remote sensing of mesoscale vortices in hurricane eyewalls
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Remote Sensing of Mesoscale Vortices in Hurricane Eyewalls. Presented by: Chris Castellano Brian Cerruti Stephen Garbarino. Abstract. A phenomena observed only by remote sensing and new high resolution technology - PowerPoint PPT PresentationTRANSCRIPT
Remote Sensing of Remote Sensing of Mesoscale Vortices in Mesoscale Vortices in Hurricane EyewallsHurricane Eyewalls
Presented by:Presented by:Chris CastellanoChris Castellano
Brian CerrutiBrian CerrutiStephen GarbarinoStephen Garbarino
AbstractAbstract• A phenomena observed only by remote A phenomena observed only by remote
sensing and new high resolution sensing and new high resolution technology technology
• Important to observe because they may Important to observe because they may play a significant role in the dynamics of play a significant role in the dynamics of the inner structures of hurricanesthe inner structures of hurricanes
• Without remote sensing instruments like Without remote sensing instruments like MODIS, AVHRR, and NEXRAD mesoscale MODIS, AVHRR, and NEXRAD mesoscale vortices would remain undetected. vortices would remain undetected.
OverviewOverview• PlatformsPlatforms
– TERRA/AQUATERRA/AQUA– NOAA 15,16,17NOAA 15,16,17– WSR-88D UnitsWSR-88D Units
• SensorsSensors– MODISMODIS– AVHRRAVHRR– NEXRAD NEXRAD
• ProductsProducts
PlatformsPlatforms• TERRA/AQUATERRA/AQUA
• NOAA 15, 16, 17 NOAA 15, 16, 17
• WSR-88DWSR-88D
TERRA Satellite (EOS-AM1)TERRA Satellite (EOS-AM1)• Multinational, multidiscipline missionMultinational, multidiscipline mission• Managed by NASA with partners in Managed by NASA with partners in
Canada and JapanCanada and Japan• Planned 15 year data set to be Planned 15 year data set to be
collected; began in February 2000collected; began in February 2000• Sun SynchronousSun Synchronous
TERRA ContinuedTERRA Continued• Descending time: Descending time:
10:30am10:30am• Ascending time: Ascending time:
1:30pm1:30pm• Dimensions: 5.99 x Dimensions: 5.99 x
1.7 x 2.0 meters1.7 x 2.0 meters• Weight: 5190kgWeight: 5190kg• Power: 2530 W on Power: 2530 W on
averageaverage
MODISMOPITT
CERES MISR ASTER
AQUA Satellite (EOS-PM1)AQUA Satellite (EOS-PM1)• Launched to collect data about the Launched to collect data about the
earths water cycleearths water cycle• Shares some of the same Shares some of the same
instruments in its payload as TERRA instruments in its payload as TERRA satellite satellite
• First of the “Afternoon” Satellites First of the “Afternoon” Satellites • Also uses a sun synchronous orbitAlso uses a sun synchronous orbit
AQUA ContinuedAQUA Continued• Descending time: Descending time:
1:30pm1:30pm• Ascending time: Ascending time:
10:30am 10:30am • Dimensions: 4.8 x 16.7 Dimensions: 4.8 x 16.7
x 8 metersx 8 meters• Mission Life: 6 yearsMission Life: 6 years• Weight: 2,934 kgWeight: 2,934 kg• Power: 4,860 W on Power: 4,860 W on
averageaverage
NOAA 15NOAA 15• Launched: May 1998Launched: May 1998• Operational Status: AM secondaryOperational Status: AM secondary• Altitude: 807 kmAltitude: 807 km• Inclination: 98.5 degreesInclination: 98.5 degrees• Period: 100.1 minutesPeriod: 100.1 minutes• Carries a variety of instruments Carries a variety of instruments
including AVHRRincluding AVHRR
NOAA 16NOAA 16• Launched: September 2000Launched: September 2000• Operational Status: PM secondaryOperational Status: PM secondary• Altitude: 849 kmAltitude: 849 km• Inclination: 99 degreesInclination: 99 degrees• Period: 102.1 minutesPeriod: 102.1 minutes• All instruments on NOAA 15 plus one All instruments on NOAA 15 plus one
additional instrumentadditional instrument
NOAA 17NOAA 17• Launched: June 2002Launched: June 2002• Operational Status: AM backupOperational Status: AM backup• Altitude: 810 kmAltitude: 810 km• Inclination: 98.7 degreesInclination: 98.7 degrees• Period: 101.2 minutesPeriod: 101.2 minutes• All instruments on NOAA 16All instruments on NOAA 16
NOAA 15 NOAA 15 Before Before LaunchLaunch
WSR-88D WSR-88D • Weather Surveillance Weather Surveillance
Radar 1988 DopplerRadar 1988 Doppler• Detects precipitation Detects precipitation
and atmospheric and atmospheric movement (wind)movement (wind)
• Three modesThree modes– Clear air mode (slow Clear air mode (slow
scanning)scanning)– Precipitation mode Precipitation mode
(faster scanning)(faster scanning)– Severe weather mode Severe weather mode
(very fast scanning)(very fast scanning)
SensorsSensors• MODISMODIS
– TERRA and AQUA SatellitesTERRA and AQUA Satellites• AVHRRAVHRR
– NOAA 15, 16, 17 SatellitesNOAA 15, 16, 17 Satellites• NEXRAD NEXRAD
– WSR-88D UnitsWSR-88D Units
MODISMODIS• Moderate Resolution Imaging Moderate Resolution Imaging
Spectroradiometer Spectroradiometer • On board both the Terra (am) and On board both the Terra (am) and
Aqua (pm) satellitesAqua (pm) satellites• Provides high resolution radiometric Provides high resolution radiometric
sensitivitysensitivity• Global coverage every 1-2 daysGlobal coverage every 1-2 days
MODIS continuedMODIS continued• Range: 0.4um to 14.4umRange: 0.4um to 14.4um• 36 spectral bands36 spectral bands
– 2 have Nadir Resolution: 250 m2 have Nadir Resolution: 250 m– 5 have 500 m resolution5 have 500 m resolution– Rest have 1km resolutionRest have 1km resolution
• +- 5 degrees scanning pattern+- 5 degrees scanning pattern• Altitude: 705 kmAltitude: 705 km• Achieves 2,330 km swathAchieves 2,330 km swath
MODIS continuedMODIS continued• Uses a whiskbroom scanning method to Uses a whiskbroom scanning method to
collect datacollect data• The optical system uses a two mirror off-The optical system uses a two mirror off-
axis a-focal telescopeaxis a-focal telescope– Directs energy to 4 refractive objective Directs energy to 4 refractive objective
assemblies assemblies – One for each One for each
• VisVis• NIRNIR• SW/MW IRSW/MW IR• LW IRLW IR
MODIS continuedMODIS continued• Uses a photodiode-Uses a photodiode-
silicon technology silicon technology for visible and NIR for visible and NIR to reduce noiseto reduce noise
• Has 4 on board Has 4 on board calibrators as well calibrators as well as a view to space as a view to space to keep the to keep the measurements measurements accurateaccurate
MODIS ImageryMODIS Imagery• Hurricane IsabelHurricane Isabel• Visible bandVisible band• 13 September 13 September
20032003
MODIS ImageryMODIS Imagery• Hurricane KatrinaHurricane Katrina• Terra SatelliteTerra Satellite• 28 August 200528 August 2005
MODIS ImageryMODIS Imagery• Hurricane WilmaHurricane Wilma• 21 October 200521 October 2005
AVHRRAVHRR• Advance very high resolution radiometerAdvance very high resolution radiometer• Used to remotely determine cloud cover Used to remotely determine cloud cover
and “surface temperature”and “surface temperature”• Whiskbroom scannerWhiskbroom scanner• At 833km the IFOV 1.1 x 1.1km at nadirAt 833km the IFOV 1.1 x 1.1km at nadir• 4 site revisitations per day4 site revisitations per day• 6 different channels6 different channels
AVHRR continuedAVHRR continuedAVHRR Channel Characteristics
Channel Number Resolution at
Nadir Wavelengt
h (um) Typical Use
1 1.09 km 0.58 - 0.68 Daytime cloud and
surface mapping
2 1.09 km 0.725 -
1.00 Land-water boundaries
3A 1.09 km 1.58 - 1.64 Snow and ice detection
3B 1.09 km 3.55 - 3.93 Night cloud mapping, sea
surface temperature
4 1.09 km 10.30 -
11.30 Night cloud mapping, sea
surface temperature
5 1.09 km 11.50 -
12.50 Sea surface temperature
AVHRR ImageryAVHRR Imagery• Hurricane KatrinaHurricane Katrina• NOAA-15NOAA-15• 28 August 200528 August 2005
AVHRR ImageryAVHRR Imagery• Hurricane IsabelHurricane Isabel• NOAA-15NOAA-15• 15 September 15 September
20032003
AVHRR ImageryAVHRR Imagery• Hurricane DeanHurricane Dean• NOAA-16NOAA-16• 20 August 200720 August 2007
NEXRADNEXRAD• Determines location and intensity of Determines location and intensity of
precipitation, wind speed to/from the precipitation, wind speed to/from the radar site, as well as several other radar site, as well as several other products (VIL, storm tracks, etc.)products (VIL, storm tracks, etc.)
• 16 tilts (data levels ) are available16 tilts (data levels ) are available• .6 x .6 miles resolution out to 143 .6 x .6 miles resolution out to 143
miles for base reflectivity at 0.5 miles for base reflectivity at 0.5 degrees (tilt 1)degrees (tilt 1)
NEXRAD continuedNEXRAD continued• Clear air modeClear air mode
– 5 elevation angles5 elevation angles• Precipitation modePrecipitation mode
– 9 elevation angles9 elevation angles• Severe weather modeSevere weather mode
– 14 elevation angles14 elevation angles– Sub-mode of precipitation mode, not Sub-mode of precipitation mode, not
regularly delineated from itregularly delineated from it
NEXRAD continuedNEXRAD continued• How does radar work?How does radar work?
– Creates EM pulse focused by an antenna Creates EM pulse focused by an antenna transmitted through the atmospheretransmitted through the atmosphere
– Objects within range scatter and reflect the Objects within range scatter and reflect the energy energy
– Energy returning to the radar is called an Energy returning to the radar is called an echoecho
– Large target = stronger echo (hail)Large target = stronger echo (hail)– Many targets = stronger echo (heavy Many targets = stronger echo (heavy
precip)precip)
NEXRAD continuedNEXRAD continued
NEXRAD continuedNEXRAD continued
NEXRAD continuedNEXRAD continued• What is important for our use?What is important for our use?
– Base Radial VelocityBase Radial Velocity•Measurement of movement of particles Measurement of movement of particles
to/from radarto/from radar– Storm Relative Radial Velocity Storm Relative Radial Velocity
•4 tilts, storm motion is subtracted from the 4 tilts, storm motion is subtracted from the base radial velocitybase radial velocity
NEXRAD ImageryNEXRAD Imagery
NEXRANEXRAD D ImagerImageryy
SummarySummary• PlatformsPlatforms
– TERRA/AQUATERRA/AQUA– NOAA 15,16,17NOAA 15,16,17– WSR-88D UnitsWSR-88D Units
• SensorsSensors– MODISMODIS– AVHRRAVHRR– NEXRAD NEXRAD
• ProductsProducts
Questions?Questions?
…sometimes you don't need a …sometimes you don't need a satellite…satellite…
International Space StationSept 13, 2003