Dealing with earthquakes and other non-linear motions

Slides:



Advertisements
Similar presentations
Anomaly Detection in Problematic GPS Time Series Data and Modeling Dafna Avraham, Yehuda Bock Institute of Geophysics and Planetary Physics, Scripps Institution.
Advertisements

Track Short Course: Track Introduction and Commands Lecture 01 Thomas Herring, MIT Room A
Earth, Atmospheric and Planetary Sciences Massachusetts Institute of Technology 77 Massachusetts Avenue | A | Cambridge MA V F.
The Community Geodetic Model (CGM): What is it and how does it relate to studies of lithospheric rheology? Jessica Murray, David Sandwell, and Rowena Lohman.
Generating velocity solutions with globk
Survey-mode measurements and analysis M. Floyd K. Palamartchouk Massachusetts Institute of Technology Newcastle University GAMIT-GLOBK course University.
“Real-time” Transient Detection Algorithms Dr. Kang Hyeun Ji, Thomas Herring MIT.
Examples of track use M. Floyd K. Palamartchouk Massachusetts Institute of Technology Newcastle University GAMIT-GLOBK course University of Bristol, UK.
 ss=  * +(a-b) ln(V/V * ) a-b > 0 stable sliding a-b < 0 slip is potentially unstable Correspond to T~300 °C For Quartzo- Feldspathic rocks Stationary.
July 17, 2002Zambia GNSS Earth Science Global Navigation Satellite Systems (GNSS) for Earth Sciences Prof. Thomas Herring, Massachusetts Institute.
New Scientific Applications with Existing CGPS Capabilities Earthquakes, Soil Moisture, and Environmental Imaging Andria Bilich Geosciences Research Division.
TIME SERIES by H.V.S. DE SILVA DEPARTMENT OF MATHEMATICS
Earth, Atmospheric and Planetary Sciences Massachusetts Institute of Technology 77 Massachusetts Avenue | Cambridge MA V F
SNARF: Theory and Practice, and Implications Thomas Herring Department of Earth Atmospheric and Planetary Sciences, MIT
Earth, Atmospheric and Planetary Sciences Massachusetts Institute of Technology 77 Massachusetts Avenue | Cambridge MA V F
Dealing with earthquakes and other non-linear motions T. A. Herring R. W. King M. A. Floyd Massachusetts Institute of Technology GPS Data Processing and.
Using GPS and InSAR to study tectonics, deformation, and earthquakes GPS displacements, velocities (and transients) InSAR displacements.
Issues in GPS Error Analysis What are the sources of the errors ? How much of the error can we remove by better modeling ? Do we have enough information.
Earth, Atmospheric and Planetary Sciences Massachusetts Institute of Technology 77 Massachusetts Avenue | Cambridge MA V F
Data weighting, and dealing with earthquakes and other non-linear motions M. Floyd K. Palamartchouk Massachusetts Institute of Technology Newcastle University.
Survey-mode measurements and analysis T. A. Herring R.W. King M. A. Floyd Massachusetts Institute of Technology GPS Data Processing and Analysis with GAMIT/GLOBK/TRACK.
Error Modeling Thomas Herring Room ;
Vertical velocities at tide gauges from a completely reprocessed global GPS network of stations: How well do they work? G. Wöppelmann 1, M-N. Bouin 2,
Introduction to the modelling of GPS results GPS provides Surface crustal velocities in a global reference frame, or with respect to a block, realized.
Aug 6, 2002APSG Irkutsk Contemporary Horizontal and Vertical Deformation of the Tien Shan Thomas Herring, Bradford H. Hager, Brendan Meade, Massachusetts.
Issues in GPS Error Analysis What are the sources of the errors ? How much of the error can we remove by better modeling ? Do we have enough information.
Limits of static processing in a dynamic environment Matt King, Newcastle University, UK.
Future Directions and Capabilities of Simulators Jim Dieterich
Modeling Problems & Signals
Evaluation of transient deformation from continuous GPS time series in Western North America ( ) Yehuda Bock1, Brendan W. Crowell 1, Danan Dong.
Contemporary Horizontal and Vertical Deformation of the Tien Shan
Information for virtual participants
Generating time series with glred
Motion of Bering Plate? Jeff Freymueller.
GPS measurements in the field
Dealing with earthquakes and other non-linear motions
Generating velocity solutions with GLOBK
Hector Mine & Landers Earthquakes
Generating time series with glred
Velocities in ITRF – not appropriate for interpretation
Kinematic Modeling of the Denali Earthquake
Samik Sil (1) and Jeffrey T. Freymueller(2)
Generating velocity solutions with GLOBK
Basics of processing workflow for GAMIT/GLOBK
GLOBK Velocity Solutions
Geodesy & Crustal Deformation
學生:林承恩(Cheng-en Lin) 指導老師:陳卉瑄(Kate Huihsuan Chen)
Basics of GPS processing workflow
Geodesy & Crustal Deformation
Tsunamis.
Using the Global Positioning System (GPS) to Measure Plate Motion
Generating time series with glred
Generating velocity solutions with globk
Track Output Interpretation
Earthquake Magnitude Ahmed Elgamal
Principles of the Global Positioning System Lecture 14
Principles of the Global Positioning System Lecture 11
Track Output Interpretation
GPS: GLOBAL POSITIONING SYSTEM Satellites transmit radio signals Receivers on ground record signals and find their position from the time the signals arrive.
DeltaV Neural - Expert In Expert mode, the user can select the training parameters, recommend you use the defaults for most applications.
Ken Creager, Wendy McClausland and Steve Malone
by Laura M. Wallace, Spahr C
Generating velocity solutions with globk
M. A. Floyd Massachusetts Institute of Technology, Cambridge, MA, USA
Generating time series with glred
Generating time series with glred
Generating velocity solutions with globk
Basics of processing workflow for GAMIT/GLOBK
M. A. Floyd Massachusetts Institute of Technology, Cambridge, MA, USA
Basics of processing workflow for GAMIT/GLOBK
Presentation transcript:

Dealing with earthquakes and other non-linear motions M. A. Floyd Massachusetts Institute of Technology, Cambridge, MA, USA School of Earth Sciences, University of Bristol United Kingdom 2–5 May 2017 Material from T. A. Herring, R. W. King, M. A. Floyd (MIT) and S. C. McClusky (now ANU) http://web.mit.edu/mfloyd/www/courses/gg/201705_Bristol/

Earthquakes and Non-linear 2017/05/05 Outline Previous lecture showed common time series models Linear rate Seasonal terms Temporally correlated noise Irregular perturbations to such models include Discontinuities due to equipment or environment changes Discontinuities due to earthquakes Non-linear motions due to earthquakes Non-linear motions due to transient events (e.g. volcanic inflation episodes) Recommended implementation 2017/05/05 Earthquakes and Non-linear Earthquakes and Non-linear

Earthquakes and Non-linear Changes to equipment Antenna is main concern, although receiver may also affect continuity of calculated position Even antennas of the same model type may not be manufactured within acceptable geodetic tolerance stinf_to_rename useful for creating automatic list 2017/05/05 Earthquakes and Non-linear

Changes in multipath environment 2017/05/05 Changes in multipath environment Photograph by M. Floyd Photograph by M. Floyd Photograph by R. Haught Photograph by R. Haught SB4 showing November 2013 fire (http://cdfdata.fire.ca.gov/incidents/incidents_details_info?incident_id=932). GPS antenna (TG01) in upper right. 2017/05/05 Earthquakes and Non-linear Earthquakes and Non-linear

Earthquakes and Non-linear Rename scheme Rename scheme uses first character of suffix XXXX_GPS → XXXX_2PS → XXXX_3PS → … etc. Beyond “9PS”, convert to 10th letter of alphabet (“JPS”) and beyond … → XXXX_9PS → XXXX_JPS → XXXX_KPS → … etc. But remember “XPS” is a special case for excluding sites from globk runs For manual renames (e.g. due to manual inspection rather than known events), use 8 available letters in alphabet before “J” XXXX_APS, XXXX_BPS, etc. But remember “GPS” is a special case (the default) 2017/05/05 Earthquakes and Non-linear

Earthquakes and Non-linear Earthquakes occur at known times May exhibit more than just a discontinuity Take care when earthquake occurs in the middle of processing day Some data will fall before and some after ground displacement Time series point on day of earthquake may appear between pre-earthquake and post-earthquake position 2017/05/05 Earthquakes and Non-linear

Earthquakes and Non-linear Radius of influence eq_def line in eq-file contains earthquake ID (two characters), location, etc. ID is used to substitute last two characters of 8-character site name, e.g. XXXX_GPS → XXXX_GSN sh_makeeqdef will search archives (ANSS ComCat or ISC) to generate eq_def records 2017/05/05 Earthquakes and Non-linear

Earthquakes and Non-linear Non-linear motions Logarithmic decay Exponential decay Derives from afterslip on fault plane controlled by rate-and-state friction (e.g. Marone et al., 1991) Velocity perturbation reduces with 1/t Derives from assumption of viscoelastic relaxation in stressed medium, e.g. after an earthquake 2017/05/05 Earthquakes and Non-linear

Earthquakes and Non-linear Non-linear motions Logarithmic decay Exponential decay Logarithmic looks good in East; Exponential looks good in North; Height doesn’t care 2017/05/05 Earthquakes and Non-linear

Earthquakes and Non-linear Many earthquakes… Complications arise in a tectonically active area with multiple events Sites may be renamed several times and therefore have various two-character suffixes Non-linear motions may be included in apr-file with “EXTENDED” records (see globk help) 2017/05/05 Earthquakes and Non-linear

Earthquakes and Non-linear Undocumented effects 2010-04-04 Mw7.2 Time series inspection is very important to catch undocumented effects Insert manually-determined discontinuities using letter for first character of suffix ? Jump is due to washer removal from top of the antenna. ? 2017/05/05 Earthquakes and Non-linear

Earthquakes and Non-linear Other phenomena Several examples of other phenomena some of which are likely to be motions of the monuments (often not tectonic), propagation medium effects, or failed equipment. With continuous data these types of effects can often be diagnosed from the data. For artifact effects, multipath and SNR measures are often useful for diagnostics. 2017/05/05 Earthquakes and Non-linear

Earthquakes and Non-linear Bombay Beach Creep? 2017/05/05 High light FOGMEX rate sigma (red sloped lines). Vertical rate of El Major Cucapah (2010/04/04) 2017/05/05 Earthquakes and Non-linear Earthquakes and Non-linear

Episodic events: Yellowstone Profile of velocity estimates across region. Large error bars (FOGMEX) show systematic sites List of noisy sites 2017/05/05 Earthquakes and Non-linear

Selected Yellowstone time series 2017/05/05 Earthquakes and Non-linear

Episodic Tremor and Slip (ETS): Cascadia 2017/05/05 Annual in height but east is ~14 months (notice offsets move relative to sinusoidal wave). 2017/05/05 Earthquakes and Non-linear Earthquakes and Non-linear

Earthquakes and Non-linear Other examples The following examples are from the UNACVO GAGE Data technical news: http://plus.google.com/u/0/communities/112834235701900858710 Reports here on various anomalies that have been detected and investigated. Useful place to look for site issues. GAGE ACC quarterly reports also contain information on anomalies 2017/05/05 Earthquakes and Non-linear

Earthquakes and Non-linear Local collapse Site EOCG http://plus.google.com/u/0/communities/112834235701900858710 2017/05/05 Earthquakes and Non-linear

Earthquakes and Non-linear Landslide prone site Location of earlier landslide showing strong seasonal 2017/05/05 Earthquakes and Non-linear

Earthquakes and Non-linear Ground water P271 Site P271 is strongly affected by ground water withdrawal There are also horizontal periodic signals as well 2017/05/05 Earthquakes and Non-linear

Earthquakes and Non-linear Vegetation Growth P158 North (not shown) is less affected. 2017/05/05 Earthquakes and Non-linear

Earthquakes and Non-linear 2017/05/05 Bad antennas Red lines are Hector Mine and El Mayor Cucapah. 2017/05/05 Earthquakes and Non-linear Earthquakes and Non-linear

Earthquakes and Non-linear Snow on antenna 2017/05/05 Earthquakes and Non-linear

Skewed position residuals: Atmosphere delays? 2017/05/05 Site sits near two high volcanoes with a NS valley between the volcanoes. 2017/05/05 Earthquakes and Non-linear Earthquakes and Non-linear

Earthquakes and Non-linear Recommendations Know your goals Only fit “nuisance” terms It is usually best not to try to fit signals that you are interested in, e.g. seasonal terms if you are studying these. Depending on your goal (e.g. linear tectonic velocities), sometimes you just have to abandon data as it is likely to do more harm than good (rename to xxxx_XPS or xxxx_XCL). Adding large process noise in GLOBK is one approach but be careful not to make too large. GLOBK sig_neu command can be used for small duration “bad” events. 2017/05/05 Earthquakes and Non-linear