Time Transfer by Laser Link : first results

Transcription

1 Time Transfer by Laser Link : first results P. Exertier, E. Samain, Ph. Guillemot, I. Petitbon, Ph. Berio, O. Laurain and Cl. Foussard OCA-GRGS, avenue Copernic Grasse

2 Time Transfer experiences : Objectives» ground to board AND between ground stations in common (and non common) view Monitoring of the DORIS USO» from several 10 of seconds» correlation with CARMEN-2 data (SAA area) Improvement of SLR data for orbitography» using the on-board dates and full rate data» test of 1 way pseudo-range for contributing to POD Fundamental physics : anisotropy of the speed of light» at the level of 2,7.10-9, but with the USO limitations» fine structure constant α» possibiliy of comparing frequencies at over 10 days of integration in common view» measurement limited by grond clocks quality

3 Principle A ground station fires laser pulses in the satellite's direction and records the dates and local times of the firings. Laser Reflect. Array (Departure and return dates are measured in an accurate way with regard to the ground clock ; arrival dates on the satellite are given with regard to an arbitrary reference). Detector U.S.Oscillator Aboard the satellite, the T2L2 instrument records the arrival dates of photons in on-board time. A system of retroreflectors, complement to the embarked equipment, reflects some photons back toward the ground station, which records the return dates in local time.

4 t R sat Principle (2) LRA t GPS sat dt TR USO t R sat t T sta t R sta = t T sta + dt TR t T sta, dt TR, t R sat : measured set = «triplet» (dt T is computed) t T sta dt T dt TR UTC

5 10 10 Freq stability of atomic clocks (for positioning&navigation systems) Doris Rubidium compact Césium industriel à déflexion magn Ions mercure Césium compact à pompage optique Maser H passif Maser H actif Fontaine à césium heure 1 jour Durée d'échantillonnage: τ [seconde] Instabilité relative de fréquence: σ y (τ)

6 Expected T2L2 stability : common-view 1000 σ x (τ) (ps) 100 Doris 10 1 Atmosphère Dateur Sol Géométrie Dateur Sol - Retour OUS 1000 Dateur Bord S/S vues communes σ x (τ) (ps) τ (s) non common-view Atmosphère Géométrie OUS Dateur Sol Dateur Sol - Retour Dateur Bord S/S vues non communes 300s S/S vues non communes 1000s S/S vues non communes 3000s τ (s)

7 monitoring <1µsec date of T2L2 events T2L2 events GPS : on board PPS (at 1 sec) : 0.15 µsec and f/f = SLR stations (clocks) : 100ns class : Arequipa, Tahiti, Yaragadee, Hartebeestoek, Greenbelt, MacDonald, MtPeak, Wettzell 1-2ps class : Grasse, Herstmonceux, Matera (soon), Wettzell (soon) intermediary class : Changchun, FTLRS(Ajaccio), Zimmerwald, Mt Stromlo 1µsec : easy 50 ns : ok now < 10ps : soon... ± < 1 ns

8 USO along time df/f ± > dt ± 70 ns

9 exemple of Time Transfers 100 ns 1 ns

10 SLR network

11 mois en 2008 MERIT-II CRD juin 11 (_a) 0 juillet 72 (_a) (_b) août 63 (_a) (_b) septembre 82 (_a) (_b) octobre 64 (_a) 04 (_b) 48 SLR data Format CRD, mois en Changchun , Zimmerw., CH , FTLRS Calern , Mt Stromlo, AUS , Hx, RU , MeO, F , FTLRS, Ajaccio **

12 SLR data Nb of mes

13 T2L2 event statistics day

14 Energy

15 SLR vs T2L2 data

16 Sets of «triplet» (3 dates) < 1ns / 100 sec : 1 ns

17 Effects and limitations Effects not (currently) modeled : On-board : calibration of received energy (non linear) detector time walk attitude (LRA - T2L2 optics) relativity SLR-station(s) : calibration (telemetry vs clock) bias (?) Limitations : on-board OUS proper error budget of telemetry, and calibrations non-common view

18 Improving corrections Conclusion Performing campaigns in 2009 with : SLR : FLTRS (in Paris) Grasse Hx, Wettzell Atomic clocks (Cesium, Maser-H, mobile fontain) DORIS (new beacon at Grasse SLR station) Calibrations (stations, energy,...) Futur analyses of Time Transfers Comparisons with the 2-way µwave technique