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O. de La Beaujardière, L. Jeong, K. Ray, J. Retterer, B. Basu, W. Burke, F. Rich, K. Groves, C. Huang, L. Gentile, D. Decker, W. Borer, C. Lin NSPWX meeting,

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Presentation on theme: "O. de La Beaujardière, L. Jeong, K. Ray, J. Retterer, B. Basu, W. Burke, F. Rich, K. Groves, C. Huang, L. Gentile, D. Decker, W. Borer, C. Lin NSPWX meeting,"— Presentation transcript:

1 O. de La Beaujardière, L. Jeong, K. Ray, J. Retterer, B. Basu, W. Burke, F. Rich, K. Groves, C. Huang, L. Gentile, D. Decker, W. Borer, C. Lin NSPWX meeting, Jan 2006 The Communication/Navigation Forecasting System (C/NOFS) Mission to Predict Equatorial Ionospheric Density and Scintillation

2 2 Why do we Care About the Ionosphere and Scintillation? Scintillation prevents communications with satellites Ionosphere reflects, refracts, diffracts & scatters radio waves Global Positioning Satellite (GPS) relies on transmissions at GHz frequencies (L band) GPS signal is affected by L Band scintillation – Effect is max at equator Many systems depend on GPS – Aviation (FAA) – Navigation – Timing – Many more Scintillation: priority number 1 for AF Sp Wx

3 3 C/NOFS Mission C/NOFS First satellite to provide continuous, global ambient ionosphere and scintillation forecasts Mission elements Satellite Ground-based instruments Models Data center Mission Goals Nowcasts and forecast ionospheric electron density and presence of irregularities Develop capability to produce long term outlook (2 to 5 days) Develop improved understanding of equatorial ionosphere and processes that trigger / inhibit irregularities

4 4 Satellite – low altitude / low inclination - Inclination: 13 deg (target) - Perigee/ Apogee: 375 and 720 Km - Orbital Period: 96 min/rev - TDRSS transmitter for near-real-time downlink Launch - April 2006 - Dedicated Pegasus XL launch Ground-based component: - Scintillation and beacon receivers - Other Ground-based instruments C/NOFS Mission Components

5 5 Payload Description Six Instruments RAM Plasma Sensors Planar Langmuir Probe (PLP) Developed by AFRL/VS (D. Hunton PI) Measures: Ion Density, Ion Density Variations, Electron Temperature Ion Velocity Meter (IVM) Developed by Univ. of Texas (R. Heelis PI) Measures: Vector Ion Velocity, Ion Density, Ion Temperature Neutral Wind Meter (NWM) Developed by Univ. of Texas (R. Heelis PI) Measures: Vector Neutral Wind Velocity RF Beacon Coherent EM Radio Tomography (CERTO) Developed by NRL (P. Bernhardt PI) Measures: Remote sensing of RF scintillations and LOS TEC GPS Receiver C/NOFS Occultation Receiver for Ionospheric Sensing and Specification (CORISS) Developed by Aerospace (P. Straus PI) Measures: Remote sensing of LOS TEC Electric Field Instrument Vector Electric Field Instrument (VEFI) Developed by NASA/GSFC (R. Pfaff PI) Measures: Vector AC and DC electric fields

6 6 C/NOFS ground based instruments SCINDA Ground Stations (2008 plan) 30N 0 30S 210E 240E 270E 300E330E 0 30E 60E90E120E 150E Backbone SitesSupporting SitesUnited Nations IHY Sites SCINDA: Scintillation Decision Aid – a network of receivers monitoring radio scintillation along lines of sight to satellite-based transmitters Additional ground instruments include GPS TEC Rx, all sky cameras, ionosondes, radars, etc

7 7 C/NOFS Forecast Model Plasma Instability Calculator Global Turbulence Modeler Bubble Evolution Calculator Scintillation Statistics Calculator Display Global Ambient Forecast Model Turbulence Seed Retterer et al. 2003, 2006 Iono model Turbulence model Scintillation Display

8 8 Ionospheric Models C/NOFS Models: – PBMOD (AFRL) being used in CNOFS forecast – ASSIM_IONOS (SEC) being used for CNOFS specification Models validated both pre- and post-launch Other models being considered Three data assimilation models: – GAIM (USU) is being transitioned for operational use at AFWA In FY 2005 demonstrated superiority of GAIM over PRISM, previous operational model In FY 2006 continue validation work in support of transition – GAIM (USC/JPL) being used in study on impact of CNOFS data in assimilation models Results are being tested in National Program Systems – Fusion Numerics model being regularly exercised by developer

9 9 C/NOFS Validation and Campaigns Pre-C/NOFS campaigns: – April 2002, Oct 2003 mag storms – May 31-June 1, 2002 – COPEX (Oct-Nov 2002) – World days 2002 to 2005 – Numerous validation periods with satellite data Instrument Validation Campaigns – E-Field and winds are most critical Flux Tube Campaign – To calculate parameters along magnetic flux tube, including E- region conductivity “Seeding Campaigns” – To determine if waves (TIDs, Gravity waves, tropospheric storms, other) play a role in triggering turbulence Global campaigns (using world days) – For validating density and scintillation at all longitudes during a 1 to 5 day period Shuttle Engine Burn Campaign Ex of validation: can C/NOFS models reproduce observed airglow intensity?

10 10 Questions Addressed Using C/NOFS Questions that will be addressed by the C/NOFS Mission include: Ambient Ionosphere: – Nowcast and forecast global Ne profiles E field: – Longitude variations – Pre reversal enhancement – Penetration E field, disturbance dynamo E field Wind: – Present average models are inaccurate – Variation as a function of LT, lat, long, season, solar activity, magnetic activity How do bubbles evolve in time and space? – Bubbles birth, growth and decay – What triggers their growth – What prevents them from growing – Can we determine a bubble’s age from observations of it’s irregularity spectrum, drift speed, AC E-field – How detrimental to Nav and Comm are old bubbles Turbulence and scintillation climatology

11 11 Concluding Remarks Appleton fountain and bubbles dominate equatorial ionospheric “weather” Ionospheric irregularities cause scintillation, which prevents communication, navigation, surveillance C/NOFS satellite launched to forecast ambient ionosphere and scintillation Will be the only US satellite dedicated to the ionosphere – DMSP and TIMED will also provide ionospheric data, but these are secondary to the mission Important array of ground-based instruments are part of C/NOFS Sophisticated models will provide forecast Many important space weather science questions remain that will hopefully be answered by the C/NOFS mission C/NOFS data will be not be restricted NSF and NASA have C/NOFS Guest-Investigator type initiatives C/NOFS Web site : http://www.vs.afrl.af.mil/Factsheets/cnofs.html http://www.vs.afrl.af.mil/Factsheets/cnofs.html

12 12 Questions? Jicamarca Radar, Peru – Oct 22, 1996 GUVI


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