Meteorology 2 Quiz Wednesday, 18th five slide review first Atmosphere Composition and Properties 10 0 % Atmosphere has weight – 14.7 psi @ sea level or 1013.2 mb – Half of it is below 18,000 feet – No well defined upper surface but satellite drag data indicates some air at 1,000 miles – Gases each contribute to Oxygen 21% atmospheric pressure Water/Other 1% – Water vapour usually less Nitrogen 78% than 1% but can be 3.5% 90% 80% 70% 60% 50% 40% 30% 20% 10 % 0% Vertical Structure THERMOSPHERE IONOSPHERE 3000 ° C @700km MESOPAUSE MESOSPHERE STRATOPAUSE STRATOSPHERE TROPOPAUSE TROPOSPHERE SEA LEVEL KM 120 110 100 Vertical Structure -108 90 275,000 feet 80 70 60 -2.5 165,000 feet 50 40 30 20 36,089 feet 10 0 -110 -100 -90 -80 -70 -60 -56.5 -50 -40 -30 -20 -10 0 10 20 30 40 50 HIGH LOW 2nd low TROUGH COL RIDGE 1000 +/WIND Pressure Areas • Lows move at about 500 miles a day in the summer and faster, about 700 miles a day, in the winter. • Flying from a HI to a LO “LOOK OUT BELOW” H L – LAPSE RATES – RADIATION – TEMPERATURE – TURBULENCE – AIR MASSES – FRONTS – WATER DROPLETS LAPSE RATES LAPSE RATES • • • • • • • • • STANDARD LAPSE RATE 1.98OC DRY ADIABATIC LAPSE RATE 3OC SATURATED ADIABATIC LAPSE RATE 1.5OC SATURATED RANGE ACTUALLY 1.1OC TO 2.8OC STEEP LAPSE RATE SHALLOW LAPSE CONDITIONALLY UNSTABLE – AIR DRY – STABLE CONDITIONALLY UNSTABLE – AIR WET - UNSTABLE POTENTIAL INSTABILITY – AIR MASS ASCENT SHORT RADIATED AS LONG WAVE Pg 2-5 Radiation Absorption & Windows Pg 2-4 Radio Horizon Radio transmissions less than about 10 metres wavelength (VHF, UHF, RADAR) are refracted downward by the atmosphere, roughly a third beyond the distance to the visual horizon. A strong inversion and a significant humidity decrease with height can cause greater refraction. Such a layer is called a radio duct. It is typically 50 to 1,000 feet deep. The bend in the path is just enough for the wave to curve back to the surface, bounce off the earth, and continue on several further bounces. This is known as anomalous propagation. It is not related to the Ionosphere and its influence on radio waves. Page 4-10 Air Command Weather Manual SUN’S PARTICLES and UV RADIATION THERMOSPHERE MESOPAUSE - 108 IONOSPHERE O2 H2 N2 fluoresce 275000 feet MESOSPHERE STRATOPAUSE - 2.5 165000 OZONOSPHERE ABSORBS UV STRATOSPHERE 65000 HENCE TEMP INCREASE HERE DEEP OVER POLES MAY BE THIN OVER EQUATOR 33000 O3 CORROSIVE & HARMFUL - 56.5 SEA LEVEL SEASONAL HEATING HEAT & IT’S MOVEMENT • The atmosphere is heated from below. • Temperature increase decreases density. • Advection: horizontal movement of air. Cold air becomes warmed by the ground as it moves over it • Convection: sun heats ground, ground heats the air • Turbulence: vertical mixing of air due to winds and convection • Compression: air sinks, compresses and heats (Chinooks, highs) AIR IS A HUGE TRANSPORTER OF HEAT BY VIRTUE OF THE MOISTURE EVAPORATED IN IT AS WATER VAPOUR. HEATING the TROPOSPHERE Advection: horizontal movement of air. Cold air becomes warmed (infrared) by the ground as it moves over it CHANGES OF STATE Convection: sun (short wave) heats ground, ground (longer wave) heats the air Turbulence: vertical mixing of air due to winds and convection MECHANICAL TURBULENCE TURBULENCE • Mechanical: Friction between the air and ground causes eddies. Instability in the air aids in turbulence. • Thermal: Convection currents such as those found in storm clouds can be great enough to cause structural failure to some aircraft. • Frontal: Two opposing air masses produce turbulence in the frontal zone. • Wind shear: Any marked changes in wind with height produces local areas of turbulence. • CAT: Clear air turbulence (Jet streams) CLOUD CLASSIFICATION • Turbulence related – stable or unstable • Rain - showers vs. steady • Four families of cloud as below LOW CLOUD 3,000 ASL MIDDLE CLOUD 7,000 ASL MIDDLE CLOUD 11,000 ASL HIGH CLOUD 30,000 ASL Turbulence Levels • Light: slight changes in attitude, slight strain on seat belts. • Moderate: more intense, definite strain • Severe: large abrupt changes in altitude, attitude and airspeed. Occupants forced violently against seatbelts. Mountain Waves L C L R Rapid pressure drop associated over crest of hill Cap clouds, Rotor clouds and Lenticular Clouds Air Masses • An air mass is a large section of the troposphere with uniform temperature and moisture in the horizontal. • Weather in an air mass is determined by: – moisture content – cooling process – stability • Formed over water: Maritime • Formed over land: Continental Air Mass Stability • Weather in an air mass is determined by: – moisture content – saturated or unsaturated adiabatic lapse rate if cooled? – cooling process – various lift types – stability • Cold air mass – usually unstable • Warm air mass – usually stable Air Masses of North America • Continental Arctic: Ca – not in summer; low water content; warmed from below, strong winds produce turbulence; heap clouds and snow showers; rarely in B.C. except as a cold-air invasion • (Continental Polar: Cp) • Maritime Arctic: Ma – starts as Ca that spends some time over the northern Pacific ocean; moist and unstable at high altitudes; stratocumulus and cumulus; pe/sn/-shra; Summer: northern lakes affect air mass • Maritime Polar: Mp – more time spent over Pacific ocean; warmer in lower levels; more stable than Ma; orographic lifting makes rain west of mountains and dry east of mountains; Summer: Tsra/Cb • Maritime Tropical: Mt – very warm and moist; Gulf of Mexico, Caribbean & south of 30°N; Winter: rarely at surface N of Great lakes, but present at high altitudes; unstable when Frontal lift; sn/ra/zr/icing and turbulence; FOG (east coast); Summer: shra/tsra POLAR FRONT Fronts • The transition zone between two air masses is called a front. • Named by the movement of the cold air: – Cold Front: that portion of the front where the cold air is advancing – Warm Front: that portion of the front where the cold air is retreating – Stationary Front: the cold air is neither advancing nor retreating. – Occluded Fronts and Trowals: trough of warm air aloft. The Cold Front • Factors: • • • • • • • Moisture of the warm air mass • stability of the warm air mass • speed and steepness of the frontal surface Wind: Veer, some gusts Temperature: drops Visibility: improves after passage Pressure: approaching front, pressure will drop, then rise after passage Turbulence: usually associated with Cb’s Precipitation: showery in character, usually a narrow band 50 n.m. Cold Warm Cold Front Cold Front The Warm Front • Factors: • • • • • • • • • Moisture Degree of overrunning Wind: Veer Frontal Slope: 1 in 150 to 1 in 200 Temperature: gradual rise Visibility: low ceiling and low visibility; fog Pressure: drop, then rise Turbulence: usually little Precipitation: steady precipitation CI, CS, AS, NS Warm Stability Cold The Warm Front WIND SHEAR @ WARM FRONT FRONTAL WAVE FRONTS FRONTS Warm Colder Cold Warm Colder Cold Warm OCCLUSION or Occluded Front Colder Cold Precipitation • Precipitation occurs when water droplets grow sufficiently in size and weight and then fall due to gravity. – Showery precipitation: Cumulus – Steady precipitation: Stratus • Condensation Nuclei – Smoke, sea salt, etc. Precipitation . Precipitation MOISTURE CONTENT @40OC one cubic metre of air can hold 50 grams of water vapour. One M3 of air weighs about 1.35 kg. This represents about 3.5% by weight. +