Comparison of Travel-Time Definitions
LoHCo Meeting --- Stanford, 2009 March 12 - 13
- S. Couvidat and the HMI Time-Distance
Pipeline Team
Comparison of Travel-Time Definitions S. Couvidat and the HMI - - PowerPoint PPT Presentation
Comparison of Travel-Time Definitions S. Couvidat and the HMI Time-Distance Pipeline Team LoHCo Meeting --- Stanford, 2009 March 12 - 13 Three travel-time definitions Gabor Wavelet (Kosovichev & Duvall, 1997): G = A exp[- 2 /4 (- g
LoHCo Meeting --- Stanford, 2009 March 12 - 13
Pipeline Team
Gabor Wavelet (Kosovichev & Duvall, 1997): G = A exp[-δω2/4 (τ-τg)2] cos[ω0(τ-τp)] Gizon & Birch (2002): X±(r1,r2,t)= ∫ dt f(t’) [C(r1,r2,t)-Cref(Δ,t’-t)]2 τ±(r1,r2) = argmint {X±(r1,r2,t)} Gizon & Birch (2004): τ±(r1,r2) =
Δ= 6.2 Mm
Δ= 30.55 Mm
Black = GB02, Green= GB04, Red= Gabor
Solid = Gabor, dashed= GB02, dash-dotted= GB04 upper=mean, lower=difference
(S. Couvidat & A. Birch)
used in local helioseismology by, e.g., Braun et al. (2007), Zhao et
maps, using shift theorem in Fourier domain; 12 flow velocities
studied f-mode case)
distances source-receiver
τP=29 min τP=23.5 min τP=18 min
δτNS not unique because ωNorth = ωSouth
Ray-path kernels can be corrected to include this dependence on the reference phase time: δτNS~ -2 ∫ nU/c2 ds + (δωS-δωN)/ω τp
Standard phase- speed filters Following Braun & Birch (2006)
Broad phase- speed filters
covariances have been normalized
can be problematic: the reference phase time used should always be mentioned
time differences not linear in the flow strength