuring wind A. Winds named for the direction from which they come B. Prevailing wind describes the usual direction of wind 1. sometimes indicated by slant of tree trunks, or branch density 2. US has generally west winds: we are in the Westerly Wind Belt 3. interference of migrating cyclonic systems C. anemometer measures wind speed D. some areas have very reliable predominant winds: 1. knowledge of persistent pressure patterns helps predict these 2. Trade Winds are example VII. El Nino and La Nina A. Interruption of Trade winds and equatorial oceanic current B. Consequent see-saw of pressure centers in southern hemisphere

4 VIII. Air Masses A. Defined: large body of air, 1600 km or more across, with similar temperature and moisture at similar altitudes 1. Brings these characteristics with it as it moves to different areas 2. example a. Canadian continental air mass goes to Mexico b. Air mass temperature changes, but brings its cold characteristics 3. Boundary between air masses called front B. Source regions indicated by simple code tells you what air mass is like 1. Polar vs. Tropical: a. Designation of temperature b. capital P and capital T after the little letter 1) P: cold polar, from high latitudes 2) T: warm tropical, from low latitudes 2. maritime vs. continental: a. designation of moisture content b. little m and little c at beginning of symbol 1) m: moist maritime: from sea 2) c: dry continental: from land C. Weather due to movement of air masses 1. Lake Effect snow due to movement of continental polar air mass a. cold air moves over Great Lakes b. acquires warmth and moisture from water of lakes c. moves over cold land, and snow result of cooling of moist air 2. Maritime tropical air from Gulf of Mexico, Caribbean Sea, Equatorial Atlantic Ocean a. Warm, moist, unstable air moves onto North America in summer b. High temperature, humidity, most of rainfall of eastern 2/3 of continent 3. few continental tropical air masses affect North America 4. maritime polar air masses a. often originate as Siberian continental polar air masses 1) gain moisture on travel across Pacific Ocean 2) orographic uplift results in precipitation in intermountain west b. Nor easters are also maritime polar air masses IX. Fronts the not-mixing of air masses A. narrow bands between contrasts of temperature and moisture B. slope at low angle, with warmer air above cooler air C. named for type of air that is displacing the type present: idealized descriptions follow, actual weather associated with a front may vary 1. warm fronts bring warm air a. warm air rides over cold air in place 1) ground friction inhibits movement of cold air in place 2) difficult to move out of the way b. gently sloping wedge of cold air carries warm air aloft 1) 1:200 common 1 km up for 200 km ground distance 2) adiabatic cooling creates clouds and precipitation a) sequence of clouds associated with approaching warm front b) cirrus to cirrostratus to alto stratus to nimbostratus

5 c) light to moderate precipitation common with warm fronts c. shift in wind direction commonly indicates passage of front d. designated with red lines and half-circles on advancing side 2. cold fronts force warm air present to ascend a. steeper angle of front created by pushing warm air up 1:100 b. cold fronts advance faster than warm fronts c. more active weather associated with cold fronts 1) heavy downpours 2) strong winds, gusty d. designated with blue line and triangles on advancing side 3. occluded fronts a. when cold front catches warm front b. result is sudden uplift of all of the warm air present c. dissipates due to lack of more warm air to lift

6 X. Mid-latitude Cyclone 30 O to 60 O latitude A. Large centers of low pressure moving in the westerly wind belt 1. circulation inward around low pressure 2. generally contain a cold front and a warm front, extending from the center of the low pressure, toward the outward edge 3. convergence toward center of low, and frontal lifting create weather associated with mid-latitude cyclones B. Life cycle generally lasts a week or two 1. development well predicted by air mass interaction model 2. initial clash of unlike air masses, a. traveling in opposite direction along front b. wave develops along front due to irregularities present 3. wave changes surface air flow, pressure patterns a. Low pressure situated at the apex of the wave b. result in nearly circular isobars cyclonic flow! c. Uplift and precipitation created by 1) Convergence toward low pressure 2) Frontal development along unlike air masses 4. cold front moves faster than warm front catches it! a. Occlusion begins as this starts to occur, from low pressure outward b. Intensifies storm as this step is initiated c. Forcing all warm air aloft ends mid-latitude cyclone C. Passage of a mid-latitude cyclone see figure in book 1. point A a. cirrus clouds when front is 1000 km away, pressure falling b hours later, light rain begins, temperature rises, wind shifts 2. point C and D a. starts with warm southwesterly breezes b. replaced by cooler gusty west or northwest winds c. precipitation along cold front wind shift as it passes 3. point F and G a. greatest intensity of storm b. temperatures remain cold at surface c. passage of warm air aloft results in storminess D. Airflow aloft relation to cyclone-anticyclone systems 1. maintains the persistence of the cyclones and anticyclones 2. divergence aloft keeps cyclone from filling and dissipating 3. surface air from anticyclone feeds cyclone 4. convergence aloft maintains anticyclone

7 XI. Cyclone A. Circulating storm system B. Alternative meanings 1. hurricane (Most cyclones are not hurricanes) a. Hurricane: defined by wind speed, area of origination b. Smaller than mid-latitude cyclones (typically 600 km across) c. Often have greater pressure differences from center to edge 2. tornado a. small (1/4 km), extremely violent cyclones b. extreme pressure gradient creates incredible wind speeds XII. Thunderstorms A. Occurrence 1. clouds of vertical development created by absolute or conditional instability a. single cumulonimbus cloud, or clusters over large area b. within tropical maritime air masses that have moved into continent, lifted by daytime heating, often shortlived c. orographic or frontal lifting of warm moist air makes larger set 2. characteristics a. must have thunder and lightning b. commonly has gusty winds, intense rainfall, hail c. may also have microburst or tornado development 3. statistics a thunderstorms in progress at any time b. there are 6000 lightning strikes/min. worldwide c. Florida has most thunderstorms per year in US B. Development need uplift of warm, moist air 1. latent heat released with condensation creates unstable conditions 2. cumulus stage commonly produced by daytime heating 3. mature stage reached with unstable conditions leading to cooling a. adiabatic expansion cools air b. reaches dew-point temperature, but continues to rise c. requires there to be condensation for continued cooling d. downdrafts associated with consequent rainfall 4. dissipation stage reached when downdrafts dominate, surface is cooled by rainfall/hail C. Lightning safety considerations 1. fully enclosed vehicles with windows closed conduct electricity around them rubber tires not significant insulation from ground 2. get away from high or exposed places a. open fields, peaks, lakes isolated trees b. towers, metal fences, flagpoles, open vehicles 3. do not use electrical or plumbing fixtures inside during lighting storms a. telephone, light switches, cable TV connections b. faucets, shower 4. If you can hear it or see it, take action! a. don t wait for rainfall b. don t go out too soon it can get you after it passes

8 XIII. Tornadoes local storm of short duration associated with thunderstorms A. Characteristics 1. large pressure drop (to 10%) over short distance (250 m) results in extreme pressure gradient 2. creates extreme wind speeds (can be over 450 km/hr!!) 3. wind spirals inward, convergent lifting into parent thunderstorm 4. many have multiple suction vortices circulating around central core B. Occurrence 1. most thunderstorms do not produce tornadoes a. tornado development favored if thunderstorm complex becomes a mesocyclone vertical cylinder of rotation 3-10 km across b. tornadoes associated with hurricanes, strong cold fronts 2. atmospheric conditions a. commonly at cold front of a mid-latitude cyclone b. contrasting air masses in central US in springtime 1) continental polar air meets maritime tropical air 2) few topographic barriers to keep them apart 3. climatology a. average 1200/year in US b. most occur from April to June, but can happen in any month C. Development 1. characteristics a. wind speeds within tornado estimated up to 500 km/hr b. 150 to 600 m across c. Travels at average 45 km/hr across landscape 1) Ahead of cold front so 2) usually from SW toward NE d. Cuts path of about 10 km long for documented tornadoes 1) Most are weak, shortlived 2) Occasional ones cause devastation in 1 km path for 150 km 2. destruction a. Fujita intensity scale determined by damage of strong winds b. Winds cause damage, flying debris causes injuries 3. forecasting a. important because of potential destruction and injury 1) difficult because of minute size in large weather system 2) forecast of severe thunderstorms can be up to a day ahead b. watches and warnings 1) watch alerts people to possibility 2) warning issued when tornado has been sighted, or is indicated on radar, indicates direction and speed of tornado c. Doppler radar can detect motion of mesocyclone its circulation! 1) Sharp gradients of wind speeds can be seen 2) Crescent shape in wind speed plot indicates likely tornado

9 XIV. Hurricanes tropical cyclones, typhoons A. Characteristics 1. form between 5 and 20 O of equator, most in Pacific, north of equator 2. wind speed greater than 119 km/hr 3. average 600 km across, 12 km high into atmosphere (base of stratosphere) 4. pressure drop from edge to center commonly 50 millibars (1.5 in Hg) a. pressure gradient results in high wind speeds b. convergence creates uplift 5. components a. eye wall of cumulonimbus towering clouds 1) greatest wind speeds at eye wall 2) heaviest rainfall from towering cumulonimbus there b. circular shaped eye in center 1) nearly windless 2) weakly subsiding air not strong enough to be cloudless c. trailing bands of cumulonimbus around eye wall B. Development 1. high water temperatures in tropical ocean fuels formation a. uplift creates inflow, Coriolis effect creates circulation b. Cannot form within 5 O of equator, because Coriolis is too weak 2. tropical disturbances organize with rotation a. release of latent heat warms storm system, enhances uplift b. pressure drop at center creates pressure gradient 1) increases wind speeds 2) brings fuel : warm moist air that will lift c. divergence at top of storm enhances inflow at surface 3. wind speed determines what the disturbance is a. tropical depression: less than 61 km/hr b. +61 km/hr=tropical storm get a name at this point c km/hr designated hurricane 4. movement of storm causes it to gain or lose strength a. over land or cooler water loses energy source: diminishes b. over warm water intensifies C. Destruction 1. loss of life has been minimized by excellent forecasting 2. property damage has been rising: greater development in coastal areas 3. causes of destruction a. storm surge 2-3 m above tide level 1) most common cause of property damage and death 2) created by intense low pressure, and wind push of water 3) greater impact if storm has landfall at high tide b. wind damage 1) greater area affected than storm surge 2) poorly built structures, flying debris 3) some tornadoes imbedded in hurricanes c. inland flooding 100s of km from storm center 1) several inches of rain even after winds subside 2) outlying areas actually may benefit from rainfall