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[object Object],[object Object],October 24, 2008 David Helms [email_address] NOAA/NWS  Office of Science and Technology
Why NOAA Observes the Atmosphere? Current verses Objective Resolution Requirements ▼ ▼ Reference:  Schlatter, et al, 2005:  A Phenomenological Approach to the Specification of Observational Requirements ▼ ▼ Current Objective Req.
Integrated Upper-Air Observing System (IUOS) ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
First Weather Bureau and Regional Airline Collaboration
What is AMDAR? ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
U.S. AMDAR (MDCRS) ,[object Object],[object Object],[object Object],[object Object],CONUS: 150,000 Observations per Day
24hrs AMDAR Data Collection: Southwest U.S. 32  1 0 6 7 6 7 5 5 7 6 7 6 0 1 32 Tucson  (TUS) 18 21 30 25 29 18 11 152 Phoenix (PHX) Sa Fr Th We Tu Mo Su Wk
TAMDAR ,[object Object],[object Object],[object Object],[object Object],30,000 Observations per Day
AMDAR Data Collection: Comparison to Radiosonde 25 50 75 10 20 30 40 50 100 125 25 50 75 100 125 290 mph 600 mph Descent Ascent +5min +10min +22min Aircraft Climb Rate : ~1.5kft/min Aircraft Descent Rate : ~1.0kft/min -28min -20min -10min +10min +20min +30min +50min +40min Avg Wind : 60 Kts 600 mph Aircraft Speed Kft Balloon Climb Rate : ~1.0kft/min Distance (NM) Distance (NM)
AMDAR Data Collection: Sampling Frequency
AMDAR Data Collection: Ascent/Descent Sampling Frequency
AMDAR Data Collection: En Route Sampling Frequency
NWS Forecast Office Applications ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Data Comparison Wind Profilers Commercial aircraft GOES and POES Satellites Wind Estimates from Doppler Radar Radiosondes Numerical models
High Winds Schematic of Santa Ana winds in southern California
High Winds AREA FORECAST DISCUSSION NWS SAN DIEGO CA 1120 PM PST FRI DEC 22 2006  .DISCUSSION... UPDATE TO UPGRADE THE WIND ADVISORY FOR THE INLAND EMPIRE AND THE SANTA ANA MOUNTAINS AND FOOTHILLS TO A HIGH WIND WARNING THROUGH EARLY AFTERNOON SATURDAY. RECENT  ACARS SOUNDINGS FROM ONTARIO SHOW A VERY IMPRESSIVE SUBSIDENCE INVERSION NEAR 700 MB FAVORABLE FOR MOUNTAIN WAVE DEVELOPMENT AS WELL AS AN OVERALL STRONG WIND FIELD BELOW 700 MB WITH WINDS UP TO 50 KNOTS OR SO.  WINDS IN THE WINDIER LOCATIONS...BELOW THE CAJON PASS AND NEAR FREMONT CANYON HAVE GUSTED TO AROUND 60 MPH IN THE PAST HOUR.  Santa Ana
High Winds  AMDAR sounding at 0411 UTC December 23, 2006 from Ontario, California showing mountain top inversion and strong wind field. Santa Ana
Winter Precip @ SDF  RAIN KSDF 151843Z 06015KT 2 1/2SM RA BR OVC013 01/M01 A3001 RMK AO2 RAB30
Winter Precip @ SDF  METAR KSDF 160156Z 05009G17KT 5SM -PL BR OVC020 M01/M04 A3009 RMK  AO2 FZDZE55PLB55 SLP192 P0001 T10111039  = FZRA, FZDZ, PL
KSDF 160556Z 04009KT 4SM -PL BR OVC018 M03/M04 A3006=  KSDF 160456Z 04010KT 6SM -PL BR OVC020 M02/M04 A3007= ICE PELLETS Winter Precip @ SDF
AMDAR Future:  Building on our Success ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Adding Water Vapor to Data Collection:
AMDAR Links: AMDAR Flyer http://www.wmo.ch/web/aom/amprog/Publications/Final%20Production%20AMDAR%20Flyer.pdf U.S. AMDAR Page http://amdar.noaa.gov/ Automated Meteorological Reports from Commercial Aircraft by Bill Moninger, Rich Mamrosh, and Pat Pauley (2003). Published in the February, 2003 issue of the Bull. Amer. Meteor. Soc. 84, 203-216.  http://amdar.noaa.gov/docs/bams/ Optimization Requirements Document for the Meteorological Data Collection and Reporting System / Aircraft Meteorological Data Relay System, 2006, submitted to NOAA by ARINC. http://amdar.noaa.gov/docs/ARINC_Optimization_%20Req_March2006.pdf
Comments??? David Helms 301-713-3557 x193 [email_address] NOAA/ NWS  Office of Science and Technology
Observation Accuracies  – Temperature and Wind Speed - More discussions of observed data quality will follow Comparison of AMDAR and GPS radiosonde winds
Avg # Reports  per 6hr Cycle (+/- 3 hr window)  per Layer Count by Pressure Layer (mb) Temperature Observation Counts North American Domain (20-70 North, 60-140 West) January 2006 2500 Aircraft Obs vs.  200 Radiosonde Obs per Layer
Avg # Reports  per 6hr Cycle (+/- 3 hr window)  per Layer Count by Pressure Layer (mb) Wind Observation Counts North American Domain (20-70 North, 60-140 West) January 2006 2500 Aircraft Obs vs.  200 Radiosonde Obs per Layer    Max Count = VAD Winds
Avg # Reports  per 6hr Cycle (+/- 3 hr window)  per Layer Count by Pressure Layer (mb) Relative Humidity Observation Counts North American Domain (20-70 North, 60-140 West) January 2006 300 Aircraft Obs vs.  170 Radiosonde Obs per Layer
AMDAR Data Collection:  Sometimes too much data?? Numbers indicate average number of ascent/descent soundings per day  during the week of April 10, 2005 157 100 208 64 96 DAL:  31 DFW: 23 AFW: 10 64 135 53 20 151 18 131 LAX:120 SAN: 24 ONT: 23 BUR:  3 170 54 SFO:  78 OAK:  39 SMF:  10 MHR:  7 SJC:  7 FAT:  1 142 JFK:  64 EWR: 39 LGA:  32 135 43 15 22 24 35 31 6 7 13 13 10 10 17 5 64 7 14 5 5 18 22 8 2 88 13 7 8 5 9 1 17 Average Daily MDCRS Aircraft Soundings (Ascents and Descents) 26 15 13 13 9 9 9 7 7 7 5 5 5 4 3 3 3 2 2 2 2 2 2 1 1 1 1 1 1 9 6 142 3 170 1 4
MDCRS Data: Surface to 15K ft MDCRS Data: 15Kft to 40K ft Most Observations  Above 25K ft Most Ascents/Descents In the Midwest and East and West Coasts AMDAR Data Collection: Spatial Coverage
Weekly Data Availability  Varies by 40%  Daily Data Availability Varies by 60% AMDAR Data Collection: Temporal Coverage

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Amdar & acars by david helms

  • 1.
  • 2. Why NOAA Observes the Atmosphere? Current verses Objective Resolution Requirements ▼ ▼ Reference: Schlatter, et al, 2005: A Phenomenological Approach to the Specification of Observational Requirements ▼ ▼ Current Objective Req.
  • 3.
  • 4. First Weather Bureau and Regional Airline Collaboration
  • 5.
  • 6.
  • 7. 24hrs AMDAR Data Collection: Southwest U.S. 32 1 0 6 7 6 7 5 5 7 6 7 6 0 1 32 Tucson (TUS) 18 21 30 25 29 18 11 152 Phoenix (PHX) Sa Fr Th We Tu Mo Su Wk
  • 8.
  • 9. AMDAR Data Collection: Comparison to Radiosonde 25 50 75 10 20 30 40 50 100 125 25 50 75 100 125 290 mph 600 mph Descent Ascent +5min +10min +22min Aircraft Climb Rate : ~1.5kft/min Aircraft Descent Rate : ~1.0kft/min -28min -20min -10min +10min +20min +30min +50min +40min Avg Wind : 60 Kts 600 mph Aircraft Speed Kft Balloon Climb Rate : ~1.0kft/min Distance (NM) Distance (NM)
  • 10. AMDAR Data Collection: Sampling Frequency
  • 11. AMDAR Data Collection: Ascent/Descent Sampling Frequency
  • 12. AMDAR Data Collection: En Route Sampling Frequency
  • 13.
  • 14. Data Comparison Wind Profilers Commercial aircraft GOES and POES Satellites Wind Estimates from Doppler Radar Radiosondes Numerical models
  • 15. High Winds Schematic of Santa Ana winds in southern California
  • 16. High Winds AREA FORECAST DISCUSSION NWS SAN DIEGO CA 1120 PM PST FRI DEC 22 2006 .DISCUSSION... UPDATE TO UPGRADE THE WIND ADVISORY FOR THE INLAND EMPIRE AND THE SANTA ANA MOUNTAINS AND FOOTHILLS TO A HIGH WIND WARNING THROUGH EARLY AFTERNOON SATURDAY. RECENT ACARS SOUNDINGS FROM ONTARIO SHOW A VERY IMPRESSIVE SUBSIDENCE INVERSION NEAR 700 MB FAVORABLE FOR MOUNTAIN WAVE DEVELOPMENT AS WELL AS AN OVERALL STRONG WIND FIELD BELOW 700 MB WITH WINDS UP TO 50 KNOTS OR SO. WINDS IN THE WINDIER LOCATIONS...BELOW THE CAJON PASS AND NEAR FREMONT CANYON HAVE GUSTED TO AROUND 60 MPH IN THE PAST HOUR. Santa Ana
  • 17. High Winds AMDAR sounding at 0411 UTC December 23, 2006 from Ontario, California showing mountain top inversion and strong wind field. Santa Ana
  • 18. Winter Precip @ SDF RAIN KSDF 151843Z 06015KT 2 1/2SM RA BR OVC013 01/M01 A3001 RMK AO2 RAB30
  • 19. Winter Precip @ SDF METAR KSDF 160156Z 05009G17KT 5SM -PL BR OVC020 M01/M04 A3009 RMK AO2 FZDZE55PLB55 SLP192 P0001 T10111039 = FZRA, FZDZ, PL
  • 20. KSDF 160556Z 04009KT 4SM -PL BR OVC018 M03/M04 A3006= KSDF 160456Z 04010KT 6SM -PL BR OVC020 M02/M04 A3007= ICE PELLETS Winter Precip @ SDF
  • 21.
  • 22. AMDAR Links: AMDAR Flyer http://www.wmo.ch/web/aom/amprog/Publications/Final%20Production%20AMDAR%20Flyer.pdf U.S. AMDAR Page http://amdar.noaa.gov/ Automated Meteorological Reports from Commercial Aircraft by Bill Moninger, Rich Mamrosh, and Pat Pauley (2003). Published in the February, 2003 issue of the Bull. Amer. Meteor. Soc. 84, 203-216. http://amdar.noaa.gov/docs/bams/ Optimization Requirements Document for the Meteorological Data Collection and Reporting System / Aircraft Meteorological Data Relay System, 2006, submitted to NOAA by ARINC. http://amdar.noaa.gov/docs/ARINC_Optimization_%20Req_March2006.pdf
  • 23. Comments??? David Helms 301-713-3557 x193 [email_address] NOAA/ NWS Office of Science and Technology
  • 24. Observation Accuracies – Temperature and Wind Speed - More discussions of observed data quality will follow Comparison of AMDAR and GPS radiosonde winds
  • 25. Avg # Reports per 6hr Cycle (+/- 3 hr window) per Layer Count by Pressure Layer (mb) Temperature Observation Counts North American Domain (20-70 North, 60-140 West) January 2006 2500 Aircraft Obs vs. 200 Radiosonde Obs per Layer
  • 26. Avg # Reports per 6hr Cycle (+/- 3 hr window) per Layer Count by Pressure Layer (mb) Wind Observation Counts North American Domain (20-70 North, 60-140 West) January 2006 2500 Aircraft Obs vs. 200 Radiosonde Obs per Layer  Max Count = VAD Winds
  • 27. Avg # Reports per 6hr Cycle (+/- 3 hr window) per Layer Count by Pressure Layer (mb) Relative Humidity Observation Counts North American Domain (20-70 North, 60-140 West) January 2006 300 Aircraft Obs vs. 170 Radiosonde Obs per Layer
  • 28. AMDAR Data Collection: Sometimes too much data?? Numbers indicate average number of ascent/descent soundings per day during the week of April 10, 2005 157 100 208 64 96 DAL: 31 DFW: 23 AFW: 10 64 135 53 20 151 18 131 LAX:120 SAN: 24 ONT: 23 BUR: 3 170 54 SFO: 78 OAK: 39 SMF: 10 MHR: 7 SJC: 7 FAT: 1 142 JFK: 64 EWR: 39 LGA: 32 135 43 15 22 24 35 31 6 7 13 13 10 10 17 5 64 7 14 5 5 18 22 8 2 88 13 7 8 5 9 1 17 Average Daily MDCRS Aircraft Soundings (Ascents and Descents) 26 15 13 13 9 9 9 7 7 7 5 5 5 4 3 3 3 2 2 2 2 2 2 1 1 1 1 1 1 9 6 142 3 170 1 4
  • 29. MDCRS Data: Surface to 15K ft MDCRS Data: 15Kft to 40K ft Most Observations Above 25K ft Most Ascents/Descents In the Midwest and East and West Coasts AMDAR Data Collection: Spatial Coverage
  • 30. Weekly Data Availability Varies by 40% Daily Data Availability Varies by 60% AMDAR Data Collection: Temporal Coverage

Notas do Editor

  1. Invited Panel Presentation for the Regional Airline Association: http://www.raa.org/
  2. External Users: Executive Director, Mid-Atlantic Regional Air Management Association (MARMA) Lead Scientist, Northwest Association of Networked Ocean Observing Systems (NANOOS) Lead Meteorologist, Northwest Airlines Aviation Modeler, National Center for Atmospheric Research Hydrologist, National Hydrologic Warning Council (NHWC) Lead Meteorologist, Pacific Gas & Electric Meteorological Services CEO, WindLogics Science Applications International Corporation (SAIC) Chair, Weather Coalition Northwest Pacific Fishermen’s Association Maryland Emergency Management Agency European Composite Observing System (EuCOS) Chair, AMS Board on Private Sector Meteorology Director, IPS MeteoStar National Weather Association Chair, Expert Team on Observational Data Requirements And Redesign of the Global Observing System, WMO Chair, OPAG on Upper-Air Observation Technology, WMO Chief Scientist, Cooperative Institute for Meteorological Satellite Studies Internal Users: Director, NOAA OAR Air Resources Lab Program Lead, - Meteorological Requirements (ATO), FAA, DoT Lead Energy Initiative Modeler, National Severe Storms Lab, NOAA/OAR Principal Hydrologic Engineer, U.S. Army Corp of Engineers Science and Operations Officer, NOAA/NWS USAF Liaison to NOAA National Fire Weather Program Manager, Bureau of Land Management, DoI Director of Operations, National Atmospheric Release Advisory Center (NARAC), DoE IMAAC Deputy Program Manager, DHS Hazardous Materials Response Division (HAZMAT), Office of Response and Restoration, NOAA/NOS Scientist, Defense Threat Reduction Agency, DoD Chief Scientist, NOAA Rapid Update Cycle Model
  3. Selected aircraft were collecting atmospheric observations in the 1920’s, and only after this date did radiosondes commence operations in the 1950’s as the main in situ atmospheric observing system. From: Automated Meteorological Reports from Commercial Aircraft by Bill Moninger, Rich Mamrosh, and Pat Pauley (2003). Published in the February, 2003 issue of the Bull. Amer. Meteor. Soc. 84 , 203-216 http://acweb.fsl.noaa.gov/docs/bams/
  4. Automated Meteorological Reports from Commercial Aircraft by Bill Moninger, Rich Mamrosh, and Pat Pauley (2003). Published in the February, 2003 issue of the Bull. Amer. Meteor. Soc. 84 , 203-216. http://amdar.noaa.gov/docs/bams/
  5. Automated Meteorological Reports from Commercial Aircraft by Bill Moninger, Rich Mamrosh, and Pat Pauley (2003). Published in the February, 2003 issue of the Bull. Amer. Meteor. Soc. 84 , 203-216. http://amdar.noaa.gov/docs/bams/
  6. From 2006 ARINC Optimization Study.
  7. From 2006 ARINC Optimization Study.
  8. From 2006 ARINC Optimization Study.
  9. We will divide this part of the presentation into the seven different phenomenon based groups above.
  10. AMDAR provide yet another means of comparing data from different upper air systems. AMDAR is frequently used by meteorologists to verify the initialization and performance of the numerical weather prediction models. It has also been used to flag erroneous radiosonde, profiler, and WSR-88D VAD winds, and to verify GOES and POES satellite soundings.
  11. Randy Baker/UPS
  12. Aircraft observations provide opportunities to cost effectively enhance our public/private partnership including adding water vapor sensors, turbulence, and icing observations. WVSS II AMS Poster, August 2005 http://www.nws.noaa.gov/ost/wvss/AMS_NWP-WVSSII_Poster_JUL05.pdf
  13. From Ralph Petersen
  14. Brad Ballish, NOAA/NCEP, 2006.
  15. Brad Ballish, NOAA/NCEP, 2006.
  16. Brad Ballish, NOAA/NCEP, 2006.
  17. A leveling of data collection is sorely needed to more equally provide data in time and space.
  18. 1. ACARS Coverage - May 2001: A study in support of the TAMDAR project by Brian D. Jamison and Bill Moninger, Forecast Systems Laboratory. 2. Data (lower left and right figures) is from December 11, 2003.
  19. ACARS Coverage - May 2001: A study in support of the TAMDAR project by Brian D. Jamison and Bill Moninger, Forecast Systems Laboratory.