This week, we learned more about projections. We learned how they work, how to identify the best projection for your intended purpose, how to create custom projections, and the science and history behind projections. Below, I created a map of my home state of Nebraska. I used the Nebraska State Plane Projection and added a grid and graticules.
Saturday, January 30, 2021
Map Projections
Tuesday, January 26, 2021
Typography and Labeling of the San Francisco Bay Area
For this week's exercise, we were tasked with labeling various features in the San Francisco Bay area. Below is the map I created:
I chose Sitka font
for this project because I felt like a serif font helped me read smaller type.
For each respective category, I changed the font size from large to small
depending on the relative size of the object being labeled within each
category. For example, when labeling the
water features, I used the largest font on the Pacific Ocean, the next largest
for the San Francisco Bay, and so on. I
used this same philosophy when naming all of the general features with the
largest being San Francisco, Marin Peninsula, and so on. I created a visual hierarchy by
separating each category of feature by at least 2 font sizes with the water and
general features.
I used 8-point font
on all parks and topographic names and 10-point font size for the Golden Gate
Bridge. I placed most every label on top
of the respective feature and used halos or shadows with different colors to
represent the various categories. This
helped each font stand out amongst a busy background. I used a white halo for
the general category, a green halo for parks, and a yellow shadow for the
geographic features. I did not use a
halo for the water features or the Golden Gate Bridge. I did use Italic font
for the water features, however. I also used a callout for Lake Merced and the
Golden Gate Bridge.
Friday, October 9, 2020
Scale and Gerrymandering
This week, we reviewed how scale affects our analysis and understanding of vector data and the basic resolution of raster data. With regards to vector data, as map scale moves from large scale to small scale, it has the effect of reducing our ability to be accurate and precise in measuring landscape features. The number of specific polygons, total length, and the area is reduced because it is much harder to accurately depict what is and is not a specific feature. You have to be much more general in your analysis and descriptions. It is also much easier to miss features altogether when viewing on a relatively small scale.
The images below help depict the effect of scale on vector data:
|
DEM
Resolution |
Average
Slope (degrees) |
|
1m |
39.25 |
|
2m |
38.98 |
|
5m |
38.39 |
|
10m |
37.47 |
|
30m |
34.81 |
|
90m |
30.31 |
Thursday, October 1, 2020
Interpolation
This week, we evaluated several methods of interpolation for efficacy in two different example scenarios: elevation and water quality. I will first describe briefly how these interpolation methods work.
According to Esri's help documentation, IDW (Inverse Distances Weighted) operates under the assumption that objects or things close together are more similar than things farther apart. If we are interpolating what might be expected in a void, this method will assume the known data points closest to that void will be more similar that data points farther away. Each known data point has an influence that diminishes with distance.
According to Esri's help documentation on Spline interpretation, this method uses a mathematical function that attempts to create a smooth surface by minimizing overall curvature and passing through all known data points.
For elevation, we evaluated the use of Spline and IDW from known elevation data points. In this instance, Spline outperformed IDW in creating a more realistic display of the terrain. The IDW method created many potholes and areas that did not seem to fit with what a natural landscape might be like.
For water quality analysis, we evaluated the use of non-spatial analysis, Thiessen interpolation, IDW and Spline (regularized and tension). In this analysis, IDW was the most effective in presenting the data accurately and in a spatial distribution that reflects an intuitive sense of reality. This is represented in the table below:
|
Technique |
Minimum |
Maximum |
Average |
Standard Deviation |
|
|
Non-Spatial |
|
0.8 |
3.5 |
1.81 |
0.57 |
|
Thiessen |
|
0.8 |
3.5 |
1.79 |
0.56 |
|
IDW |
|
0.81 |
3.5 |
1.78 |
0.29 |
|
Spline |
|
|
|
|
|
|
|
Regularized |
-1.7 |
3.64 |
1.67 |
0.65 |
|
|
Tension |
-9.79 |
9.64 |
1.81 |
0.76 |
Below is a representation of the most accurate method used in water quality analysis, the IDW interpolation:
Tuesday, September 22, 2020
TINs and DEMs
This week, we explored Triangulated Irregular Networks (TINs) and Digital Elevation Models (DEMs). The TIN is unique in that it allows you to evaluate slope, aspect and elevation in a way that is useful for certain types of landscape analysis and quick retrieval of information regarding these types of information. An example of this is shown in the image below:
Below, I used a DEM and weighted overlay to give a visual analysis of ski slope suitability. The DEM makes the appearance of elevation data appear more smooth and it better for general map making as it is pleasing on the eye.
Tuesday, September 15, 2020
Road Completeness
This week, I completed an accuracy assessment of two road networks based on their relative completeness using 1km x1km grid for comparison. The goal of this assessment was to determine which road network is more complete. TIGER Roads or Street Centerlines, and to determine which locations are similarly accurate and which locations are more accurate with either of the two networks. The method ology I used to achieve this is outlined below.
I first used the “Clip” tool to remove portions of each road
network that were outside of the supplied grid network. Once the roads outside of the grid area were
clipped, I used the “Summarize Within” tool to calculate the lengths of the road
system inside each grid polygon. I
specified the output in kilometers so as to eliminate the need to do a separate
calculation to convert the results from feet.
Once I had the total feet for each grid and road dataset, I used the “Table to Excel” tool to export this information to Microsoft Excel and calculate the necessary statistics in order to produce the table and maps below. Once the statistics were calculated, I used the “Excel to Table” tool to import the final Excel table back into ArcGIS. Once in ArcGIS, I used the “Join Field” tool join the Percent Difference field I created in Excel to the Grid layer. I then used this field and the Grid layer to generate the map.
Street Centerlines total length in kilometers: 10,873.3
The TIGER Roads network is more complete based on this
analysis.
|
Total
Grid Cells |
297 |
|
Cells
Where Street_Centerlines is more complete than TIGER_Roads |
134 |
|
Cells
Where TIGER_Roads is more complete than Street_Centerlines |
162 |
Tuesday, September 8, 2020
Horizontal Accuracy
This week, I tested the horizontal accuracy of two street datasets in Albuquerque, NM. I tested the City of Albuquerque dataset and the StreetMap USA dataset. To complete this analysis, I overlaid the two street datasets on orthophotos of Albuquerque. I used the orthophotos to identify the true location of 20 intersections. After establishing these reference points, I identified the location of those intersections within the Albuquerque streets dataset and the StreetMap dataset, added XY data for all points, and used the NSSDA datasheet to compute the accuracy of each dataset. Please see the map below for the location of intersections used in the analysis.
ABQ Streets
Positional Accuracy: Tested 13.15 feet horizontal accuracy
at 95% confidence interval.
StreetMap Streets
Positional Accuracy: Tested 353.50 feet horizontal accuracy
at 95% confidence interval.
The relative accuracy of these two datasets is not even close, and it is clear which dataset would best be used for navigating the streets of Albuquerque.





