Showing posts with label lidar topography. Show all posts
Showing posts with label lidar topography. Show all posts

Friday, June 5, 2026

San Andreas Fault in the Carrizo Plain Field trips

Recently, I pulled together some notes for the SCEC UNREST Field trip in the Carrizo Plain. It was a great conversation to share with the esteemed colleagues.


So I can find it, here are the notes that produced as a handout: LINK

Here are a few other items/guides:

Friday, December 15, 2023

Open Science recognition prize at AGU 2023

Our OpenTopography project was honored at this year's AGU with the Open Science Recognition prize: "For outstanding contributions in cyberinfrastructure, data management, training, and outreach associated with open-access high-resolution topography." It is a great honor and nice reognition for more than 15 years of work by our team. Huge thanks to Roman DiBiase for leading the nomination and for the letter writers Mike Oskin, Paola Passalacqua, and Josh Roering.

Chelsea Scott and Chris Crosby made a nice presentation summarizing our efforts. The recording is here: link.

It was also nice to meet the other winner, Tasha Snow and appreciate her efforts. In particular, I really appreciated her articulation of Open Science values (image from her presentation):

The full award ceremony is recorded here: link.

Here are a couple of pictures of our team:

Other links:
OpenTopography news release: link

And we celebrated with the other ASU / SESE awardees (Vernon Morris and Everett Shock):

Sunday, May 14, 2023

Determining the cell size of a Digital Elevation Model from point density

We regulary refer to high resolution topography (HRT) as having Digital Elevation Model (DEM) pixel sizes with their edges less than 1 m. Many raster DEMs derived from airborne laser swath mapping available for example from OpenTopography are delivered at 1m/pix. In many cases, the point density might be high enough to support even higher resolution or smaller pixels. This seems like a fairly simple question: what is the recommended cell size of a DEM for a given point density?

The Langridge, et al., 2013 paper cites Hu, 2003 and suggests the following:

where S is the estimated cell size (typically in m), n is the number of sample points and A is the area containing the sample points.

Here is a little spreadsheet to solve this equation given A and n: link.

In the trivial case, that equation can be rearranged and show that 1 point per sq. m is consistent with a 1 m DEM. That seems ok in the sense that then on average there is one point for each pixel which would be the logic of this equation. It assumes then that the points are well distributed and that whatever average for point density that we might use to estimate a cell size represents the data well. A complication is the method of DEM computation: local function or linear interpolation. An example of the local implementation is the Points2Grid tool (see prototype here and here). Tinning or the use of triangular irregular networks linearly interpolates between (selected) points to estimate DEM pixel elevations (see blast2dem for example).

Here are some illustrations from the Jemez River Basin dataset cited below. These data have a stated point density of 9.68 points/sq. m and were computed within the OpenTopography portal using the TIN approach.
Here is an example from a site called Sulphur Creek (1 m/pix for this Digital Surface Model, DSM):


Here is a zoom to that site with the 1m/pix DSM hillshade and 14% of the points displayed from ArcMap. We can see the 1 m pixels and that there are a decent number (about 9.7) of points for each one. This has all of the points (all classes):
Here is the same view but with a 0.32 m/pix (recommended resolution from equation above), but applied to the Digital Terrain Model (DTM). Note this is not really correct resolution estimate because the number of points classified as ground is only about 1/5 of the total. And, this shows the ground returns only.
Zooming in even more, we can see the big triangular facets where the TINNING algorithm spanned the data gaps in the ground classified points for this 0.32 m/pix DTM:
Finally, zooming back out with the 1 m/pix DTM displayed, we can see that at this scale, the DTM landscape is well represented in general. We do need the interpolation by tinning across the gaps in the ground points:

References Hu, Y., 2003. Automated Extraction of Digital Terrain Models, Roads and Buildings Using Airborne LiDAR Data (PhD thesis). Department of Geomatics Engineering, The University of Calgary, Calgary, Alberta, Canada.

Jemez River Basin Snow-off LiDAR Survey. Distributed by OpenTopography. https://doi.org/10.5069/G9RB72JV . Accessed: 2023-05-14

Langridge, R.M., et al., Developing sub 5-m LiDAR DEMs for forested sections of the Alpine and Hope faults, South Island, New Zealand: Implications for structural interpretations, Journal of Structural Geology (2013), http://dx.doi.org/10.1016/j.jsg.2013.11.007

Saturday, October 5, 2019

(Finally) Getting going with python (and a bit of history)

I certainly recognize the power of scientific programming. Programming spreadsheets is obvious and there is nothing to be ashamed of there (see weeks 2-6 in my Computers in Earth and Space Exploration course). I started off in grad school with Mathemematica and appreciated the notebook style of computations and integrated graphics and text. I also taught myself enough fortran to get the main calculations for my dissertation completed.


Modeling profile development with simple diffusion (Arrowsmith, et al., 1998) using fortran code and Mathematica for the basic graphics.

I took some programming courses (Pascal) back in grad school. I was not very good at it. Once the professor even said "that is the stupidest way I have ever seen for doing that" in office hours. I was not too offended; I barely understood what I was doing. Nevertheless, I got the big picture and have stumbled along ever since.

Professor George Hilley taught me many things. One thing he was able to do after a fair amount of cajoling was to get me to start in MATLAB. The more data-oriented and matrix handling of MATLAB ended being something I could use effectively. We also worked with Don Ragan a lot on MATLAB and Latex. While I am no expert, I have taught the basics to students over the years see weeks 6-9 in my Computers in Earth and Space Exploration course). I cannot say that I have had any really great programming projects, but the various analysis and plotting needs have been satisfied. For what it is worth, I even set up a GitHub page to hold a few things. Dr. Olaf Zielke is a serious MATLAB programmer and wrote some impressive tools with GUIS for his PhD and related work. TopoToolbox is another set of MATLAB-based tools which I had the opportunity to learn and appreciate their transformative power for a lot of geomorphic analyses.

I have been watching the progressive adoption of Python and related tools in my little scientific bubble over the last 5 or so years. I have not had the time to do much as far as learning until recently, however. While my MATLAB expertise won't go away, I have appreciated the fact that it is hard to share and teach with students and colleagues who don't have access to the rather expensive licenses for MATLAB. On the other hand, Python and related tools are open and apparently so adaptable and customizeable.

Recently, I finally had an excuse and the time to get my feet wet with Python. Chris Crosby and I (OpenTopography) helped out with a short course From point clouds and full-waveform data to DEM analysis (Sep-30 to Oct-4 2019) led by Professor Bodo Bookhagen and his team.


Specific catchment area computed with the tools from Rheiwalt, et al., 2019. The basic processing was in Python with some c code and then visualized using Displaz.

Here is some basic full waveform lidar processing from Bookhagen and Rheinwalt again basic procesing in Python and then visualized using Displaz.

I still don't understand all that I am doing, but I got the basic set up and can sort of understand packages and environments. Javier Colunga helped me by getting Ananconda installed. Spyder is the development environment I had been looking for. There is so much that is possible; it is hard to even know where to start.

For my first project, I thought it would be nice to play around with a lidar point cloud (using the Dragon's Back of course): grid it using pdal and then make a hillshade using gdal. Download the data from OpenTopography.

The steps are:

  1. Launch an Ananconda terminal.
  2. Add these conda channels for package install:
    conda config --prepend channels conda-forge/label/dev
    conda config --prepend channels conda-forge
  3. Then define an environment and add the packages using conda: conda create -y -n PC_py3 python=3.6 pip scipy pandas numpy matplotlib scikit-image gdal pdal xarray packaging ipython multiprocess h5py lastools pykdtree spyder gmt=5* (this comes from the workshop).

My first problem was that I could not run pdal from inside a python script. There is something I don't understand there (even though it is installed, etc.). I see that it is possible to call python from inside the pdal json files... But, I can run it from the command line:
> pdal pipeline db.json
where the db.json has the parameters for the simple neighborhood gridding run:


{
        "pipeline":[
        "smallpiece.laz",
        {
                "resolution": 1,
                "radius": 0.707,
                "gdaldriver": "GTiff",
                "gdalopts": "COMPRESS=DEFLATE, ZLEVEL=7, GDAL_NUM_THREADS=ALL CPUS",
                "data_type": "float",
                "output_type": "idw",
                "filename":"small_idw_1m.tif"
        }
        ]
}
I was able to make a little dem (the tif file). But then, I ran the gdal from the command line only:
>gdaldem hillshade small_idw_1m.tif small_idw_1m_shd.tif

Finally, I could run a little python script to draw the hillshaded geotiff (this I could run from Spyder):


#!/usr/bin/env python
import gdal
import matplotlib.pyplot as plt

ds = gdal.Open('small_idw_1m_shd.tif').ReadAsArray()

plt.close('all')

plt.imshow(ds, cmap='gray')

f.savefig('smallDB.png', dpi=300)
plt.close('all')


Small piece of the Dragon's Back lidar data (B4 project) gridded with pdal, hillshaded with gdal, and drawn with matplotlib

So, I guess that is a bit of a success, there is a lot more to do and learn!

I keep finding references to help learn:

Monday, February 25, 2019

Updated review of fault scarp analysis

I am organizing for a presentation to my research group on fault scarp analysis. This is an ongoing obsession of mine. I have blogged about this topic here with some review. That is still a pretty good summary of things. I also have a couple of relevant Landers Earthquake posts here and here. And, we applied many of the relevant tools to analysis of cinder cone forms.

The 2017 post mentioned above is still a pretty good summary of things. However, the MATLAB-based guis for Penck1D and Scarpdater are not running well now on newer versions of MATLAB; they need an overhaul. We were really into guis back then but they require so much code relative to the actual modeling. Might be cool to rewrite in Jupyter notebooks, maybe see how much in landlab could be used.

I have prepared a new review powerpoint (PPT and PDF) with this outline:

  • Introduction and review
  • Diffusion-equation analysis of scarplike landforms
  • Observations
    • Direct dating of fault scarps
    • Fault scarp erosion monitoring
  • Modeling
    • Distributed deformation
    • Transport vs. Production limited
  • Extending processes 2D and nonlinear diffusion
  • Prospects and cautions
Of course it is incomplete and emphasizes the work of my students and colleagues. I note for example, this nice review from Wei, et al., Journal of Asian Earth Sciences, 2015:

Additional resources for my lecture include:

Some other useful web links include:

Monday, June 5, 2017

Some new San Andreas Fault tour videos of 1 m bare earth hillshades

I have been preparing a lecture and I built some new simple videos flying along the San Andreas Fault. The videos are made by me flying along in Google Earth with 1 m hillshades produced from lidar topography data collected along the San Andreas Fault. The videos are on youtube in this play list: https://www.youtube.com/playlist?list=PLFfZSFyNZ_jZm86F1TsnYfuuYNef_Uh21. I also put the MP4s in this folder--they are numbered 1-8 from NW-SE.

The flights follow generally along the San Andreas Fault from Point Arena to the southern Carrizo Plain (Dragon's Back and Northern Elkhorn Hills):

The data were processed at www.opentopography.org and come from 3 really cool datasets:

Friday, May 5, 2017

Simple Topography Lectures at University of Geneva as part of CERG-C

I am visiting the University of Geneva as part of the CERG-C project. Professor Costanza Bonadonna is the leader of the activity which is a course on hazard and risk with an international group of students. They have been in Geneva for a few weeks for classroom work and starting tomorrow they go to Vulcano Island for practical experience. I am going to join.

I gave a lecture and a practical demonstration on the general topic of Topography, but trying to emphasize its fundamental value for science and applied value for hazard assessment. And, of course making the point that high resolution data are most useful.

Here are the pdfs to my lectures and demo:

Saturday, April 8, 2017

A pair of short courses on "Geoscience Investigations of Point Clouds" and "Advancing understanding of geomorphology with topographic analysis": mid June, 2017 at Potsdam University, Golm

Two short courses are scheduled for mid June at Potsdam University. The short courses are independent of each other; however, the topics are related and probably address a similar audience.

Geoscience investigations of point clouds, June 7-9, 2017. Instructors B. Bookhagen, R. Arrowsmith, M. Isenburg, C. Crosby.
This course will explore the acquisition, post-processing, and classification of point clouds derived from airborne and terrestrial lidar scanners and structure from motion (SfM) photogrammetry from drones. The course will take place at campus Golm (UP) and includes one day of field-data collection and two days of data post-processing and analysis.
The application is here: https://goo.gl/forms/NrRAcaASXPuseRs62. The course is sponsored by Geo-X.
Here is the flyer: PDF for more details.

Advancing understanding of geomorphology with topographic analysis emphasizing high resolution topography, June 12-15, 2017. Instructors R. Arrowsmith, W. Schwanghart, C. Crosby, B. Bookhagen.
This course will focus on advanced understanding of geomorphology with topographic analysis emphasizing high-resolution topography. The course will take place at campus Golm (UP) and includes theoretical background and analysis of digital topography using TopoToolbox in a Matlab environment. The course is sponsored by StRATEGy.
Here is the flyer: PDF for more details.

Thursday, March 16, 2017

Mapping landforms with applications to geomorphology and earthquake geology EXERCISE

I wanted to share a project I have developed on and off for about 10 years. It is a classroom exercise for Mapping landforms with applications to geomorphology and earthquake geology. So far, it has an example for strike-slip faults (Wallace Creek along the San Andreas Fault), and blind thrust faults (Wheeler Ridge in Southern California). I have an intention to add a normal fault example but have not finished it yet.

The basic idea is that the exercises could be done "analog"--that is on paper in a classroom. They emphasize some simple morphologic and geomorphic mapping (but on high resolution topography base maps from lidar data collected by NCALM and available for download from OpenTopography), and then provide landform ages so that students can calculate slip rate or surface uplift rates. I am not sure they are so well explained so any feed back is welcome.

Exercise material:

Saturday, October 1, 2016

NSF NEON WORKSHOP: TOPOGRAPHIC, GEOMORPHIC, AND VEGETATION ANALYSIS WITH LIDAR

Nancy Glenn (Boise State) led a training workshop with Chris Crosby (UNAVCO), Tristan Goulden & Shelley Petroy (NEON), and me this last week on topographic, geomorphic, and vegetation analysis with lidar. We emphasized the NEON project and its substantial Airborne Observation Platform with its lidar scanners. Tristan is the Remote Sensing Specialist with lidar expertise for NEON and in charge of those acquisitions. Shelley is the data products lead for all of NEON. It was quite interesting to learn more about NEON and also to see the interesting interdisciplinary opportunities for research. The participants came from a range of backgrounds and were a pleasure to meet and work with.

Shelley Petroy and Chris Crosby sharing their knowledge with the group

The workshop web site has some good lecture and exercise/tutorial content (look towards the bottom at the "Workshop Material" link. I built some simple videos (look for playlists on NEON Points to Raster and NEON OpenTopography, Topographic Metrics and Drainage Network) demonstrating some aspects of the tutorials. At OpenTopography, we have started to distribute NEON lidar data (NEON D17 Pacific Southwest- California).

We had a great time in Boise. The classroom was excellent and Nancy was kind to schedule a civilized stop time in the afternoon so there was time for a run before the pleasant evening receptions. Below is a picture from above Boise:

An interesting coincidence was that at the same time as our workshop and in Boise was the Subduction Zone Observatory Workshop. I could imagine having been at that meeting too!

Saturday, April 2, 2016

COMET Topography Workshop 31/3/2016 – 1/4/2016

The COMET Topography workshop just completed (31/3/2016 – 1/4/2016) with great success. It was hosted by the Oxford University Earth Sciences and ably lead by Austin Elliott (also active here: @TTremblingEarth). John Elliott, David Mackenzie, and Zhou Yu made important contributions. Professors Barry Parsons and Rich Walker provided oversight. I had a great time helping out with the workshop. It was great fun to share our enthusiasm for high resolution topography and to represent and present OpenTopography to the esteemed group of mostly earthquake faulting and volcano scientists.

The workshop emphasized topography produced from photogrammetric methods. The first emphasis was on more traditional photogrammetry applied to relatively high resolution space-based bi- or tri-stereo imaging (e.g., SPOT and Pleiades). The software of choice was ERDAS Imagine with its Photogrammetry Suite. I enjoyed learning more about this technology and these data which the Oxford team among others has been using with great success for characterizing active faulting.The second emphasis was on Structure from Motion--something I have some more experience with. It was great to see the strong interest and burgeoning expertise among the various participants as they apply this methodology with ground and UAV-based images to a range of faulting and volcanic problems. The OpenTopography workshops over the last couple of years have featured SfM as well (with great contributions from Ed Nissen). I got a good primer on georeferencing and networked SfM.

The workshop agenda is here: link.

See also this nice blog post about the workshop: link.


The group photo. Sunny moment in Oxford; lots of great scientific power here and a fun lot too! Photo by David Sandwell (Oxford University).


Introductory science motivations: "Sharpening our view of earth processes with high resolution topography". Photo by David Sandwell (Oxford University).

Tuesday, November 11, 2014

Fall 2014: PATA-Days in Busan, Korea

I had a wonderful trip to Busan, Korea for the Paleoseismology, Active Tectonics, and Archeoseismology (PATA Days) meeting. I really enjoyed it. It was great to see old and new friends, catch up on the latest developments, and to travel in southern South Korea.
Here is a presentation/overview I made for my students and colleagues for our seminar:
PPT
Here is the paper I wrote for the meeting: pdf.

I spent some nice time with my friends Koji Okumura and Shmulik Marco:

It was also an interesting trip because my father was based at the Pusan East (K-9) air base in 1951. He was curious to hear about the trip and mentioned that he turned 21 there. He said they played a lot of cards and that a few times he got to go off base to help his friends who worked at a reservoir.

Monday, September 29, 2014

Some TU Dresden SfM and lidar links

I got a nice tip from Univ.-Prof. Dr. Klaus Reicherter about some good structure from motion (SfM) and lidar links at the Technical University Dresden:


I also note for reference that we have the OpenTopography Tool Registry

Monday, March 31, 2014

Exploiting high resolution topography data for advancing the understanding of mass and energy transfer across landscapes: Opportunities, challenges, and needs (USGS Powell Center working group)

"TIME FOR IN-DEPTH ANALYSIS WITHOUT DISTRACTIONS"--That is one of the opportunities presented to USGS Powell Center Working Groups. Indeed and quite pleasantly we have begun our discussions in the working group entitled "Exploiting high resolution topography data for advancing the understanding of mass and energy transfer across landscapes: Opportunities, challenges, and needs". This project is lead by Paola Passalaqua (UT Austin) and Patrick Belmont (Utah State). Here is a flyer on our project: link. We had our first meeting a couple of weeks ago in Fort Collins at the Powell Center and it was extremely stimulating. Lots of great discussion and sharing of ideas among a dynamic group. I very much enjoyed seeing old and new friends. We mostly worked on brainstorming a big review of the state of analysis of high resolution topography and so I think there will be a publication coming from that. We also had a quite interesting field trip to appreciate the geomorphic responses to the High Park Fire (for which there is some repeat lidar topography coverage). Here are some pictures. Stay tuned for more cool stuff and many thanks to my friends and colleagues for the chance to work together.

Friday, February 28, 2014

Science videos: naive efforts and connecting with the pros (for example, http://lifeonterra.com/)

I have been playing around with video production for science explanation and tutorials since some efforts in graduate school for the The Stanford Rock Fracture Project. Lately, I have generated many tutorial and lecture videos and pushed then to my youtube site: jrarrowsmith youtube. There are also many videos, some have been viewed more than 10,000 times on the OpenTopography youtube site.

My friend Merri Lisa Trigilio is a geoscientist who is now in the Film program at Montana State University. It has been fun to talk to her about filmmaking and we will work together in the coming weeks on a video project. Stay tuned for updates. I the meantime, have a look at the Life on Terra website--run by the film students at MSU.

As part of a Southern California Earthquake Center (SCEC) and OpenTopography collaboration, Sarah Robinson (former ASU M.S. student) and Andrew Whitesides (USC undergraduate) - supported by SCEC's ACCESS program (Advancement of Cyberinfrastructure Careers through Earthquake System Science) and in collaboration with numerous SCEC scientists and the OpenTopography team - produced a new educational video entitled LiDAR - Illuminating Earthquake Hazards. The video provides an introduction to both LiDAR technology as well as the earthquake science that is being done with the data.

Thursday, January 23, 2014

Spring 2014 Active Faulting and Surface Process Seminars

We have two nice seminars going now: Active Faulting and Surface Processes.

We have started to run the Active Faulting seminar and track it the last few semesters. Thanks to Emily Kleber and the other students for taking the lead and organizing and documenting. Emily says: "This semester we are focused on discussing current research projects and trending topics in active tectonics and tectonic geomorphology. Subject matter is centered around (but not limited to) quantitative structural geology, geomorphology, paleoseismology, and the acquisition and application of high-resolution topography to all of the above." Here is the web site: http://activetectonics.asu.edu/ActiveFaultingSpring2014.html .

The Surface Process seminar has been going since at least Spring 2008. The topics vary and it is run in the evenings at a faculty member or student home. We enter the critical zone of commentary and sometimes the topic is about the Critical Zone (from the top of the canopy to the bottom of the roots). This semester's topic is generally hillslope processes.

Monday, September 2, 2013

Short Course at LIPI : Techniques in Active Tectonic Study

In July 2013, Gayatri Marliyani and I taught a short course at LIPI in Bandung, Indonesia on Techniques in Active Tectonic study. I put together almost 30 lectures on various topics in active tectonics, neotectonics, tectonic geomorphology, paleoseismology, earthquake geology, and related topics. Special thanks to Mudrik Daryono (course coordinator for LIPI/ITB/GREAT), Irwan Meilano (ITB/GREAT), Danny Hilman Natawidjaja (LIPI/GREAT), Eko Yulianto (LIPI/GREAT), and the participants.

Gayatri built a nice website with all of the freely available lectures and other course content. We also recorded most of the lectures and they are on youtube.

The course web site is: http://activetectonics.la.asu.edu/lipi/. Look under the schedule link for the lectures and the link for some exercise content.

Group picture on field trip along the Lembang Fault.

Exploring topographic response to interacting surface processes and rock uplift: the Dragon's Back Pressure Ridge along the San Andreas Fault, Carrizo Plain, CA


The Dragon's Back Pressure Ridge is an amazing landform along the San Andreas Fault in the Carrizo Plain of California. A recent paper in Science by Hurst, et al. examined it to explore how hillslope form might be used to indicate waxing and waning responses to a pulse of rock uplift. George Hilley (a coauthor on the recent paper) and I along with David Pollard and Dallas D. Rhodes have spent more than 20 years pondering and exploring the Dragon's Back. With this blog entry I want to highlight a few links for more information.

This is the main published paper on the Dragon's Back up to now: Hilley, G. E., and Arrowsmith J R., Geomorphic response to uplift along the Dragon's Back pressure ridge, Carrizo Plain, California, Geology, v. 36; no. 5; p. 367–370; doi: 10.1130/G24517A.1, 2008.

Ph.D. theses:

  • Arrowsmith, JR, 1995, Coupled Tectonic Deformation and Geomorphic Degrada tion along the San Andreas Fault Zone [Dissertation thesis]: Stanford, Stanford University.
  • Hilley, G. E., 2001, Landscape development of tectonically active areas [Dissertation thesis]: Arizona State University.

Hillshades and digital elevation model (B4 project data processed by OpenTopography):

Other links:

The digital elevation models that enabled much of the analysis discussed here come from the B4 project and the data and models are available from OpenTopography.
The B4 project created an unprecedentedly accurate surface model along the San Andreas and San Jacinto Faults in southern California that enabled the research reported here. It was supported by the U. S. National Science Foundation and led by Ohio State University and the U. S. Geological Survey. The National Center for Airborne Laser Mapping performed the airborne data acquisition and laser data processing. Optech International generously contributed use of the ALTM3100 laser scanner system. UNAVCO and SCIGN assisted in GPS ground control and continuous high rate GPS data acquisition. A group of volunteers from USGS, UCSD, UCLA, Caltech and private industry, as well as gracious landowners along the fault zones, also made the project possible.

Monday, March 18, 2013

LaDiCaOZ and Lateback: reconstructing horizontal offsets in topography websites for tools

Dr. Olaf Zielke developed some very useful tools for interacting with high resolution topography for horizontal back slip of offsets due to earthquakes. These were the tools for the science results presented in:

  • Zielke, O., Arrowsmith, J R., Grant Ludwig, L., Akciz, S. O., High resolution topography-derived offsets along the 1857 Fort Tejon earthquake rupture trace, San Andreas Fault, Bulletin of the Seismological Society of America, doi: 10.17850120110230, vol. 102 no. 3 1135-1154, 2012.
  • Zielke, O., Arrowsmith, J R., Grant Ludwig, L., Akciz, S. O., Slip in the 1857 and earlier large earthquakes along the Carrizo Plain, San Andreas Fault, Science, DOI: 10.1126/science.1182781, p. 1119–1122, 2010.
He also documented the approach and the software in this paper:
Zielke, O., and J R. Arrowsmith, LaDiCaoz and LiDARimager -MATLAB GUIs for LiDAR data handling and lateral displacement measurement, GeoSphere Special issue on high resolution topography, v. 8, no. 1, p. 206221, doi:10.1130GES00686.1, 2012.

Olaf is now at KAUST. His email address is: Olaf.Zielke@kaust.edu.sa.

He has made the supplemental on line material from the Geosphere paper available here.
And, the LaDiCaoz_LiDARimager tools and information is available on this dropbox link

This research was supported by the US National Science Foundation, the US Geological Survey, and the Southern California Earthquake Center.