PHASE REFERENCED MAPPING AND DIFFERENTIAL ASTROMETRY: APPLICATIONS JON MARCAIDE 26 Sept 2001 Castel San Pietro Terme Very Long Baseline Interferometry (VLBI) s B = B·s / c Phase referenced map: I(x,y) =∫∫V(u,v) e-i 2 (ux + vy) du dv V(u,v) e-iA-B Marcaide & Shapiro, Ap.J. 276, 56-59 (1984) Phase-reference mapping: Differential phase: A-B = A-B(str) + A-B(pos) + A-B(ins) +A-B(atm) Phase referenced map: I(x,y) =∫∫V(u,v) e-i 2 (ux + vy) du dv V(u,v) e-iA-B Marcaide & Shapiro, A.J. 88, 1134-1137 (1983) Differential astrometry vs phase reference Alternating observation: A(t1) B(t2) A(t3) B(t4) A(t5) B(t6) ... Analysis: A(t1;res) = A(t1;obs) A(t1;thr) B(t2;res) = B(t2;obs) B(t2;thr) A-B(t’1;res) = A(t1;res) B(t2;res) A-B(res) = A-B(res; str) + A-B(res; pos) +A-B(res; ins) +A-B(res; atm) Phase-reference mapping: Differential phase: A-B(res) = A-B(res; str) + A-B(res; pos) + A-B(res; ins) +A-B(res; atm) 0 Phase referenced map: I(x,y) =∫∫V(u,v) e-i 2 (ux + vy) du dv V(u,v) e-iA-B(res) 0 Differential astrometry: A-B(res) = A-B(res; str) + A-B(res; pos) + A-B(res; ins) +A-B(res; atm) 0 WLSF Residuals (30º a 7mm) Technique • Walter Alef (1989), Very Long Baseline Interferometry: Techniques and Applications, M. Felli & R.E. Spencer, Eds. NATO ASI Series, Kluwer C283 • Phil Diamond, idem • Thompson, Moran & Swenson (1986) “Inteferometry and Synthesis in Radio Astronomy”, p. 384 PRECISION DIFFERENTIAL ASTROMETRY • For a long time: Standard frequencies: 8.4 & 2.3 GHz • Difficulty in reference point definition: “-arcsec astrometry vs. m-arcsec resolution images” • Examples: 4C39.25, 1928+738.... 4C39.25 1928+738 A hybrid approach Observations of the pair 0735+178 / 0748+128 Combination of : 1) Differential astrometry @ 8.4 GHz 2) Simultaneous maps @ 43GHz The idea is to interpret the 8.4GHz astrometry with the help of the 43GHz maps. 0735+178 3.6cm 0735+178 3.6cm 0735+178 3.6cm 0735+178 7mm 3.6cm Differential astrometry @ 7mm Advantages: • • • Easier identification of the reference point Reference point closer to central engine (assumed stationary) Ionospheric contribution 25 times smaller than @ 3.6cm Disadvantages: • • Tropospheric water vapor contribution larger Phase cycle duration: 23ps (5 times shorter than @ 3.6cm) ¿Are the Earth Orientation models precise enough to predict the interferometric phase to a small fraction of 23ps? Astrometry @ 7mm Observation cycle vs weather Observation cycle (switching time) is VERY dependent on weather Observation cycle vs weather Observation cycle vs weather 1928+738 / 2007+777 @ 7mm 1928+738 / 2007+777 @ 7mm Rate residuals 1928+738 / 2007+777 Rate residuals 7mm 1928+738 / 2007+777 7mm Astrometric model: • IERS Standard •Ionosphere (IONEX) •Troposphere (nodes) r.m.s. 30º Differenced phase delay residual ( 2 ps) Important for phase reference mapping Beyond Earth limitations: SPACE VLBI V.S.O.P. VLBI Space Observatory Program Astrometry with VSOP Halca limitations for astrometry: HALCA (Highly Advanced Laboratory for Communication and Astronomy) Short memory span to manoever the antenna (Difficulty for alternating observations of sources) Large fractional errors in the space baselines: () B/B B 50-100m (JPL) This implies that for source pairs with 1º, () 10 mas However, how about observing two sources simultaneously? Astrometry with VSOP VLBA + HALCA observations of the pair of quasars 1342+662 / 1342+663 @ 6cm 1342+662 / 1342+663 with separation = 4‘ have been observed simultaneously by HALCA y VLBA 1342+662 / 1342+663 Maps of 1342+662 and 1342+663 1342+662 1342+663 Phase reference analysis of 1342+662 A-B(res) = A-B(res; str) + A-B(res; pos) + A-B(res; ins) +A-B(res; atm) I(x,y) =∫∫V(u,v) e-i 2 (ux + vy) du dv Phase reference analysis of 1342+662 Phase reference analysis of 1342+662 Astrometric information: = -0.5 mas = 1.5 mas Phases of 1342+662 referenced to 1342+663 Phases of 1342+662 referenced to 1342+663 B HALCA ~ 10 m Phase-referenced maps of 1342+662 Only VLBA VLBA +HALCA Only HALCA Space astrometry with VSOP Scatter of position of maximum in maps: 50 as B HALCA ~ 3m Exoplanet search