The purpose of this seminar is to emphasise the ... · MOUNTAIN FLYING As compared to flatland...
Transcript of The purpose of this seminar is to emphasise the ... · MOUNTAIN FLYING As compared to flatland...
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MOUNTAIN FLYINGMOUNTAIN FLYING
As compared to flatland soaringAs compared to flatland soaring
The purpose of this seminar is to emphasise The purpose of this seminar is to emphasise the differences between these two flight the differences between these two flight
styles and environmentsstyles and environments
The seminar is especially directed to the The seminar is especially directed to the Junior Pilots, coming to Junior Pilots, coming to RietiRieti for the Jfor the J--WGC of WGC of
20072007
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Main differencesMain differences
• The influence of the territory• Typical mountain soaring conditions• Turbulence, and strong sink• Better lookout - improving airspace scanning techniques
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The influence of the territoryThe influence of the territoryThe pilot must:
• Maintain the ridge well in sight• Constantly re-assess its distance from the ridge• Safely assess the intensity of turbulence• Scan the airspace effectively for other (glider) traffic and
fixed obstacles (wires, cables)• Specifically plan your flight• Be well-rested, trained and current
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The influence of the territoryThe influence of the territory
General Rules - The pilot must:• Have flown with a mountain-flying instructor• Maintain higher flight speeds• Keep excellent look-out• Always prepare himself with a good pre-flight briefing (or
self-briefing), not only in contests• Gradually explore the territory• Study every landable area and fields, before the flight• Plan the following phases of the flight during every climb• Have the necessary and correct equipment/accessories
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Typical mountain soaring conditionsTypical mountain soaring conditions
• Ridge lift• Thermal ridge lift• Thermodynamic lift• Convergence, cloud streets in alpine territory• Valley breezes• Sea breezes and the influence of mountain ranges• Lee-side thermals• Thermal-wave inside the valleys• Wave flying
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Ridge LiftRidge LiftRequirement: wind
Flying technique
- Speed higher than E-max (Best Glide Speed)- Correct “figure 8” turns- Exploiting the most energetic height-band- Adjust distance from the ridge accordingly to steepness
of the ridge- Placing the glider in the correct position over the ridge
line
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Ridge LiftRidge Lift
+1
+2
+3
+1
windacceleration of the wind
Working height band
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Ridge LiftRidge Lift
Warnings- Wind gets stronger at the top of the ridge- Look-out for cables and other obstacles- Other gliders do fly on the same or opposite heading- Always remember the basic rules for ridge flying:
a) right of wayb) overtakingc) turns: always turn away from the ridged) safe distance from the ridge
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Thermal Ridge LiftThermal Ridge Lift
Features:
Super-adiabatic gradientWhere to look for thermalsThe tephigram and the thermal trigger pointsThermals start from different places during different times
of the day (position of the sun)
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Thermal Ridge LiftThermal Ridge Lift
Warnings
• Turbulence and strong sink; even worse when the inversion is close or below the top of the ridge
• Don’t progress into unknown, or dead-end valleys; avoid high plateaux
• Stalls can happen suddenly, much more frequently than over flatland. Keep safe flying speeds
• “Figure 8” turns until over the ridge top• Keep excellent rudder/stick co-ordination
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Thermal ridge soaringsun
from 9 to 10 p.m.
Inversione Inversione notturna di valleNight valley inversion
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solesune sole
inversione
Thermal ridge
Dopo after 12 a.m. approx.
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Lift from ridge foot late afternoon
Lift from the valley late afternoon
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Thermodynamic liftThermodynamic lift
Requirements and features:
• The ridge surface must be exposed to the wind and sun at the same time
• The stronger the wind, the more ridge-flying techniques apply
• The weaker the wind, the more thermal-flying techniques apply
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wind
sun
20/25 km/h
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When and where make 8 turns or spirals
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Thermodynamic liftThermodynamic lift
Warnings
• Climb to a higher level before crossing a gap• Beware of wave resonance phenomena• Same rules as per Thermal mountain-flying, even higher
importance for flying “8” instead of circles
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Cloud StreetsCloud StreetsHow and where:• Thermodynamic lift, good gradient up to condensation
altitude, an inversion just above• Convergence of air masses• In the mountains, cloud streets are rectangular to the
wind direction (in the flatland, parallel to wind)• Cloud streets are stationary in alpine territory (in the
flatland, they drift along with the wind)
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SeaSea--breezesbreezes
How and where:
• Synoptic wind and the breeze: opposite directions
• High surface temperatures in the continental side
• Mountain ranges allow for easier soaring exploitation
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SeaSea--breezesbreezes
Exploiting Sea-breeze fronts
• Easy to see and recognise• Using the optimum height-band• Turbulence can be challenging at lower altitudes;
dangerous when in close proximity to other gliders
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LeeLee--side Thermalsside Thermals
• The Lee-side face is exposed to the sun• The thin boundary layer is overheated• Rotors, in the lee-side, are a different thing from
thermals• Sun-heated ridge faces generate a breeze which
opposes the synoptic wind• Lee thermals can drift with the wind, after a while;
seldom they are linked to a feature on the ground• The need for an outlanding may arise very quickly;
plan and be aware of landing opportunities
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Lee-side thermals
wind
breaze
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ThermalThermal--WaveWave
Lee Thermal-WaveOften get their origin from Lee-side Thermals, together with weak waves in the upper layers
• Identifying the optimum distance from the ridge• Not good for huge height gains, but excellent for long runs without height-loss• Generally turbulence-free
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ThermalThermal--WaveWave
Wind 20/25 km/h
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ThermalThermal--WaveWave(Windward Thermal-Wave)
•On the face of cumuli exposed to the wind, and to the sun•Transition from thermal below cloud-base, to wave, is tricky•The correct technique
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Windword thermal wave
+ 2 m/s
+ 1 m/s
wind
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Wave FlyingWave Flying
Prerequisites for the generation of waves- Wind direction relative to the mountain range/ridge- Wind speed gradient- Tephigram
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Rotors and lenticulars clouds
Increase of wind speed
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Wave FlyingWave Flying
Warningsa) the pilot can suffer from:- Hypoxia and its effects- Low temperatures- Reduction of his judgement/abilities- Effects of the strong winds- Setting of the sunb) the glider can be damaged:- Overspeeding (Vne, Va, Vra, altitude)- Cracks in the gelcoat
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THE ENDTHE END