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Research on the impact of mountain waves on general aviation. Deon van der Mescht. Mountain wave definition.
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Research on the impact of mountain waves on general aviation Deon van der Mescht Templ ref: CRS–CC-PRES-TEMP-003.2 Doc Ref no:
Mountain wave definition The American Meteorological Society (AMS) defines a mountain wave as an atmospheric gravity wave which forms in the lee of a mountain barrier as statically stable air passes over the barrier (AMS 2010). Templ ref: PPT-ISO-colour.001 Doc Ref no:
Mountain wave features Templ ref: PPT-ISO-colour.001 Doc Ref no:
General aviation ICAO defines general aviation operation by exception: those flight activities not involving commercial air transportation or aerial work. Templ ref: PPT-ISO-colour.001 Doc Ref no:
List of studies Hex River Mountains 2010 Tsitsikamma Mountains 2018 Tsitsikamma Mountains 2018 (M Geldenhuys) Beaufort West 2019-? Templ ref: PPT-ISO-colour.001 Doc Ref no:
Hex River Mountains Templ ref: PPT-ISO-colour.001 Doc Ref no:
Hex River Mountains Templ ref: PPT-ISO-colour.001 Doc Ref no:
Hex River Mountains Templ ref: PPT-ISO-colour.001 Doc Ref no:
Hex River Mountains Templ ref: PPT-ISO-colour.001 Doc Ref no:
Hex River Mountains Templ ref: PPT-ISO-colour.001 Doc Ref no:
Hex River Mountains Cessna 182 climb rate = 1120 ft/min = 1416ft/min descent rate Reversed flow = turbulence Templ ref: PPT-ISO-colour.001 Doc Ref no:
16 December 2015 • CRASH INSPIRED TWO STUDIES: • Satellite image study • MSc thesis by M Geldenhuys Templ ref: PPT-ISO-colour.001 Doc Ref no:
TSITSIKAMMA MOUNTAINS SATELLITE STUDY Templ ref: PPT-ISO-colour.001 Doc Ref no:
TSITSIKAMMA MOUNTAINS SATELLITE STUDY Templ ref: PPT-ISO-colour.001 Doc Ref no:
TSITSIKAMMA MOUNTAINS SATELLITE STUDY • NEXT STEPS IN STUDY: • COMPARE TO OTHER SUCH EVENTS IN THE PAST • ATTEMP TO CLASSIFY WAVES Templ ref: PPT-ISO-colour.001 Doc Ref no:
TSITSIKAMMA MOUNTAINS SATELLITE STUDY • ARRANGING EVENTS: • COLD FRONTS • CUT-OFF LOWS • RIDGING HIGH PRESSURES Templ ref: PPT-ISO-colour.001 Doc Ref no:
TSITSIKAMMA MOUNTAINS SATELLITE STUDY ARRANGING EVENTS ACCORDING TO POSITION OF WAVES IN RELATION TO ISOLATED PEAKS Templ ref: PPT-ISO-colour.001 Doc Ref no:
TSITSIKAMMA MOUNTAINS MSC THESIS RESULTS: Templ ref: PPT-ISO-colour.001 Doc Ref no:
TSITSIKAMMA MOUNTAINS MSC THESIS RESULTS: Templ ref: PPT-ISO-colour.001 Doc Ref no:
TSITSIKAMMA MOUNTAINS MSC THESIS LARGEST GAP IN THE KAREEDOUW-TSITSIKAMMA MT RANGE Templ ref: PPT-ISO-colour.001 Doc Ref no:
TSITSIKAMMA MOUNTAINS MSC THESIS Templ ref: PPT-ISO-colour.001 Doc Ref no:
TSITSIKAMMA MOUNTAINS MSC THESIS Templ ref: PPT-ISO-colour.001 Doc Ref no:
TSITSIKAMMA MOUNTAINS MSC THESIS Templ ref: PPT-ISO-colour.001 Doc Ref no:
TSITSIKAMMA MOUNTAINS MSC THESIS Templ ref: PPT-ISO-colour.001 Doc Ref no:
TSITSIKAMMA MOUNTAINS MSC THESIS Templ ref: PPT-ISO-colour.001 Doc Ref no:
TSITSIKAMMA MOUNTAINS MSC THESIS Templ ref: PPT-ISO-colour.001 Doc Ref no:
TSITSIKAMMA MOUNTAINS MSC THESIS • RESULTS: • 21m/s wind trough gap flow jet (75.6kph/40kt) • Max 3 visible waves per event (low energy wave events) • Wind increase 15m/s from one side of the mountain to the other at 500m elevation (54kph/29kt) • SEVERE TURBULENCE IN SPITE OF LOW ENERGY WAVES Templ ref: PPT-ISO-colour.001 Doc Ref no: