Aftershock Blue Cool Citrus Liqueur, 70 cl

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Bai, Y., Liu, C., Lay, T., Cheung, K. F. & Ye, L. Optimizing a model of coseismic rupture for the 22 July 2020 M W 7.8 Simeonof earthquake by exploiting acute sensitivity of tsunami excitation across the shelf break. J. Geophys. Res.: Solid Earth 127, e2022JB024484 (2022). Herman, M. W. & Furlong, K. P. Triggering an unexpected earthquake in an uncoupled subduction zone. Sci. Adv. 7, eabf7590 (2021). Hayes, G. P. et al. Slab2, a comprehensive subduction zone geometry model. Science 362, 58–61 (2018).

Crowell, B. W. & Melgar, D. Slipping the Shumagin gap: A kinematic coseismic and early afterslip model of the M W 7.8 Simeonof Island, Alaska, earthquake. Geophys. Res. Lett. 47, e2020GL090308 (2020). Mulia, I. E., Heidarzadeh, M. & Satake, K. Effects of depth of fault slip and continental shelf geometry on the generation of anomalously long-period tsunami by the July 2020 M W 7.8 Shumagin (Alaska) earthquake. Geophys. Res. Lett. 49, e2021GL094937 (2022).

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Horowitz, W. L., Steffy, D. A. & Hoose, P. J. Geologic report for the Shumagin Planning Area, Western Gulf of Alaska. (U.S. Department of the Interior, Minerals Manages Services, Alaska OCS Region, 1989). OCS Report, MMS 89-0097.

As seismic and geodetic data can provide complementary constraints on the rupture process, we used both data types to invert the rupture process of the 19 October 2020 event assuming first one and then two fault segments. We performed non-linear finite fault inversions 29, 30, involving the joint analysis of coseismic static offsets, hr-GNSS time series, and seismic waveforms. A simulated annealing algorithm was used to solve for the slip magnitude and direction, rise time, and average rupture velocity for subfaults on the two segments. For each parameter, we set specific search bounds and intervals. The subfault size is chosen as 5 km × 5 km, and the rake angles on the two fault segments are constrained to be right-lateral purely strike-slip and purely dip-slip, respectively. We allowed both the rise and fall intervals of the asymmetric slip rate function for each subfault to vary from 0.6 to 6.0 s; thus, the corresponding slip duration for each subfault is limited between 1.2 and 12 s. We let the slip vary from 0.0 to 8.0 m, and the average rupture velocity is allowed to vary from 0.5 to 3.0 km/s. Green’s functions for static displacements and seismic waveforms are computed using a 1-D layered velocity model 31. Equal weighting among the data functionals for GNSS statics and seismic waveforms was used in this study. Tsunami modelingDrooff, C. & Freymueller, J. T. New constraints on slip deficit on the Aleutian megathrust and inflation at Mt. Veniaminof, Alaska from repeat GPS measurements. Geophys. Res. Lett. 48, e2020GL091787 (2021). Ye, L. et al. Rupture model for the 29 July 2021 M W 8.2 Chignik, Alaska earthquake constrained by seismic, geodetic, and tsunami observations. J. Geophys. Res.: Solid Earth 127, e2021JB023676 (2022). We select 62 P and 50 SH broadband recordings from the Incorporated Research Institutions for Seismology (IRIS) data management center with well-distributed azimuthal coverage at teleseismic epicentral distances between 30° and 90° (station distributions and data are shown in Supplementary Fig. 3). Instrument responses are removed to obtain ground velocities in the passband 1–300 s with waveform durations of 100 s. We precisely aligned P and SH wave initial motions manually. In August 2008, it was announced that the Alcohol Content (abv) would be lowered to 30%, from 40%. It was also announced that the Green variant (Thermal Bite) would be discontinued. Dziewonski, A. M. & Anderson, D. L. Preliminary reference Earth model. Phys. Earth Planet. Inter. 25, 297–356 (1981).