The importance of prefiltering.

Slides:



Advertisements
Similar presentations
Functions with Inverses Functions with Inverses
Advertisements

Figure S1: Reaction mechanisms of NRs lacking CTDs alter channel kinetics. Kinetic models optimized by fitting 5C2O open state models to entire records.
Seismic Reflection Ground Roll Filtering Ted Bertrand SAGE 2004.
Notes Over 6.4 Graph Sine, Cosine Functions Notes Over 6.4 Graph Sine, Cosine, and Tangent Functions Equation of a Sine Function Amplitude Period Complete.
Objectives: Define and explain the components of the slope-intercept form of a linear equation. Use the slope-intercept form of a linear equation. Standards.
Depth (m) Time (s) Raw Seismograms Four-Layer Sand Channel Model Midpoint (m)
3,000Ft 4,000Ft 5,000Ft O2O2 O2O2 O2O2 O2O2 O2O2 O2O2 O2O2 O2O2 O2O2 O2O2 O2O2 O2O2 O2O2 O2O2 O2O2 O2O2 O2O2 O2O2.
Joint Migration of Primary and Multiple Reflections in RVSP Data Jianhua Yu, Gerard T. Schuster University of Utah.
McDaniels – Dec 5, Outline ADC Calculations – Estimation of placement uncertainty – Effect on Set 1 and Set 2 values.
1 Press Ctrl-A ©G Dear 2010 – Not to be sold/Free to use Distance between Two Points. Stage 6 - Year 11 Applied Mathematic (Preliminary Extension 1)
Analyzing Functions Inverses and Combinations Polynomial and Radical Functions Rational and Logs/Exp Functions
FRONT- I50 sq. ft. BACK-150 sq. ft. SIDE-80 sq. ft. + SIDE-80 sq. ft. 460 sq. ft. 460 sq. ft. 460 ÷ 10 =46 gallons , x x 46.
Goal: Graph horizontal and vertical lines Eligible Content: A / A
Possible exam questions for the chapter 10 exam. A.1175 in 2 B.1000 in 2 C.65 in 2 D.130 in
Tapering and prewhitening fFT taper, h(u). Need for prewhitening/prefiltering periodogram is generally biased.
Fundamentals Introduction Seismic waves: Propagation Velocity and Amplitudes Seismogram Measurement systems Sources, receivers, Acquisition strategies.
Calculating Components. Vector Projections It often becomes necessary to find the projection of one vector across the length of another. When this is.
ENGR 107: Engineering Fundamentals Lecture 8: Engineering Estimations & Data Acquisition C. Schaefer October 13, 2003.
$100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300.
Spiking Deconvolution In order to compress seismic signal in time and whiten the spectrum. Advantages: shows embedded signal in noise Disadvantages: heightens.
How to Read, Develop, and Interpret GRAPHS! OBSERVATIONS: often are recorded in a data table. We INTERPRET our data table by making INFERENCES and PREDICTIONS.
Section 3.5 Graphing Techniques: Transformations.
How to Read, Develop, and Interpret GRAPHS!  OBSERVATIONS: often are recorded in a data table  INTERPRET (make inferences of) your  DATA TABLE by performing.
Graph Y-Intercept =(0,2) Horizontal Asymptote X-Axis (y = 0) Domain: All Real Numbers Range: y > 0.
Notes Over 14.2 Translations of Trigonometric Graphs Translation of a Sine Function Amplitude Period.
Measuring Earthquakes (5-2 Notes). Magnitude = a measure of an earthquake’s strength Based on seismic waves.
4.1 NOTES. x-Axis – The horizontal line on the coordinate plane where y=0. y-Axis – The vertical line on the coordinate plane where x=0.
Check it out! : Constructing Functions from Graphs and Tables.
1 SITE RESPONSE ANALYSIS USING MICROTREMORS Boğaziçi University Kandilli observatory and Earthquake Research Institute Department of Geophysics Korhan.
Gray Area: Edgewater Construction Elevation Build up, No Data 01 ft. Storm Surge Gray Area: Edgewater Construction Elevation Build up, No Data NOTE: No.
Algebra 2 Notes May 20, Homework #63 Answers 1) 4) 7) direct; 8) inverse; 12) neither 13) 17) A varies jointly with b and h 18) h varies directly.
Extraction of surface impedance from magnetotelluric data
Susan L. Beck George Zandt Kevin M. Ward Jonathan R. Delph.
A bank of band-pass filters
Profs. Charles A. DiMarzio and Stephen W. McKnight
Objective: Computing work.
An Example. The question Data Analyses Conclusions.
6.4 GARCH models..
فاز سوم تدوين استراتژيهاي سازمان
NY Times 25 November 2008.
With joint time series data and either a bivariate model, data (X(t),Y(t); t = 0,...,T-1) or a regression/transfer function model the following R functions.
Acoustic Reflection 2 (distance) = (velocity) (time) *
9-4 Quadratic Equations and Projectiles
Detection of Mobile Fluids
ARCH(m) Example. S&P/TSX Capped Composite
An ARCH(m) example S&P/TSX Capped Composite 4/26/2010 to 4/26/2013
Click to see each answer.
postscript(file="sales.eps",paper="letter")
5.4 GARCH models..
Speech Pathologist #10.
The Importance of Informal Sector Statistics
Example I: F.T. Integration Property
Comparison of Seismic and Well Data
Celtic Sea Dublin, 12 September 2018
Calculating Averages with
Shot Gather For Shot 1 Source Receivers R1 R2 R3 R4 R5 S1
Raw Data - Marine SLIDE 6 Here is a display of raw seismic data – what would be recorded for one shot/explosion (marine example) The horizontal scale is.
Casing Gen DE axial recorded at different speeds and at load
Review of Coherent Noise Suppression Methods
Slope 3.5 Rate and Slope Horizontal and Vertical Lines Applications.
Medium effects on waves Reflection/refraction
Noise and Requirement of BRT
Record your QUESTIONS as your read.
Locating an Earthquake's
Teacher This presentation describes how to locate, download and use the Summative Test resources. Please allow about minutes to go through the presentation.
D × t % A Wt. of liquid Wt. of water × dwd =.
Completely labeled graph
1. Recognized $80,000 of revenue on account.
a. What is the accounting term for this type of acquisition?
a. Record the above transactions in general journal form.
Presentation transcript:

The importance of prefiltering. The estimates are generally biased E{ fT()} =  WT (-) f() d Seismic noise horizontal components recorded at UCB Estimated coherence can be 1,0 when no relation Estimated coherence can be 0.0 when linearly time invariantly related

postscript(file="seismic.eps") junkx<-scan("ts_drb.16.dat") junky<-scan("ts_drb.17.dat") par(mfrow=c(2,1)) xaxis<-c(1:2500)*.08 plot(xaxis,junkx,type="l",main="Vertical component seismic noise at Berkeley",xlab="time (sec)",ylab="",las=1) plot(xaxis,junky,type="l",main="West component",xlab="time(sec)",ylab="",las=1) par(mfrow=c(2,3)) junk<-spec.pgram(cbind(junkx,junky),spans=15,taper=0,detrend=F,demean=T,plot=F) junk$freq<-junk$freq/.08 plot(junk$freq,junk$spec[,1],type="l",las=1,main="Vertical noise",xlab="frequency (hertz)",log="y") plot(junk$freq,junk$spec[,2],type="l",las=1,main="West noise",log="y") plot(junk$freq,junk$coh,type="l",ylim=c(0,1),main="Raw data",las=1) abline(h=1-(1-.95)^(1/(.5*(junk$df-2))))

junkxx<-ar(junkx,order.max=2) junkyy<-ar(junky,order.max=2) Junkx<-junkxx$resid Junky<-junkyy$resid Junkx<-Junkx[3:length(Junkx)];Junky<-Junky[3:length(Junky)] Junk<-spec.pgram(cbind(Junkx,Junky),spans=15,taper=0,detrend=F,demean=T,plot=F) Junk$freq<-Junk$freq/.08 plot(Junk$freq,Junk$spec[,1],type="l",las=1,log="y") plot(Junk$freq,Junk$spec[,2],type="l",las=1,log="y") plot(Junk$freq,Junk$coh,type="l",ylim=c(0,1),main="AR(2) residuals",las=1) abline(h=1-(1-.95)^(1/(.5*(junk$df-2)))) graphics.off()