For this assignment, we had to pick a type of thematic map, and create
data for the poverty levels in the United States. I chose quantile
mapping, because I found it to be the most aesthetically appealing,
while still displaying accurate data (!!NOTE!! Louisiana does not have
data, and I could not find an efficient and accurate way to enter it, so
all values in that area are set to zero).
As you can see, the areas with the most poverty are mostly in the south, with a small patch in the northern USA. Why did I pick this map? While the alternatives did add more accurate detail, they made for a cluttered and messy overview, especially when you take into account that the data was separated by counties. However, one problem I experienced with quantile mapping was that it seemed to be incompatible with Alaska and Hawaii... This type of mapping did not appear to register with them, and failed to produce any results.
Despite the problems, I actually find that this map is very effective. I went about creating it by first using kriging to organize and group the data, then, I went about and transformed that data into a more visually appealing map. This was accomplished by using the Geostatistical Analyst tool, the Geostatistical Wizard, and properly entering the data.
Tuesday, April 10, 2012
Thursday, March 29, 2012
Chapter 6 Maps
Here are the maps that I created for our chapter 6 assignment. The information and processes that went behind their creation can be found in my post "Chapter 5 and 6 Essays".
A normal QQ Plot, derived from USGS earthquake data. |
Covariance (top) and semivariance (bottom) graphs. |
Trend Analysis Chart, from same source. Notice how it has the rough outline of the United States (source material). |
A Voronoi Map, same source. Again, see if you can make out the rough outline of the USA. |
Chapter 5 and 6 Essays
I forgot to post my essay for chapter 5, so I thought I would combine the two into one post and save some time.
Chapter 5
Using
the information gathered with the three maps (IDW, Kriging, and Spline), I have
determined that the highest values of fecal coliform levels reside in the
northern part of the study area. The IDW
and spline maps show that the levels have the highest concentration in the very
northernmost tip, whilst the kriging map shows that they are most prominent in
the northwest portion of the map. By
examining all three and comparing them, I was able to average out the three
sets of data and come to my conclusion that the fecal coliform levels are
mostly present in the northern area of the map, mainly in the northernmost
area, with a smaller concentration in the middle of the map.
Chapter 6
In this
assignment, we had to take earthquake data from the USGS and create points on
our map, by taking the data from an Excel file we were to create. Using this data, I was able to find out that
the west coast of the United States had approximately 4960 earthquakes, and the
east coast had approximately 529, from the period of January 1st
2010 to February 1st 2012. I
was able to create many charts and maps, detailing both depth and magnitude
(these will be posted to my blog and to the EMU website. However, using the information, I was able to
find that the center of the earthquakes (the point in the middle of each set of
data) was in the northeast portion of Nevada.
Using a
normal QQ Plot, I was able to find that the magnitude of these earthquakes was
fairly consistent and “normal” in a mathematical sense. Most points were able to be plotted normally
along a straight line, with very little variance at the ends (there were a few
points that were at the extremes of each end).
The most powerful was recorded at a magnitude of 18, and appeared to be
near Virginia. This occurred on
4/24/2011. In the end, I was very
surprised by how many earthquakes were on the east coast, and that the most
powerful one was as well.
Thursday, March 15, 2012
Lesson 5 Assignments
Tuesday, February 21, 2012
Lesson 4
This is my map for lesson 4. Here is the paper I wrote describing it:
For this lab, I
used the Little Colorado River dataset.
To find it, I looked it up on Google Maps, and then found the
approximate location on the USGS Seamless Server. To derive the sediment transport index, I
used a variety of steps which we learned in class. What follows is a summary of what I did. First, I unzipped the DEM and loaded it into
ArcGIS. Then, I took the DEM and
converted it from the GCS North America 1983 geographic coordinate system into
the USA Contiguous Albers Equal Area projected coordinate system.
After
inserting the new map into a new dataframe, I filled the sinks and created a
new raster from that data. Then, I
created Flow Accumulation and Direction maps.
Next, I used the raster calculator to find streams with a value greater
than that of 3000. After using this data
to create a stream network map, I used the stream to feature function to create
a vector map from the stream link data.
Then,
I created a pour point at the beginning of the Little Colorado River, and
calculated a watershed like I did in Lesson 3.
I also did the operations to calculate sediment deposition. When creating my map, I had a great deal of
difficulty including the sediment data into the map. I couldn’t fit the entire stream data into my
map, so I included the watershed of the area, and a legend with the Sediment
Deposition per Square Meter. I apologize
if this isn’t exactly what was asked for, and I can make changes if needed.
Wednesday, February 15, 2012
Adventures in ArcGIS! Watersheds
For this assignment, we had to construct a watershed chart for a specific area. I chose Mason county in Michigan. First, I went to the Seamless Server and downloaded a DEM of the county, and converted it to the proper measurements for ArcGIS. Then, went through various processes, including creating a pour point. The steps I took can be found within the Model Builder Model, which I will include below. This assignment went smoothly, and I encountered few problems overall.
Stream Network of Mason County, including all streams with a value greater than 3000. |
Watershed of northern stream network in Mason County. Notice the pour point, where the watershed meets Lake Michigan in the farthest left side of the map. |
The Model Builder Model. This details the steps I took to create the Watershed Map. |
Washtenaw and Wayne Maps
Note from Matt: It seems that Blogger has failed to properly post my maps. Way to go, site! In lieu of the lost maps, I will attempt to recreate the post with the best of my memory (however shoddy it may be).
The following maps are based on various filters available in ArcGIS.
The following maps are based on various filters available in ArcGIS.
TIN Map |
Aspect Map |
Hill Curve Map |
Hillshade Map |
Slope Map |
Wednesday, January 18, 2012
Adventures in ArcGIS! Part 1
Today, I experimented in the art of creating 3D models in ArcGIS 10. More specifically, I worked on getting my 3D maps to display different kinds of data, such as slope models. Speaking of which, I was able to create a 3D slope model of Washtenaw and Wayne counties in Michigan:
With this model, the red areas are those of sharper slope, while the green areas are those of gentler slope. To make this map, I first downloaded digital elevation model data from michigan.gov/cgi, and loaded it into ArcMap. I then mosaic'ed the rasters together, making sure I used the Focal Mean tool to eliminate any seams in the image. After that, I converted the raster to a TIN file, and loaded the file in ArcScene. After doing that, I converted the DEM file I created earlier into slope data, and draped it over the TIN, creating the image you see above. I have also done work with draping orthophotos over this TIN as well:
This is the Manchester area, as viewed when draped upon the aforementioned TIN file. This picture constitutes the NW, NE, SW, and SE areas of the village.
Here is a hillshade map, using the slope raster.
This is an aspect map, showing which direction each hill faces.
And a curvature map.
With this model, the red areas are those of sharper slope, while the green areas are those of gentler slope. To make this map, I first downloaded digital elevation model data from michigan.gov/cgi, and loaded it into ArcMap. I then mosaic'ed the rasters together, making sure I used the Focal Mean tool to eliminate any seams in the image. After that, I converted the raster to a TIN file, and loaded the file in ArcScene. After doing that, I converted the DEM file I created earlier into slope data, and draped it over the TIN, creating the image you see above. I have also done work with draping orthophotos over this TIN as well:
This is the Manchester area, as viewed when draped upon the aforementioned TIN file. This picture constitutes the NW, NE, SW, and SE areas of the village.
Here is a hillshade map, using the slope raster.
And a curvature map.
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