Lab 5: Using Lidar Data
Introduction
To create accurate and high
resolution maps we need to use data that is not from Digital Elevation Models
which are becoming obsolete. The data that we need to use to create highly
accurate high resolution maps is known as LIDAR or Light Detection and Ranging.
This data is very interesting since it using UV Visible and NIR wavelengths to
map physical features by emitting a laser to the ground and measuring the
return rate. Using this data we can begin to create high resolution maps that
are useful for Agriculture, Geologic process, surveying and even mapping of the
ocean floor. Our application of LIDAR was to create basic hill shaded Digital
Terrain Models (DTM) and Digital Surface Models (DSM)
Goals
The main goal of this lab exercise
was to gain basic knowledge of lidar data structure and processing. The tasks
that we were required to do were the processing and retrieval of the various
surface and terrain models and to use this data to process and create a variety
of images and products from the point cloud developed by the lidar data.
Methods
To create these high resolution
maps we first downloaded the raw Lidar data from the assigned lab folder
provided. Using this data we created a new LAS data set named Eau_Claire_City. After
adding the LAS files to the data set window we were able to calculate and
project a coordinate system for the xyz axis. When this data was projected onto
ArcMap we were able to see the point cloud returns from the data. Using this
raw Lidar data we are able to warp the map based on elevation, contour lines,
aspect and slope. We were also using the lidar dat to create interactive views
by using the profile view tool in the LAS Toolbar
The power of Lidar, Returns of Phoenix park bridge
We were then able to create a DSM
and DTM by manipulating the LIDAR data. We used the Arc Tool box to create a
raster from the LIDAR data by following the route:
Conversion tools to raster> to las
dataset> to raster
This allowed us to create a DSM
based on the criteria that we selected. For our models we used parameters of
Binning, Cell Assignment set to maximum and natural neighbor as the void fill
method with a cell size of 2 meters per pixel for the raster. After the DSM was
completed we then created a Hillshade effect to the DSM.
DSM Raster before Hillshade
DSM after Hillshade
Next we created a DTM which would
only show the terrain of the area we were studying. We followed the same route
as the DSM but switched it to minimum cell assignment type. We also only looked
at the ground return of the LIDAR data. This will ignore all other returns
except for those marked by the ground effectively giving us a look at only the
terrain model.
We also created an Intensity image
that is only in black and white. This is very helpful for identifying features
where a lot of detail is needed.
Intensity Image
Results
The results involved us creating
new and exciting LIDAR maps based on DSM, DTM and Intensity. All of these will
allow us to use lidar data to our advantage. This will be helpful in geologic
practices, land use surveying and slope effects in the Eau Claire area.
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