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Aviation Meteorology FAA estimates than 50% of aircraft accident are weather related Substantial implications of weather Cancellations Delays Extra fuel.

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Presentation on theme: "Aviation Meteorology FAA estimates than 50% of aircraft accident are weather related Substantial implications of weather Cancellations Delays Extra fuel."— Presentation transcript:

1 Aviation Meteorology FAA estimates than 50% of aircraft accident are weather related Substantial implications of weather Cancellations Delays Extra fuel Controls who can fly

2 Major Aviation Hazards
Icing Turbulence Obstructions to Visibility Wind shear

3 Aircraft Icing Two main failure modes:
Commercial plane taking off in or after snow General aviation plane in terrain

4 Air Florida Flight 90 13 January 1982 78 killed

5 Icing Causes Problems in Many Ways
Increased weight Decreased lift by changing shape of airfoil Increased drag Engine system icing Reduced control of aircraft surfaces Sensor malfunction.

6 Rime Ice

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10 Clear Ice

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12 Frost

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15 NOAA P3 During IMPROVE

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17 Physical Factors Affecting Aircraft Icing
Most icing occurs as aircraft fly through supercooled clouds or freezing rain. Ice crystals (e.g., snow) are not problems—just bounce off aircraft. Major factors include temperature, liquid water content, and droplet size distribution

18 Temperature T < -40C: no supercooled water and no threat
T > 0C, no problem T between 0C and roughly -15C is the big threat range. Few active freezing nuclei in this temperature range Thus, lots of supercooled water, which freeze on contact with airframe.

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20 Intensity of Icing Trace: Perceptible but not hazardous
Light: Accumulation may create a problem under prolonged exposure (> 1hr). Deice occasionally. Moderate: Short encounters are potentially hazardous. Deicing/antiicing mandatory Severe: Deicing/anti-icing equipment is inadequate. Immediate diversion is necessary

21 Liquid Water Content (LWC)
Probably the most important factor in determining ice accumulation rate. In general, MUCH greater in cumuloform than stratiform clouds. Generally highest at higher portion of clouds.

22 Droplet Size Distribution
Small particles are collected less effectively. Why? They tend to follow the airstream that is deviated by the aircraft. Large droplets have so much momentum that have a great tendency to hit the plane.

23 Non-Meteorological Factors
Collection efficiency of aircraft Radius of curvature is important Sharp, narrow structures have more collection Aerodynamics heating Adiabatic compression and friction Very slow aircraft ~ 1F Supersonic at low altitude ~50F!

24 Aicraft Icing by Meteorological Situation
Low-mid stratiform (stratus, stratocumulus) Convective-cumuloform Cirrus Warm fronts Cold fronts Orographic clouds Freezing Rain

25 Freezing Rain

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27 Portland is well known for freezing rain

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30 Pilot Reports (PIREPS)

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32 Available at AWC

33 Some Planes Have Deicing Equipment: Icing Boots and Heating

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36 Greater Emphasis on Deicing at Airports

37 Turbulence: Five Types
Mechanical turbulence Convective turbulence Shear-induced turbulence Wave-related turbulence Wake turbulence

38 Turbulence Intensity Light: Acceleration < 1 g
Moderate: Acc. .5 to 1 g Severe: Acc > 1 g Extreme: Loss of control of plane

39 Turbulence Levels

40 Wind Shear Induced Turbulence
Occurs when winds changes rapidly with height. Often associated with frontal zones, upper fronts, jet stream flanks, sharp troughs Most associated with Kelvin-Helmholtz Instability (KHI) KHI develops in stably stratified flow when the shear exceeds a certain threshold.

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44 Some Videos https://www.youtube.com/watch?v=ELaZ2x42dkU

45 Richardson Number (RI)

46 Some Preferred Locations for shear-induced turbulence above the BL
Upper trough on cold side of jet Along jet north and northeast of developing low Above and below midlatitude jet core Shear-induced turbulence is not necessarily in cloud. Called Clear Air Turbulence (CAT).

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50 Richardson Number Theoretical studies and observations suggest Ri needs to get to .25 or below for instability You need some stability to allow the build up of shear for instability (rubber band analog)

51 Low-level shear turbulence: eastern WA example
Cold air near surface in basin Warmer air above, with inversion in betwee Strong winds in warm air, weak winds in cold air The result is a small Ri and turbulence at low levels (e.g., Tri-Cities)

52 Predicting Shear Induced Turbulence
Models provide winds and temperature fields. Can calculate RI Also “rules of thumb” > 4 knots per 1000 ft: potential for light turbulence >6 knots per 1000 ft: potential for moderate to severe turbulence.

53 Shear-Induced Turbulence Guidance

54 Shear Induced Turbulence
Often patchy… ascending or descending a few thousand feet can get you out of it. That is pilots sometimes “test altitudes” or get “ride reports” from FAA controllers, and request new altitudes.

55 Wake Turbulence Largest behind large planes
A major reason for separation rules. Biggest problem on runway, but can have impact aloft when cross recent flight path.

56 Aircraft Wake Turbulence

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58 Movie

59 Boeing Field 59

60 Wave-related turbulence
Associated with the breakdown of gravity waves, particularly waves created by mountains (mountain waves). Convection can also produce gravity waves Gravity waves can produce up to severe turbulence for all levels of the troposphere and stratosphere.

61 Low-Level Wind Shear Associated with Gust Fronts, Downbursts (Microbursts and Macrobursts)

62 Downbursts

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64 Downbursts can be Divided into Two Main Types
MACROBURST: A large downburst with its outburst winds extending greater than 2.5 miles horizontal dimension. Damaging winds, lasting 5 to 30 minutes, could be as high as 134 mph. MICROBURST: A small downburst with its outburst, damaging winds extending 2.5 miles or less. In spite of its small horizontal scale, an intense microburst could induce damaging winds as high as 168 mph.

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67 Wet microburst photo taken by Bill Bunting. A series of three sides.
Downburst Hazards. Downburst winds can exceed 100 mph and are capable of doing the same damage as a weak to strong tornado. Rapidly shifting wind direction and changes in visibility pose problems to mobile spotters. 67

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69 Strongest winds occur in the curl.
Heavy rains and flooding are likely when you see something like this. Don’t drive your vehicle into something like this. 69

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73 Downbursts Microburst Dry Microburst Wet Microburst
Damaging winds less than 2.5 miles in diameter Accompanied by little or no rainfall Wet Microburst Damaging winds less than 2.5 miles in diameter Accompanied by very heavy rainfall and perhaps hail 73

74 Downburst Video http://www.youtube.com/watch?v=TkavH9aZue8

75 Extremely Dangerous For Aircraft Landing and Taking Off

76 Research by NCAR and collaborators in the 1980s uncovered the deadly one-two punch of microbursts: aircraft level off when they encounter headwinds, then find themselves pushed to the ground by intense downdrafts and tailwinds. 76

77 Eastern Airlines Flight 66 Pan Am Flight 759 Delta Airlines Flight 191
The following are some fatal crashes that have been attributed to windshear/ microbursts in the vicinity of airports: Eastern Airlines Flight 66 Pan Am Flight 759 Delta Airlines Flight 191 USAir Flight 1016 77

78 Eastern Air Lines 66 June 24, 1975 New York – Kennedy Airport
112 killed 12 injured Crashed while landing Boeing 727 78

79 Pan Am 759 July 9, 1982 New Orleans Airport 145 passenger/crew killed
8 on ground killed Crashed after takeoff Boeing 727 79

80 Delta 191 August 2, 1985 Dallas-Fort Worth Airport Crashed on landing
8 of 11 crew members and 128 of the 152 passengers killed, 1 person on ground killed Lockheed L-1011 80

81 USAir 1016 July 2, 1994 Charlotte/Douglas Airport Crashed on landing
37 killed 25 injured McDonnell Douglas DC-9 81

82 August 1, 1983 the strongest microburst recorded at an airport was
observed at Andrews Air Force Base in Washington DC. The wind speeds may have exceeded 150 mph in this microburst. The peak gust was recorded at 211 PM – 7 minutes after Air Force One, with the President on board, landed on the same runway. 82

83 the pilot experiences a headwind and increased aircraft performance
During take-offs the pilot experiences a headwind and increased aircraft performance followed by a short period of decreased headwind a downdraft and finally a strong tailwind 83

84 the airplane begins the descent flying into a strong headwind
During landings the airplane begins the descent flying into a strong headwind a downdraft and finally a strong tailwind represents the extreme situation just prior to impact 84

85 Macroburst Wisconsin on the 4th of July, 1977, with winds that were estimated to exceed 115 mph, and completely flattening thousands of acres of forest Microburst 85

86 Joint Airport Weather Studies (JAWS)
Major research effort between FAA and NCAR during the 1980s to understand and find ways of dealing with downbursts. Centered at Stapelton Airport in Denver Once the phenomenon was understood, proposed solution to allow warnings: terminal doppler radars and LLWAS.

87 The Terminal Doppler Weather Radar (TDWR) is now deployed at 44 major airports. The TDWR mission is to provide wind shear detection services to air traffic controllers and supervisors

88 Low Level Windshear Alert System (LLWAS)

89 LLWAS In 1983, the FAA asked NCAR to develop a version of LLWAS that could detect microbursts. Between 1983 and 1988, NCAR developed and tested a new LLWAS system that detected microbursts, determined the strength in terms of headwind/tailwind gains or and located the event (on the runway, at 1, 2, or 3 nm on departure or arrival). This system was later improved and is now called the Phase-3 LLWAS. A typical Phase-3 LLWAS will have enough sensors to be spaced 2-km apart (~1 nm apart) and cover out to 2 nm from the end of each major runway. The largest LLWAS is at Denver International Airport. It has 32 wind sensors. Most Phase-3 systems have between 12 and 16 wind sensors.

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91 Microburst “Season & Time”
The four best known downburst aviation disasters in the U.S. happened in the summer. (1 in June, 2 in July, 1 in August) All four happened in the late afternoon or early evening (from 4:05 to 7:43 local time)

92 Still not there The threat of wind shear has been reduced but not eliminated. It was mentioned in an average of 25 National Transportation Safety Board accidents and incident reports a year from 1983 through But the vast majority of cases were nonfatal and mostly involved general aviation.


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