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Occultation TEC Measurements from FORMOSAT-3/COSMIC - IGS

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<strong>Occultation</strong> <strong>TEC</strong> <strong>Measurements</strong> <strong>from</strong><br />

<strong>FORMOSAT</strong>-3/<strong>COSMIC</strong><br />

Tiger J.Y. Liu, GPSARC, NSPO, NOAA<br />

Institute of Space Science, College of Earth Sciences,<br />

National Central University, TAIWAN


Outline<br />

<strong>FORMOSAT</strong>-3/<strong>COSMIC</strong><br />

Tropospheric Observation<br />

Ionospheric Observation<br />

Seismo-ionospheric Study<br />

FOEMOSAT-7/<strong>COSMIC</strong>-2<br />

Summary<br />

2<br />

21-Jul-10


Solar Terrestrial Environment


Thermosphere<br />

Plasmasphere<br />

(Protonsphere)<br />

Ionosphere<br />

Mesosphere<br />

Stratosphere<br />

Neutral Atmosphere<br />

Troposphere


<strong>TEC</strong>u<br />

120<br />

Ionospheric total electron content<br />

(<strong>TEC</strong>) derived <strong>from</strong> GPS<br />

Receiver: YMSM (North Taiwan)<br />

L1:1575.42 MHz (10.23 MHz×154 )<br />

L2:1227.60 MHz (10.23 MHz×120)<br />

C/A code (1.023 MHz)<br />

P code (10.23 MHz)<br />

90<br />

60<br />

30<br />

0<br />

08:00 14:00 20:00 02:00 08:00<br />

(x i , y i , z i ) Local Time<br />

<strong>TEC</strong> (total electron content)<br />

unit: <strong>TEC</strong>u (10 16 ele/m 2 )<br />

ionosphere<br />

S o =[(x i -x j ) 2 +(y i -y j ) 2 +(z i -z j ) 2 ] 1/2<br />

Line-of-sight<br />

(x j ,y j , z j )<br />

6


<strong>FORMOSAT</strong>-3/<strong>COSMIC</strong><br />

Space-based GPS receiver


<strong>FORMOSAT</strong>-3/<strong>COSMIC</strong><br />

Global Real-time<br />

Weather (Meteorology)<br />

Space Weather (Ionosphere)<br />

Observation and Prediction<br />

The <strong>FORMOSAT</strong>-3/<strong>COSMIC</strong> program is an international<br />

collaboration between Taiwan and the United States that<br />

will use a constellation of six remote sensing microsatellites<br />

to collect atmospheric data for weather prediction and for<br />

ionosphere, climate and gravity research. Data <strong>from</strong> the<br />

satellites will be made freely available to the international scientific<br />

community in near real-time.


<strong>FORMOSAT</strong>-3/<strong>COSMIC</strong><br />

• <strong>FORMOSAT</strong>-3/<strong>COSMIC</strong><br />

Constellation was launch at<br />

01:40 UTC, April 14, 2006<br />

(Taiwan Time: April 15 2006) at<br />

Vandenberg Air Force Base,<br />

CA. Minotaur Launch<br />

• Maneuvered into six different<br />

orbital planes (inclination ~72°)<br />

for optimal global coverage (at<br />

~800 km altitude).<br />

• All satellites are in good<br />

health and providing science<br />

data.


<strong>FORMOSAT</strong>-3/<strong>COSMIC</strong><br />

The <strong>FORMOSAT</strong>-3/<strong>COSMIC</strong> system is a<br />

constellation of 6 LEO micro-satellites<br />

Each satellite carries 3 payloads:<br />

– GPS occultation ti receiver<br />

– Tiny Ionospheric<br />

Photometer<br />

– Tri-Band Beacon.<br />

Global observation of pressure,<br />

temperature, water vapor,<br />

refractivity, ionospheric<br />

electron density and<br />

scintillation for weather and space weather<br />

research as well as climate monitoring<br />

Demonstrate quasi-operational GPS limb<br />

sounding with global coverage in near-real<br />

time


Global<br />

Positioning<br />

i<br />

System


Gps <strong>Occultation</strong> eXperiment (GOX)


<strong>FORMOSAT</strong>-3/<strong>COSMIC</strong><br />

Profiling the Troposphere, Stratosphere and Ionosphere by Radio <strong>Occultation</strong>


Mission Orbit of <strong>FORMOSAT</strong>-3/<strong>COSMIC</strong>


<strong>FORMOSAT</strong>3/<strong>COSMIC</strong><br />

-Troposphere<br />

p<br />

Walker Circulation: La Niña, El Niño<br />

Hadley Circulation: Plateau Heating<br />

Polar Circulation: Planetary Wave


Distribution of occultation events observed<br />

by <strong>FORMOSAT</strong>-3<br />

More than 2500 radio occultation (RO) soundings (green dots)<br />

obtained by the GPS <strong>Occultation</strong> Experiment (GOX) each day. In<br />

comparison, radiosondes d (red dots) provide only approximately 1500<br />

soundings per day.


Super Typhoon Jangmi (2008)


<strong>COSMIC</strong> Profile Availability<br />

22.5-1.5 1.5-4.5 4.5-7.5 7.5-10.5<br />

10.5-13.5 13.5-16.5 16.5-19.5 19.5-22.5<br />

22.5-1.5(+1d)<br />

00 00z 00z<br />

DA time window<br />

Free forecast<br />

NCEP GFS for IC and LBC<br />

Availale conventional data<br />

<strong>COSMIC</strong> data is available continuously<br />

Not like radiosonde data available only at 00 and 12Z<br />

Not like radiosonde data available only at 00 and 12Z<br />

Cycling 3DVAR for long data assimilation time window<br />

is one of the optimal assimilation scheme


Cold 3DVAR vs Cycling 3DVAR<br />

Cold 3DVAR<br />

Cycling 3DVAR<br />

Significant improvement for trackforecast in cycling<br />

3DVAR


El Niño La Niña<br />

Walker Circulation


La Niña<br />

El Niño<br />

[Webster and Chang, J. Atmos. Sci., 1988]


Global F3/C tropopause height<br />

ENSO Warm<br />

ENSO Cold<br />

Normal<br />

ENSO Warm


(b)<br />

Tropospheric Pressure<br />

ENSO Warm<br />

ENSO Cold<br />

Normal<br />

ENSO Warm<br />

21-Jul-10<br />

23


Tropospheric Temperature<br />

ENSO Warm<br />

ENSO Cold<br />

Normal<br />

ENSO Warm


Tropospheric Water Vapor<br />

ENSO Warm<br />

ENSO Cold<br />

Normal<br />

ENSO Warm


Tibetan Plateau Heating<br />

Hadley Circulation and<br />

the reserved


Global Tropopause Height in July 2008


Global Tropopause Height in July 2009


Polar Cell Circulation<br />

Planetary Wave


The planetary wave signature


<strong>FORMOSAT</strong>3/<strong>COSMIC</strong><br />

-Ionosphere


Distribution of occultation events<br />

observed by <strong>FORMOSAT</strong>-3<br />

GOX


Ionosphere<br />

EIA and Plasma Cave<br />

Plasma Depletion Bay<br />

Pre-earthquake Anomaly


Equatorial plasma fountain<br />

Altitude (km)<br />

Low-Latitude Ionosphere is dominated by the<br />

electrodynamics<br />

1000<br />

900<br />

800<br />

Plasma<br />

fountain<br />

magnetic<br />

field line<br />

700<br />

600<br />

500<br />

400<br />

300<br />

200<br />

<br />

1600 LT<br />

<br />

Ratcliffe [1972]<br />

LT 10:00<br />

1000<br />

800<br />

600<br />

400<br />

200<br />

−20 0 20 40<br />

LT 13:00<br />

1000<br />

800<br />

600<br />

400<br />

200<br />

−20 0 20 40<br />

LT 16:00<br />

1000<br />

100<br />

−10 0 10 20 30 40<br />

Geographic Latitude<br />

A model simulated plasma fountain effect<br />

starting ti in the morning and enhance to its<br />

maximum around noon<br />

800<br />

600<br />

400<br />

200<br />

−20 0 20 40


Altitde [km]<br />

500<br />

400<br />

0100<br />

300<br />

200<br />

100<br />

Equatorial Ionization Anomaly<br />

0700 1000 1500<br />

[e]/cm 3 x 10 5<br />

10<br />

0300 0730 1030 1600 8<br />

9<br />

7<br />

0500 0800 1100 1700<br />

6<br />

0530 0830 1200 1900<br />

5<br />

4<br />

0600 0900 1300 2100 3<br />

2<br />

0630 0930 1400 2300<br />

1<br />

−45 −30 −15 0 15 30 45<br />

Geomagnetic latitude [ o N]<br />

Lin et al.[GRL 2008]<br />

July-August 2006<br />

0


2007 M-month


2007 J-month


2007 S-month


Ionospheric plasma cave/tunnel<br />

(a)<br />

(b)<br />

Plasma cave<br />

Plasma Tunnel<br />

Liu et al. (JGR, 2010)


Plasma Depletion Bay


Plasma Depletion Bay observed by F3/C and TIMED GUVI<br />

Nighttime ionospheric structures, 23:00 LT (global fixed local time)<br />

1.5<br />

1.0<br />

0.5<br />

0<br />

Geo eographic Latitud ude ( ° N)<br />

50<br />

40<br />

30<br />

20<br />

10<br />

0<br />

−10<br />

−20<br />

−30<br />

−40<br />

TIMED−GUVI 135.6nm PLOT YEAR=2006; DOY=141−153; TIME=20−22LT<br />

−50<br />

−180 −150 −120 −90 −60 −30 0 30 60 90 120 150 180<br />

Geographic Longitude ( ° E)<br />

Rayleights<br />

8<br />

6<br />

4<br />

2<br />

0


Plasma depletion bay<br />

Nighttime ionospheric structures: 3‐D images


Mid-latitude trough


Result and Interpretation<br />

<strong>FORMOSAT</strong>/<strong>COSMIC</strong> NmF2, M-month, 20:00MLT<br />

Pole edge<br />

EIA peak<br />

Pole edge<br />

Trough<br />

Trough<br />

Equator edge


<strong>FORMOSAT</strong>-3/<strong>COSMIC</strong> NmF2 Persudo-3D structure<br />

Northern Hemisphere, M-month<br />

lat ×alt ×time: 2°×2km ×0.5hr<br />

21-Jul-10<br />

49


Seasonal Variation<br />

Northern hemisphere<br />

Southern hemisphere<br />

50<br />

21-Jul-10


21-Jul-10<br />

51


21-Jul-10<br />

52


Seismo-ionospheric Precursor of<br />

the 12 May 2008 M7.9 Wenchuan<br />

Earthquake


China Earthquakes<br />

1998/05/01~2008/05/12 36 M 6.0 earthquakes<br />

2008/5/12 M7.9 Wenchuan Earthquake


Locations of the 35M6.0 earthquakes together with Wenchuan earthquake<br />

occurred in China during May 1, 1998-May 12, 2008.


A time series of GPS <strong>TEC</strong> right above the epicenter of the M7.9<br />

Wenchuan earthquake on May 15, 2008.


The GIMs observed at 08:00UT and global fixed 15:00 LT on day 6 before<br />

the 2008 Mw7.9 Sichuan Earthquake.<br />

0800UT<br />

1500LT<br />

R =10 043M 0.43M


D-6, 5/6 2008<br />

0600UT, 1300LT<br />

D-5, 5/7 2008<br />

0600UT, 1300LT<br />

D-4, 5/8 2008<br />

0600UT, 1300LT<br />

D-3, 5/9 2008<br />

1400UT, 2100LT<br />

D 2 5/10 2008<br />

D-2, 5/10 2008<br />

0400UT, 1100LT


Liu et al.[JGR, 2009]


Conclusion<br />

F3/C constantly observes the temperature,<br />

pressure, water vapor in the troposphere,<br />

which is essential for weather forecast and<br />

climate study.<br />

F3/C probes 3-D structures and dynamics of<br />

the ionospheric electron density and can be<br />

applied on space weather monitoring.<br />

F3/C+GIM should be useful to explore<br />

seismo-ionospheric anomalies of the GPS<br />

<strong>TEC</strong> before large earthquakes.


Ground- and Space-Based<br />

GPS Observations<br />

IRI assimilation<br />

GIM + F3/C <strong>TEC</strong>


GIM <strong>TEC</strong> vs. GIM+F3/C <strong>TEC</strong><br />

Latitude (°N)<br />

Longitude (°E)


<strong>FORMOSAT</strong>-7/<strong>COSMIC</strong>-2<br />

12 satellites<br />

Tri-G<br />

2014, 2017


<strong>FORMOSAT</strong>/<strong>COSMIC</strong>-Follow On<br />

Builds on the weather forecasting and<br />

ionospheric science success of<br />

<strong>FORMOSAT</strong>-3/<strong>COSMIC</strong><br />

Taiwan/NSPO and US/NOAA<br />

12 satellites + TriG receiver<br />

First launch 2014, second launch ~2017<br />

Improved performance<br />

5x+ increase in number of measurements<br />

Higher precision in the atmosphere/ionosphere<br />

C/NOFS Science Workshop 68<br />

May 20, 2010


<strong>FORMOSAT</strong>-7/<strong>COSMIC</strong>-2 v.s. . <strong>FORMOSAT</strong>-3/<strong>COSMIC</strong><br />

Mission<br />

Spacecraft<br />

<strong>FORMOSAT</strong>-7/<strong>COSMIC</strong>-2<br />

Establish an operational<br />

mission for near real-time<br />

numerical weather prediction<br />

8,000 (threshold) profiles per<br />

day (the objective number is<br />

10,000)<br />

NSPO design, procure, and<br />

integrate t 12 SCs<br />

NSPO will integrate new GNSS<br />

PL provided by JPL and perform<br />

12 SCs Integration and Test at<br />

NSPO<br />

<strong>FORMOSAT</strong>-3/<strong>COSMIC</strong><br />

Demonstration of near real-time<br />

numerical weather prediction<br />

1,600~1,800 profiles per day<br />

NSPO define system<br />

requirement<br />

NSPO and Orbital design SC ;<br />

UCAR provide PL suite<br />

EDU and FM1 I&T at Orbital<br />

FM2 to FM6 integration and test<br />

at NSPO<br />

Mission GPS/GALILEO/GLONASS GPS tracking capability<br />

Payload tracking capabilities


<strong>FORMOSAT</strong>-7/<strong>COSMIC</strong>-2 v.s. . <strong>FORMOSAT</strong>-3/<strong>COSMIC</strong><br />

Launch<br />

Vehicle<br />

Ground<br />

Operations<br />

Data<br />

Processing<br />

<strong>FORMOSAT</strong>-7/<strong>COSMIC</strong>-2<br />

NOAA will provide 2 (TBR)<br />

launches into selected<br />

orbits/inclinations<br />

NOAA’s responsibility to seek<br />

the ground Networks<br />

High degree of automated<br />

ground system for 12-satellite<br />

constellation<br />

Taiwan Data Processing<br />

Center<br />

US Data Processing Center<br />

<strong>FORMOSAT</strong>-3/<strong>COSMIC</strong> Mission<br />

Use MINOTAUR LV of the US Air<br />

Force via UCAR’s help<br />

Use USN ground stations for the<br />

first 2 years, and then supported<br />

by NOAA ground stations after 2<br />

years<br />

6-satellite constellation operations<br />

TACC and CDAAC


Social Impacts<br />

Explore Space<br />

Weather Sciences<br />

Enhance the Capabilities of<br />

Regional and Global<br />

Weather Prediction<br />

Monitor Climate Trend<br />

Enhance the Capability<br />

Enhance the Capability<br />

on Severe Weather<br />

Prediction


Mission Architecture<br />

GALILEO<br />

GLONASS-CDMA<br />

High-Inc<br />

GPS<br />

<strong>FORMOSAT</strong>-7/<br />

<strong>COSMIC</strong>-2<br />

Low-Inc<br />

TT&C stations<br />

(Taiwan)<br />

Remote TT&C stations<br />

(overseas)<br />

Fiducial<br />

Network<br />

Data Processing Center<br />

Satellite Operations<br />

and Control Center Users Researchers


Potential Constellation<br />

72° (6) and 35° (6)


Summary<br />

F3/C (future F7/C2) provides the global<br />

ionospheric i electron density in real time<br />

which should be helpful to contracture a<br />

ground/space-based GIM of the GPS <strong>TEC</strong>.<br />

F3/C (future F7/C2) should also be useful<br />

for the tropospheric climatology study.<br />

21-Jul-10<br />

74


Thank you!!!<br />

太 空 所 ISS

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