Simula'ons of COSMIC Follow On Sounding Distribu'ons and Data Latency for OSSE Studies

Similar documents
Precise Orbit Determination and Radio Occultation Retrieval Processing at the UCAR CDAAC: Overview and Results

N E S D I S C D A A C. COSMIC Operations JCSDA TACC NCEP ECMWF CWB GTS UKMO

We have processed RO data for climate research and for validation of weather data since 1995 as illustrated in Figure 1.

Algorithms for inverting radio occultation signals in the ionosphere

COSMIC-2: Next Generation Atmospheric Remote Sensing System using Radio Occultation Technique

Radio Occultation Data Processing at the COSMIC Data Analysis and Archival Center (CDAAC)

Climate Monitoring with Radio Occultation Data

ROCSAT-3 Constellation Mission

Vicky Chu, Jer Ling, Tom Lin, Joe Fong, Feng-Tai Huang, Guey-Shin Chang. April 15, 2011

Recent Advances in Radio Occultation Science and Applications and a Look at the Future

Interacciones en la Red Iberica

Evaluation of a Linear Phase Observation Operator with CHAMP Radio Occultation Data and High-Resolution Regional Analysis

COSMIC Program Office

Supporting NOAA's Commercial Weather Data Project

Evaluation of a non-local observation operator in assimilation of. CHAMP radio occultation refractivity with WRF

EUMETSAT's possible contributions to the future radio occultation constellation. COSMIC Workshop 2009 Boulder, USA

Observing System Simulation Experiments (OSSEs) with Radio Occultation observations

Observing the moist troposphere with radio occultation signals from COSMIC

Variability of the Boundary Layer Depth over Certain Regions of the Subtropical Ocean from 3 Years of COSMIC Data

Sensitivity of NWP model skill to the obliquity of the GPS radio occultation soundings

The FORMOSAT-3/COSMIC Five Year Mission Achievements: Atmospheric and Climate. Bill Kuo UCAR COSMIC

Third International Conference on GPS Radio Occultation Taipei 9-11 March FORMOSAT-3/COSMIC 20 Years of History

Latest new EUMETSAT Products: - A 15 year Reprocessed RO Data Set - GRAS Occultation Prediction

- an Operational Radio Occultation System

Use of FY-3C/GNOS Data for Assessing the on-orbit Performance of Microwave Sounding Instruments

Errors in GNSS radio occultation data: relevance of the measurement geometry and obliquity of profiles

Monitoring the depth of the atmospheric boundary layer by GPS radio occultation signals

The global positioning system (GPS) radio-occultation (RO) limb-sounding technique

Comparison of GRUAN profiles with radio occultation bending angles propagated into temperature space

Impact of 837 GPS/MET bending angle profiles on assimilation and forecasts for the period June 20 30, 1995

A comparison of lower stratosphere temperature from microwave measurements with CHAMP GPS RO data

Improvement of GPS/MET Ionospheric Profiling and Validation Using the Chung-Li Ionosonde Measurements and the IRI model

IMPACT OF GROUND-BASED GPS PRECIPITABLE WATER VAPOR AND COSMIC GPS REFRACTIVITY PROFILE ON HURRICANE DEAN FORECAST. (a) (b) (c)

Comparison of DMI Retrieval of CHAMP Occultation Data with ECMWF

Assimilation of Global Positioning System Radio Occultation Observations into NCEP s Global Data Assimilation System

Michelle Feltz, Robert Knuteson, Dave Tobin, Tony Reale*, Steve Ackerman, Henry Revercomb

Application of Radio Occultation Data in Analyses and Forecasts of Tropical Cyclones Using an Ensemble Assimilation System

New Radiosonde Temperature Bias Adjustments for Potential NWP Applications Based on GPS RO Data

Scintillation Nowcasting with GNSS Radio Occultation Data

Combined forecast impact of GRACE-A and CHAMP GPS radio occultation bending angle profiles

Calibration of Temperature in the Lower Stratosphere from Microwave Measurements using COSMIC Radio Occultation Data: Preliminary Results

Equatorial and Low Latitude Scintillation Initiated From Low Altitude Forcing via Hurricanes/Typhoons

NOAA Satellite & Information Service (NESDIS)

GPS RO Retrieval Improvements in Ice Clouds

SSC13-VI-1 MISSION DESIGN CONCEPT

IN ORBIT VERIFICATION RESULTS FROM GRAS RECEIVER ON METOP-A SATELLITE

Analysis of Gravity Waves from Radio Occultation Measurements

Development of the Next Generation GRAS Instrument

GPS radio occultation with TerraSAR-X and TanDEM-X: sensitivity of lower troposphere sounding to the Open-Loop Doppler model

The Impacts of GPS Radio Occultation Data on the Analysis and Prediction of Tropical Cyclones. Bill Kuo, Xingqin Fang, and Hui Liu UCAR COSMIC

Assimilation of GPS radio occultation measurements at Météo-France

Analysis and validation of GPS/MET data in the neutral atmosphere

The Use of GPS Radio Occultation Data for Tropical Cyclone Prediction. Bill Kuo and Hui Liu UCAR

VELOX-CI: Advanced Application of GPS for Radio Occultation and Satellite Attitude Determination

Processing of GPS radio occultation data from TerraSAR-X and TanDEM-X: Current status & future plans

Characterizing Irregularities and Scintillation with GNSS Radio Occultations

Impact of GPS RO Data on the Prediction of Tropical Cyclones

Simulation Results of Alternative Methods for Formation Separation Control

Atmospheric Climate Monitoring and Change Detection using GPS Radio Occultation Records. Kurzzusammenfassung

Estimating Atmospheric Boundary Layer Depth Using COSMIC Radio Occultation Data

4/23/2014. Radio Occultation as a Gap Filler for Infrared and Microwave Sounders Richard Anthes Presentation to Joshua Leiling and Shawn Ward, GAO

The GRAS SAF Radio Occultation Processing Intercomparison Project ROPIC

The occurrence climatology equatorial F-region irregularities in the COSMIC RO data

Dependence of positive refractivity bias of GPS RO cloudy profiles on cloud fraction along GPS RO limb tracks

Coordinate Study of the Ionospheric Stratification at Low Latitude: Results from the COSMIC and GIRO

Summary of IROWG Activities

A Physically Based Data QC Procedure and Its Impact on the Assimila9on of GPS RO Observa9ons in the Tropical Lower Troposphere

Thermal Structure of the Topside Ionosphere at Low Latitudes: New Observational Opportunities Pei Chen Lai and William J. Burke

GPS radio occultation with CHAMP and GRACE: A first look at a new and promising satellite configuration for global atmospheric sounding

Assessing attitude error of FORMOSAT-3/COSMIC satellites and its impact on orbit determination

Stratospheric temperature trends from GPS-RO and Aqua AMSU measurements

Tsunami Detection from Space using GNSS Reflections

Approaching the First Global Radio Occultation Operational Mission Using Constellation LEO Satellites

Anew type of satellite data can now be assimilated at

Science Data Products. Scott England, Project Scientist UCB/SSL

Characteristics of the POD System in the new EPS GRAS Product Processing Facility

GRAS SAF Workshop on Applications of GPS Radio Occultation Measurements. ECMWF Reading, UK; June 2008

Taiwan Radio Occultation Process System (TROPS)

A simulated Radio Occultation Data Set for Processor and Instrument Testing

Turbulence Estimation Techniques for COSMIC Occultation Data

GPS Radio Occultation Data Assimilation using GSI

Assessment of COSMIC radio occultation retrieval product using global radiosonde data

Emerging GNSS based tropospheric products

THE GRAS SAF PROJECT: RADIO OCCULTATION PRODUCTS FROM METOP

Progress on the assimilation of GNSS-RO at ECMWF

ASSIMILATION OF GRAS GPS RADIO OCCULTATION MEASUREMENTS AT ECMWF

Radioholographic analysis of radio occultation data in multipath zones

An Assessment of Contemporary Global Reanalyses in the Polar Regions

esa ACE+ An Atmosphere and Climate Explorer based on GPS, GALILEO, and LEO-LEO Occultation Per Høeg (AIR/DMI) Gottfried Kirchengast (IGAM/UG)

EUMETSAT PLANS. Dr. K. Dieter Klaes EUMETSAT Am Kavalleriesand 31 D Darmstadt Germany

Assimilation of GPS RO and its Impact on Numerical. Weather Predictions in Hawaii. Chunhua Zhou and Yi-Leng Chen

Does the ATOVS RARS Network Matter for Global NWP? Brett Candy, Nigel Atkinson & Stephen English

The Size of the Jet Launching Region in M87

EUMETSAT PLANS. K. Dieter Klaes EUMETSAT Darmstadt, Germany

Reconstructing the GPS Refractivity Profiles inside the Atmospheric Boundary Layer with MODIS Cloud top temperature over Subtropical Eastern Oceans

A first bibliometric Analysis of the Radio Occultation Publication Record. Ruth Weitzel 1, Axel von Engeln 2. EUMETSAT, Darmstadt, Germany

Impact of COSMIC observations in a whole atmosphere-ionosphere data assimilation model

Sensitivity of GNSS Occultation Profiles to Horizontal Variability in the Troposphere: A Simulation Study

GPS Radio Occultation A New Data Source for Improvement of Antarctic Pressure Field

ROM SAF CDOP-2. Algorithm Theoretical Baseline Document: Level 3 Gridded Data

Transcription:

Simula'ons of COSMIC Follow On Sounding Distribu'ons and Data Latency for OSSE Studies Bill Schreiner Bill Kuo, Chris Rocken, Sergey Sokolovskiy UCAR/COSMIC Project Office

Outline RO sounding distribugon study RO data latency study COSMIC observagon error esgmates NOT for lower troposphere Summary

RO Geometry Ray Tangent Point GPS Height of Straight Line (-200 to 150km) a r tp a α LEO Earth

SpacecraN Geometry View from Side 15 15 0-27 +v fore Limb Antenna POD Antennas Spacecraft 0-27 -v aft Limb Antenna Side Antenna View from Top Azimuth Angle +v fore aft -v Side Antennas

Constella'on Requirements Uniform RO global sampling Uniform RO local Gme sampling Minimize RO data latency Minimize deployment Gme Maximize GPS tracking data

Simula'on Inputs

Simula'on Outputs Times at start/end of occultagon LaGtude/Longitude at start of occultagon LaGtude/Longitude at end of occultagon Rise/set flag OccultaGon azimuth angle in local level frame Azimuth of occultagon plane projected onto surface of Earth Horizontal smear LEO/GPS prn numbers

Number of Orbit Planes 6 5 6 5 6 planes Inc = 90 ΔΩ=180/n=30 3 4 3 4 6 planes Inc = 72 ΔΩ=180/n=30 1 30 2 4 1 30 2 3 4 planes Inc = 24 ΔΩ=180/n=45 1 45 2 3 4 4 planes Inc = 24 ΔΩ=360/n=90 1 2

Inclina'on vs. Precession rate Ω = -1.5 (µ/a 3 ) 1/2 (R E /a) 2 cos(i) J2/(1- e 2 ) 2 Final orbit 800 km Parking orbit 525 km

Geographic Coverage

Local Time Coverage Noon Midnight

Azimuth and Horizontal Smear Inc = 72 Inc = 24 Inc = 0 ~30% more soundings for 72 inc when azimuth angles > 45 considered 100% more ionospheric data when azimuth angles > 45 considered

Occulta'on Density vs. Inclina'on Azimuth < 45 InclinaGon > 68 required to capture every ½ orbit dump from (Fairbanks, Tromso, McMurdo, TrollSat)

Occulta'on Density vs. Constella'on Op'ons IIA 8/72 & 4/24 IIB 12/72 IIC 6/72 & 6/24 IID 4/72 & 8/24 Actual COSMIC Good tracking period

COSMIC Data Latency Timelines Current COSMIC LOS + 11.5 min Occultation Events 2-5 min Downlink 3 min PTP 1 m FTP 5 min CDAAC 2.5 min Wait FTP to NESDIS AOS LOS Latency of Occultation COSMIC-II AOS + 8 min Occultation Events 2 min Downlink 1 m FTP 5 min CDAAC FTP to NESDIS AOS Latency of Occultation

COSMIC II Average Data Latency Worst Case: Current COSMIC 15 deg elevagon cutoff Data to CDAAC = LOS + 4 min CDAAC processing Gme = 7.5 min Best Case: RealisGc COSMIC II 5 deg elevagon cutoff Data to CDAAC = AOS + 3 min CDAAC processing Gme = 5 min 15 sites: Fairbanks, Tromso, McMurdo, TrollSat, Guam, Hawaii, Vandenberg, Colorado, NewHampshire, DiegoGarcia, England, Thule, Bangalore, MauriGus, Taiwan Network COSMIC (Fairbanks, Tromso) COSMIC +McMurdo COSMIC +McMurdo +TrollSat LEO Inclina'on (deg) Worst Case Average Latency (min) Best Case Average Latency (min) 72 68 57 72 58 43 72 44 32 15 StaGons 72 31 21 15 StaGons 24 48 37

Current COSMIC Latency Ave = 86 min Ave = 96 min Simulation Ave = 68 min Current (one orbit) Latency: Fairbanks (FBSK01) = 72 min Norway (NORTG5) = 74 min Ave = 85 min

Refrac'vity Precision Collocated (Tangent points within 10km, same PRN) refracgvity profiles are differenced to esgmate precision (Schreiner et al., GRL, 2007, doi:10.1029/2006gl027557) Magnitude similar to theoregcal esgmates from Kursinski et al. (1997) Profile precision ~0.1% between 10 and 20 km RepresentaGveness errors not included These errors can be mapped to non local linear excess phase observable (Sokolovskiy et al, MWR, 2005)

Bending Angle Precision Collocated (Tangent points within 10km, same PRN) raw bending angle profiles from COSMIC3 are differenced with COSMIC4 at common impact heights Daterange = 2006.200 365 2 ranges of impact height are shown for visibility 15 to 60 km 0 to 15 km Legend: Mean = Black, STD = Green, STD of mean = Red, Count = Blue Profile precision < 0.2% above 20 km 15km < Impact height < 60km STD ~ 2.5e-6 rad 0km < Impact height < 15km

TEC Errors Absolute TEC good to ~ 3 TECU RelaGve TEC ~ 0.001 TECU Actual COSMIC reference link data ~ 0.0024 TECU at 1 Hz sampling (2009.001 004)

Summary Most uniform RO sampling provided by constellagon with 8 s/c at 72 inc and 4 s/c at 24 inc Slightly increase plane separagon for 8/72 component to minimize local Gme hole Plane separagon for 4/24 component should be 90 Perform sampling error study (similar to B. Pirscher) to quangfy errors Side viewing antennas (originally proposed to UCAR by Prof. Tsuda) COSMIC II should consider adding side looking antennas (100% increase in ionosphere data) COSMIC should consider side viewing test SimulaGon and current COSMIC data latency agree reasonably well Best case 32 min average latency for 72 constellagon from polar RTSs Best case 37 min average latency for 24 constellagon from 15 RTSs Demonstrated COSMIC precision very high Simulated sounding locagons and data latency data available upon request (schrein@ucar.edu)

Acknowledgments NSF Taiwan s NSPO NASA/JPL, NOAA, USAF, ONR, NRL Broad Reach Engineering