Introduction
Sampling is a key concept in geography. Since it is impossible to attain an infinite amount of data with the constraints of limited time, money, and human power, it becomes critical to obtain a representative and statistically valid sample that can be reasonably used to draw conclusions about the whole. The strategy in choosing a sampling method that will give reliable data is foundational to any field-based project. Geographers cannot record infinite elevation points, for example, nor could a computer process that data, so instead careful consideration must be given to a strategy to simplify the collection of spatial data.According to online resources from the Royal Geographic Society (visit the link here), there are three main categories of sampling strategy:
·
Random - sample points chosen at random
·
Systematic - sample points chosen based on a spacing system
·
Stratified - Used when population contains subgroups, samples chosen from designated stratification
As with any simplification, these sampling methods are not perfect. There are tradeoffs to each regarding simplicity of data analysis and collection vs. data accuracy—cost vs. accuracy.
Lab objectives
The artist at work; Amanda constructing the sandbox landscape. |
class to develop the ability to create a Digital Elevation Surface using critical thinking skills and improvised survey techniques. This is a two-part field exercise, but the objectives reflected on in this post were:
1) To understand the pros and cons of the
different sampling strategies in order to make an informed decision about which
technique works best for mapping the sandbox terrain
2) Create a unique terrain containing a
ridge, hill, depression, valley, and plain in the sandbox provided.
3) Conduct a survey that provides accurate X,
Y, and Z coordinates and compile them in a normalized spreadsheet that can be
downloaded to ArcMap 10.4.1
Methods
Students were assigned groups of three. Group 2 was comprised of Jesse, Amanda, and Zach (who was absent for a field trip). Groups were encouraged to read up on sampling methods and develop a strategy. We chose to use a stratified systematic sampling technique. The advantages of this technique is its flexibility; we could choose to collect more data points in area of higher relief without having to increase our overall point density in areas of low relief. We also could extrapolate the data via comparisons and correlations of sub-sets.Figure 1 The red X shows the location of the sandbox site. |
Materials
·
Samsung
Galaxy S6 Edge
· measuring
tape
·
meter
stick
· push-pins
· push-pins
·
Colored
string
· 1 meter x 1 meter sandbox
For the survey, a push-pin was inserted every 5 cm around the rim of the sandbox. Then the
colored string was used to denote the lines of the grid (though this method was soon abandoned as
we decided to draw a grid onto the landscape using the meter stick). Sea level (our arbitrary
“zero” elevation) was the plane formed by the top of the sandbox’s walls. An elevation
measurement was taken in the center of each grid square and recorded as X, Y, and Z coordinates.
Areas of high elevation changes were marked with a push-pin and then measured and recorded
(Fig.3). This allowed for higher detail to be recorded where more feature definition will be
needed. Our coordinates were then transferred to a spreadsheet containing X, Y, and Z fields
(Fig.4). This spreadsheet will be imported into ArcGIS in the next field exercise.
· 1 meter x 1 meter sandbox
For the survey, a push-pin was inserted every 5 cm around the rim of the sandbox. Then the
colored string was used to denote the lines of the grid (though this method was soon abandoned as
we decided to draw a grid onto the landscape using the meter stick). Sea level (our arbitrary
“zero” elevation) was the plane formed by the top of the sandbox’s walls. An elevation
measurement was taken in the center of each grid square and recorded as X, Y, and Z coordinates.
Areas of high elevation changes were marked with a push-pin and then measured and recorded
(Fig.3). This allowed for higher detail to be recorded where more feature definition will be
needed. Our coordinates were then transferred to a spreadsheet containing X, Y, and Z fields
(Fig.4). This spreadsheet will be imported into ArcGIS in the next field exercise.
Figure 4 The normalized spreadsheet that will be used to create the Digital Elevation Surface. |
Results and Discussion
Upon conclusion of the terrain sampling, 179 data points had been collected, all with X, Y, and Z values.
Minimum elevation value: -16.00cm
Maximum elevation value: 12.00cm
Mean: -4.71 cm
Standard deviation: 4.64 cm
Conclusion
The inherent disadvantages of a stratified systematic sampling technique is that the proportions of the sub-sets must be known and accurate in order to maintain data integrity. Our system fell short on that; there were too many approximations in the measurements.
This activity demonstrates the
importance of sampling techniques for collecting spatial data; even in a 1x1
meter sandbox it would have been labor-intensive to attain accuracy down to the
centimeter level. Studying real-world geographic features requires an accurate,
scalable sampling system in order to collect data in reasonable amount of time.
It will be interesting to use the
numbers gathered during this sandbox exercise to create a DES. The uncertainty
in the data may cause some discrepancy between the model and our actual sandbox
terrain. 179 data points may prove to be less than ideal, perhaps something
like 500 points (1x1 cm grid) would have been better.
One last look at the llama keychain, the focal point of our sandbox terrain. |
Sources
Royal Geographical Society. Retrieved October 5th, 2016 from http://www.rgs.org/OurWork/Schools/Fieldwork+and+local+learning/Fieldwork+techniques/Sampling+techniques.html
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