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Software

Kite - Software for Rapid Earthquake Source Optimisation from InSAR Surface Displacement

Urheber*innen
/persons/resource/isken

Isken,  Marius
2.1 Physics of Earthquakes and Volcanoes, 2.0 Geophysics, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

/persons/resource/hsudhaus

Sudhaus,  H.
2.1 Physics of Earthquakes and Volcanoes, 2.0 Geophysics, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

/persons/resource/heimann

Heimann,  Sebastian
2.1 Physics of Earthquakes and Volcanoes, 2.0 Geophysics, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

/persons/resource/asteinbe

Steinberg,  Andreas
2.1 Physics of Earthquakes and Volcanoes, 2.0 Geophysics, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Daout,  Simon
External Organizations;

Vasyura-Bathke,  Hannes
External Organizations;

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Zitation

Isken, M., Sudhaus, H., Heimann, S., Steinberg, A., Daout, S., Vasyura-Bathke, H.(2017): Kite - Software for Rapid Earthquake Source Optimisation from InSAR Surface Displacement, Potsdam : GFZ Data Services.
https://doi.org/10.5880/GFZ.2.1.2017.002


Zitierlink: https://gfzpublic.gfz-potsdam.de/pubman/item/item_2348888
Zusammenfassung
We present a modular open-source software framework - kite (http://pyrocko.org), written in Python and C. The software enables rapid post-processing of space-born InSAR-derived surface displacement maps, swift parametrization and sub-sampling of the displacement measurements. With our package we aim to ease and streamline the optimization of earthquake source parameters from InSAR and GPS data and facilitate their joint optimization with seismological waveforms in combination with the pyrocko toolbox. Through such joint data optimizations from near- and far-field observations the determination of rupture parameters and processes will become more accurate and robust. Moreover, we present an intuitive kinematic deformation modelling sandbox for handling and manipulating various kinds of tectonic and volcanic deformation sources, interacting in elastic homogeneous or layered, full- or half-spaces.