scispace - formally typeset
J

Joachim Wassermann

Researcher at Ludwig Maximilian University of Munich

Publications -  112
Citations -  5383

Joachim Wassermann is an academic researcher from Ludwig Maximilian University of Munich. The author has contributed to research in topics: Seismometer & Rotation. The author has an hindex of 29, co-authored 107 publications receiving 4126 citations. Previous affiliations of Joachim Wassermann include University of Potsdam.

Papers
More filters
Journal ArticleDOI

ObsPy: A Python Toolbox for Seismology

TL;DR: ObsPy as discussed by the authors is a Python toolbox that simplifies the usage of Python programming for seismologists by providing direct access to the actual time series, allowing the use of powerful numerical array-programming modules like NumPy (http://numpy.thz.edu/manuals/sac/Manual.html), as well as filtering, instrument simulation, triggering, and plotting.

ObsPy: A Python Toolbox for Seismology

TL;DR: ObsPy as mentioned in this paper is a Python toolbox that simplifies the usage of Python programming for seismologists by providing direct access to the actual time series, allowing the use of powerful numerical array-programming modules like NumPy (http://numpy.mathworks.org) or SciPy(http://scipy.org).
Journal ArticleDOI

ObsPy: a bridge for seismology into the scientific Python ecosystem

TL;DR: ObsPy (http://obspy.org), a Python library for seismology intended to facilitate the development of seismological software packages and workflows, is developed to utilize these abilities and provide a bridge for seismologists into the larger scientific Python ecosystem.
Journal ArticleDOI

Global quieting of high-frequency seismic noise due to COVID-19 pandemic lockdown measures.

Thomas Lecocq, +84 more
- 11 Sep 2020 - 
TL;DR: The 2020 seismic noise quiet period is the longest and most prominent global anthropogenic seismic noise reduction on record and suggests that seismology provides an absolute, real-time estimate of human activities.
Journal ArticleDOI

Evidence for rainfall‐triggered earthquake activity

TL;DR: In this paper, the pore pressure changes due to diffusing rain water and in good agreement with the response of faults described by the rate-state friction law are shown to trigger earthquakes in a few kilometres depth.