Introduction
A 2015
study by Pew Research Center found that 68% of U.S. adults owned a smartphone,
45% owned a tablet computer. and smartphone ownership increases to 86% for
those 18-29 years old. The processing power of a smart phone or tablet is much greater
than that of a GPS, therefore it makes sense that these convenient and almost
omnipresent devices would make a good alternative to a standalone GPS device
for the use of GPS data collection. Applications such as Arc Collector even
offer the option to collect data while offline, similar to a GPS. You can
download a map or use a basemap for reference and edits can be updated once a
connection has been reestablished. In this lab, groups will utilize the same
map while online to collect micro-climate data that will be updated on the fly.
Study Area
The study area is an area
about 1.2 square kilometers that covers almost all of UWEC`s main campus. It
was divided into five zones; two zones were sampled by two groups, one zone was
sampled by one group, one zone was sampled by three groups and one zone was not
sampled at all (Figure 1). There was a small amount of zone overlap, but this did
not cause excess data collection in any of these areas. Some geographic
features noteworthy in micro-climate assessment are the large ridge running along
the southern border of zone 3 and along the borders of zones four and five, the
base map contains subtle contour lines that reveal this feature, and the two
flowing bodies of water. Little Niagara Creek runs along the borders of zones
two and three and then just within zone four before dumping into the Chippewa
River. The river constitutes a large area within zone one. There are also zones
with many buildings, as labeled in figure 1, and an area within zone three that
is forested.
Methods
To begin this lab, everyone
with a smartphone had to download the Arc Collector application on their phone,
log into ArcGIS Online using a web browser to join the group containing the map
necessary for data collection, and then log onto the application to open the
map in Arc Collector. The map included polygons dividing the study area into
zones and each group was assigned a zone in which to collect micro-climate
attribute data at numerous locations within the zone. Each group received a
Kestrel handheld ambient weather station (figure 2)
and a compass to collect temperature, dew point, wind speed, and azimuth of
wind direction. The groups consisted of two people; one for data collection and
the other for input of data into Collector. Because everyone was online and
data was being entered into a shared map; as data was entered into Arc
Collector each group could see all points as they were added. The resulting
point data as well as the zone polygons were then imported into ArcMap for
analysis. Various interpolation methods were used to visualize variations
between areas and predictions of data between points. The data was collected at
random with one zone almost completely lacking data points and the river constituting
another area lacking data points. The resulting dataset was not evenly spaced
with points clustered together in some areas and others lacking points (figure 3).
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Figure 3. Map displaying distribution of data points collected |
Figure 2. Kestrel handheld Weather Station used to collect temperature, dew point, and wind speed |
Results
Because the IDW interpolation
method assigns values based on the values of known points nearby, it is an
interpolation method that is not recommended for datasets with an uneven
distribution of sample points such as this one. This is evident in the IDW
interpolation of wind speed; the areas containing a higher density of samples
are over represented with excessive value variation radiating from areas of
high density (figure 4). The anomaly found in
the southeast section of the study area can be explained by wind direction and
the presence of the steep ridge directly south of the points. The wind was
generally blowing at an azimuth between 180 and 270 degrees, leaving the area of data collection
protected from wind by the ridge. Spline is another interpolation method not
recommended for data with over and underrepresented areas. However, it does
create a smooth transition between points and is ideal for gradually changing
values. Temperature within a small study area like this will only contain
gradual changes depending on location and the resulting interpolation contains
change that is relatively subtle (figure 5).
There are a few areas between points that have been given values that are most likely
inaccurate. These could be explained by temperatures taken near heat vents and
temperatures taken in areas with lots of shade and water, making it cooler. The
kriging method of interpolation uses a similar algorithm as IDW to assign
values to unknown points, but it also assumes correlation based on distance and
direction from known points. This addition to the method makes it more ideal
for the interpolation of dew point. The dew point of a space is partially
determined by the moisture in the air, which will vary between points taken along
water, taken near the swampy woods area, and the higher elevation of upper
campus. Distance between these points will help prevent correlations between
these points. The result provides a gradually changing interpolation of dew point
(figure 6) compared to that of the natural
neighbors result which resulted in distinct layers of change radiating from
point clusters (figure 7).
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Figure 4. IDW interpolation of wind speed, with azimuth compass |
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Figure 5. Spline interpolation of temperature |
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Figure 6. Kriging interpolation of dew point |
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Figure 7. Natural neighbor interpolation of dew point |
Conclusion
This lab
offered a look at how the convenience of data collection using Arc Collector can
then be easily used to analyze and manipulate data in ArcMap. The data analysis
tools available in ArcMap make Arc Collector a very useful tool, but it is also
useful for those who do not have access to ArcMap. Arc Collector itself can be
used to create maps and collect data and very accurately track where you’ve been.
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