Title: Aviation and Marine Applications
1Aviation and Marine Applications
- COMET Satellite Meteorology
- Gary Ellrod (NOAA/NESDIS)
- Camp Springs, Maryland
SatMet 99-2 Thursday, 29 April 1999
2Aviation/Marine Outline
- Aviation
- Stratus and fog
- Aircraft icing
- Jet streams / Clear Air Turbulence (CAT)
- Mountain waves
- Microbursts / gust fronts
- Marine
- Sea fog
- Oceanic convection
- Surface winds / cyclones
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6Is it fog or Sc/Ac?
- Fog looks smoother
- Sc/Ac is mottled
- Fog is brighter (if depth equal)
- Fog has distinct edges
- Higher clouds may have shadows
- Fog is warmer in CH4 IR (10.7 mm)
- Fog moves/develops more slowly
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8 Resolution vs Fog Detection
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11Meteorological Factors Conducive to Icing
- Temperature (0 to -20C)
- Liquid Phase (supercooled droplets)
- Large drop sizes (gt50 mm)
- High Liquid Water Content (gt0.25 gm-3)
- Weak vertical motion (1 mbar s-1)
- Embedded convection
- Large areal extent
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13GOES Channels Useful in Icing Detection
- Visible (0.6 mm)
- Thickness, coverage, phase, convection
- IR2 (3.9 mm)
- Cloud phase, drop size
- IR4 (10.7 mm)
- Cloud top temperatures, thickness, coverage
- IR5 (12.0 mm)
- Thin cirrus detection
14GOES Icing Risk Product
- Multiple channel screening technique
- Product available hourly day and night
- Strengths
- High POD (70), low FAR
- Good spatial, temporal coverage
- Weaknesses
- Obscuration by high clouds
- No data 2 hr after sunrise / before sunset
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16Turbulence-Generating Mechanisms
- Shear instability along jet and upper fronts
- Flow over obstacles
- Mountains
- Thunderstorms
- Convection (thunderstorms, dry thermals)
- Low level mechanical (strong winds over rough
terrain) - Wake turbulence from other aircraft
17Detection of Turbulence Using Satellite Imagery
- Clear Air Turbulence (CAT)
- Water vapor imagery (8 km)
- Subsidence warming with time along fronts
- Infrared (4 km)
- Transverse cirrus cloud bands
- Deformation zone cloud boundaries
- Visible (1 km)
- Billow wave clouds (K-H instability)
- Mountain waves
- Transverse cloud bands (IR/Vis)
- Lee-of-mountain cirrus with lee gap (IR/WV)
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23Extreme Turbulence Scenario
- Environmental conditions
- Strong jet intersects
- Cold front with
- Low top convection
- Extreme turbulence possible downwind from
convection
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28Pilot Reports - 4 Feb 99/15-18Z
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31Microburst/Downburst Detection with GOES
- Leading Edge (IR) Gradients (LEG) - mirrors
WSR-88D reflectivity gradients - Anvil warming to rear of storm (IR) - evidence of
rear inflow jet - Extensive clouds to rear of gust fronts
- Rapid storm motion
- GOES Sounder products
- WIND Index (WINDEX)
- Dry Microburst Potential (DMPI)
- Max. Theta-e Difference (Sfc-300mb)
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39Hazards of Volcanic Ash
- Reduced engine performance, possible stalls
- Abrasion, pitting of leading edges
- Electrical discharges (St. Elmos fire)
- Ash difficult for pilots to see at night
- Volcanoes in remote areas (North Pacific) where
few alternate airfields available - Height/depth of ash difficult to determine
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42Smoke as an Aviation Hazard
43Marine Applications
- Sea fog
- Oceanic convection
- Cyclones
- Strong wind zones
- Quantitative surface wind data
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46Cloud Streets/ Open Cell Convection
47Gulf Stream Convection
48Strong Wind Zones in Oceanic Cyclones
- Indicators of Rapid Cyclogenesis
- Cloud pattern evolution (leaf to 360o comma in lt
18 hours) - Strong dry slot subsidence (warming in WV)
- Mesoscale Cloud Features
- Closely spaced cloud streets
- Open cell convection / arc lines
- Ring Cloud feature at storm center
- Hooking or sharply-tapered comma head
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51Ring Cloud Thermal Structure
Nieman, et al., 1993
52Ocean Surface Winds from Satellite Data
- IR/Visible Cloud Drift (cloud base motion)
- Passive microwave (SSM/I, AMSU)
- 16v GHz, 22v GHz, 37vh GHz
- Valid at 20 m height upper limit 25 m/sec
- Scatterometer radar (ERS-2)
- Correlates backscattered energy to surface wind
direction and speed - Valid at 10 m height
53ERS-2 Scatterometer Swaths
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