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COSMIC Update and Highlights 8 November 2007 www.cosmic.ucar.edu/
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COSMIC launch picture provided by Orbital Sciences Corporation All six satellites stacked and launched on a Minotaur rocket Initial orbit altitude ~500 km; inclination ~72° By Dec 2007 will be maneuvered into six different orbital planes for optimal global coverage (at ~800 km altitude) Launch on April 14, 2006 Vandenberg AFB, CA
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Mariner IV at Mars July 1965 Planetary Radio Occultation Radio occultation was first applied to Planetary atmospheres by teams at Stanford U. and NASA/JPL
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GCOS Implementation Plan for the Global Observing System for Climate October 2004 Action A20 (AF13): GPS RO measurements should be made available in real time, incorporated into operational data streams, and sustained over the long-term. [ GCOS-92, WMO/TD No. 1219, October 2004] First ever constellation of RO satellites! Major international interest!
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GPS Occultation Basic measurement principle: Deduce atmospheric properties based on precise measurement of phase delay and amplitude.
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Global observations of: Pressure, Temperature, Humidity Refractivity Ionospheric Electron Density
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GPS Radio Occultation (RO) Data Climate: –Characterize climate, its variability and change –Evaluate global climate models and analyses –Monitor climate change and variability with unprecedented accuracy- world’s most accurate thermometer! Meteorology: –Improve global weather analyses, particularly over data void regions such as the oceans and polar regions –Improve skill of global and regional weather prediction models –Improve understanding of tropical, midlatitude and polar weather systems and their interactions Ionosphere: –Characterize global electronic density distribution –Observe the interactions among the upper stratosphere, mesosphere and ionosphere –Improve the analysis and prediction of space weather.
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Heritage of FORMOSAT-3/COSMIC July 1965 Mariner IV mission to Mars ~1988 JPL proposes RO mission for Earth 1993 UCAR GPS/Met proposal to NSF 1995-97 UCAR GPS/MET-1 st RO mission for Earth 1996 Concept of ROCSAT-3/COSMIC originated in Taiwan (UCAR and NSC) 1998 First tech support agreement NSPO 2001 FORMOSAT-3/COSMIC project begins 2006 Launch April 14, 2006
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A COSMIC Education Module A joint effort by COMET and COSMIC. It covers: - Basics of GPS radio occultation science - Applications to weather, climate, and ionosphere - COSMIC Mission description http://www.meted.ucar.edu/COSMIC/
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http://www.cosmic.ucar.edu * Select the 'Sign Up ' link under COSMIC Accept data use agreement * Enter information: Name, Address, email, user_id, Password, planned use of data An email will be sent within 2-3 business days to indicate access has been granted. COSMIC Data Access More than 350 users have registered
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RO-Research to Ops RO data will be valuable to: –Weather prediction –Climate monitoring and analysis –ionospheric research and space weather forecasting –Complement other satellite observing systems Need plan for transition from research into operations COSMIC II
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Characteristics of GPS RO Data Limb sounding geometry complementary to ground and space nadir viewing instruments Global 3-D coverage 40 km to surface High accuracy (equivalent to <1 K; average accuracy <0.1 K) High vertical resolution (0.1 km surface - 1km tropopause) Only system from space to resolve atmospheric boundary layer All weather-minimally affected by aerosols, clouds or precipitation Independent height and pressure Requires no first guess sounding Independent of radiosonde calibration No instrument drift No satellite-to-satellite bias Compact sensor, low power, low cost
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Current Constellation Oct. 1, 2007
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Sunday May 6, 2007 Global coverage in all weather 2111 soundings
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A typical RO sounding showing very sharp tropopause. No other instrument from space can provide this high vertical resolution.
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The Effect of Open Loop Tracking
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Penetration of setting/rising soundings More than 60% of all soundings penetrate to at least 1 km
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Detecting the Atmospheric Boundary layer with RO
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Global Distribution and Height of Atmospheric Boundary Layer
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Precipitable water estimated from COSMIC GPS RO data
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Weather Analysis and Prediction
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Leading Weather Center Newsletters
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Impact study with COSMIC 500 hPa geopotential heights anomaly correlation (the higher the better) as a function of forecast day for two different experiments: –PRYnc (assimilation of operational obs ), –PRYc (PRYnc + COSMIC) We assimilated around 1,000 COSMIC profiles per day Results with COSMIC are very encouraging
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Southern Hemisphere Forecast Improvements from COSMIC Data Sean Healey, ECMWF
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Using COSMIC for Hurricane Ernesto Prediction Without COSMIC With COSMIC Results from Hui Liu, NCAR
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Using COSMIC for Hurricane Ernesto Prediction GOES Image With COSMIC GOES Image from Tim Schmitt, SSEC
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Climate
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abc We can use RO data to calibrate other instruments N15, N16 and N18 AMSU calibration against COSMIC
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Comparison of PW data from COSMIC and global analyses PW retrieved from COSMIC GPS RO data using NCEP or ECMWF analysis as first guess PW derived from NCEP or ECMWF analyses
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Comparison of SSM/I retrieval with COSMIC
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COSMIC - CHAMP Mission Comparison
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Ionosphere and Space Weather
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Comparisons with ISR data [Lei et al., submitted to JGR 2007]
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Scintillation Sensing with COSMIC No scintillation S4=0.005 Scintillation S4=0.113 GPS/MET SNR data Where is the source Region of the scintillation?
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COSMIC Follow-On Mission NRC Decadal Survey Recommendation for NOAA: “Implement an operational radio occultation satellite constellation following COSMIC”
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Improvements expected from “COSMIC II” More receivers per launch - ~20 kg micro-satellites More soundings per receiver - added Galileo / Glonass tracking capability Higher density of profiles - data useful for global and mesoscale models Lower data latency - Can be reduced from 2-3 hours to 5 minutes (especially important for Space Weather) Improved tracking and more antenna gain - better data in the lowest moist troposphere Continued, longer, stable climate record Possibility of added capability like monitoring of reflections from sea surface and ice sheets
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COSMIC Follow-On Mission Possible Future Coverage of Daily Soundings
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Coverage of possible future constellations 6 RO constellation (COSMIC) 28 GPS Add 24 GLONASS Add 30 Galileo
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Coverage of possible future constellations 12 RO constellation 28 GPS Add 24 GLONASS Add 30 Galileo
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Coverage of possible future constellations 24 RO constellation 28 GPS Add 24 GLONASS Add 30 Galileo
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Occultation Sounding Statistics # of LEO’sTransmitters Total number of soundings Average horizontal spacing [km] Average number of soundings in 500km/500km box [#] 6GPS 3112404.81.5 6GPS+GLO 5959292.62.9 6GPS+GLO+GAL 9307234.14.6 12GPS 6267285.33.1 12GPS+GLO 11954206.65.9 12GPS+GLO+GAL 18645165.49.1 24GPS 12506201.96.1 24GPS+GLO 23905146.111.7 24GPS+GLO+GAL 37320116.918.3 48GPS 25012142.812.3 48GPS+GLO 47761103.323.4 48GPS+GLO+GAL 7453682.736.5
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RO-Research to Ops RO data will be valuable to: –Weather prediction –Climate monitoring and analysis –ionospheric research and space weather forecasting –Complement other satellite observing systems Need plan for transition from research into operations COSMIC II
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The Future FORMOSAT-3/COSMIC is Exceeding Expectations Need to complete mission Need to plan for next mission COSMIC launch picture provided by Orbital Sciences Corporation
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Summary COSMIC a successful Taiwan-U.S. project COSMIC launched on time and within budget (~$100M mission) Inexpensive way of obtaining atmospheric soundings in all weather High accuracy, precision and vertical resolution demonstrated Already positive impact on weather models Observations of tropical boundary layer from space for first time Only observing system to provide information on ionosphere, stratosphere and troposphere Will have major impact on climate monitoring-world’s most accurate, precise and stable thermometer! Free and open exchange of data—more than 600 users from 42 countries
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