Mountain biking is a popular sport in Switzerland (Fischer et al., 2021), that raises both environmental and policy issues (Pröbstl-Haider et al., 2018). In order to learn more about this recreational activity, this project takes a closer look at the movement of mountain biking. The analysis of movement data has gained increasing attention from both the GIScience community and the wider public, primarily because such data is easily accessible and appears to have a simplicity in structure (Laube, 2014). Addressing this sport from a movement and spatial analysis perspective, I hope to provide some insights about this movement pattern.
Mountain biking can be practiced on different surfaces (on or off-road), but riders show a preference for natural areas (Zajc & Berzelak, 2016). There are many different types of mountain biking practices (Zajc & Berzelak, 2016), and in this project I focus on downhill mountain biking. The goal is to find the movement pattern of mountain biking in trajectories where also other movement types occurred. In order to detect the mountain biking pattern, I define three criteria which characterize downhill mountain biking.
The criteria are:
the speed of the riding person
the type of ground cover on which mountain biking is performed
the steepness of the trajectory, which needs to be directed downhill
The speed of a person riding a mountain bike is hard to define and may vary from 59-88 kmh (Jeremy, n.d.) to 27-32 kmh (How Fast Do Professional Mountain Bikers Rip Down Hills?, 2022). Other (slower) speed ranges may apply depending on personal condition and preference. Since natural areas are preferred for biking, (Zajc & Berzelak, 2016) the ground cover type needs to be vegetated or otherwise natural. Using just one or two of the criteria will still allow for other activities. For instance, a trajectory leading through grasslands and across forests could still be regarded as hiking, the same applies to the downhill movement. As the speed of a person riding a mountain bike is subject to many factors, it is also not a unique identifier for this movement pattern. Therefore, a combination of the criteria is needed to describe and detect the biking pattern. Using GPS data that Lisa Wahlen recorded on three mountainbiking tours, I will address the research questions below.
In this project I will work on the following three research questions:
How can speed, ground cover and downward motion be used to characterize the movement pattern of downhill mountain biking?
Can I detect segments where mountain biking occurred based on speed, groundcover and downward motion?
Are the chosen criteria applicable to other movement trajectories?
For the project, I used the movement trajectories that were created by Lisa Wahlen when going mountain biking. The trajectories were recorded by using the GPS-tracking App posmo (Genossenschaft Posmo Schweiz, 2022) with a sampling rate of 10 seconds. I include 3 mountain biking tours Lisa completed in the period from the 6th of May to the 18th of May 2023. The tours were tracked in Switzerland in the areas of Wiriehorn (2 tours) and Valbirse (1 tour).
For the assessment of the criteria that describe the movement pattern of mountain biking, we used the MOPUBE vector dataset providing the land cover types of the canton of Bern, using the version last updated on the 23.05.2023 (Amt für Geoinformation des Kantons Bern, 2023). In addidtion, we worked with parts of the swiss digital terrain model swissALTI3D (Bundesamt für Landestopografie swisstopo, 2022). This elevation data is provided as a raster in a resolution of 0.5 m in grids of 1 km^2. I worked with extracts of the datasets, covering the spatial extent of the trajectories within the Canton of Bern.
I chose the tour Lisa made on the 18th of May in the Wiriehorn area (Wiriehorn 05-18) to define the characteristics of the biking movement pattern and tried to apply the criteria to the tour at Wiriehorn on the 7th of May (Wiriehorn 05-07) and the tour in Valbirse on the 6th of May for verification. The trajectories included the car ride from Solothurn to the biking location and back. A first visualisation of transport modes of the data revealed that the mountain biking part of the trajectories were labelled by the posmo app as “Car”, “Bus”, “Other” - and sometimes almost correctly with “Bike”.
Wiriehorn trajectory of the 18th of May
Navigating to the south of the trajectory you’ll find the mountain
biking part.
Wiriehorn trajectory of the 7th of May
Navigating to the south of the trajectory you’ll find the mountain
biking part.
Valbirse trajectory of the 6th of May
Navigating to the northeast of the trajectory you’ll find the
mountain biking part.
Three relevant criteria for mountain biking are speed, downhill movement and ground cover. For all three criteria I assessed the values and ranges fitting the mountain biking pattern of the Wiriehorn 05-18 tour. Then I applied the criteria to the Wiriehorn 05-06 and the Valbirse tour.
For every fix on the trajectory I calculated the average speed within the window of four neighboring points, similar to the moving window method of Laube & Purves (2011). The euclidean distance to the two points before and the two points after the fix was calculated and divided by the time difference between the fix and the two points before and after, respectively. Fixes where the speed calculation could not be completed because either the distance or the time between two points was 0, were regarded as static. On the Wiriehorn 05-18 tour, 80 points were labelled as static, and used for segmentation of the trajectory. They were located in places on the trajectory where little movement or a change in transport mode is plausible (e.g. at the bottom and the top of the cable car allmiried, somewhere in the middle of the downhill trail, at train stations in Solothurn). The segments were used to identify parts of the trajectory where Lisa was mountain biking. The relevant segments were selected based on visual assessment of the movement parameter profile (Dodge et al. 2009) of the average speed (Figure below). I assumed that Lisa went biking between 8:30 and 13:30, and that very short segments and segments with high velocities do not represent biking.
However, the selected segments included the movement of the cable car Lisa took to get uphill to the trail start. To isolate the cable car and determine the relevant speed range for mounainbiking, the average speed distribution of the selected segments was calculated. The speed values that best characterized the movement of mountain biking were identified through a process of testing.
The MOPUBE dataset showed 22 ground cover types (see figure below). Knowing about the preference for natural contexts for mountain biking (Zajc & Berzelak, 2016) I assume that Lisa rode on vegetated and/or natural groundcovers. Thus, every groundcover type seems suitable except for “Abbau, Deponie”, Bahn”, “Gebäude”, “Strasse, Weg”, “Trottoir”, “übrige befestigte” and “Verkehrsinsel”. We could argue that water bodies are not suitable as well, but depending on their size it is not impossible to cross such features when biking.