1. Introduction
Landslides represent one of the most pervasive natural hazards in mountainous environments and occur when gravitational forces exceed the resisting strength of soil, regolith, or bedrock. Their initiation reflects the interplay of geological structure, hydrological conditions, geomorphology, and external triggers. Common drivers include rainfall [
1,
2], snowmelt [
3], earthquakes [
4], volcanic activity [
5], forest fires [
6,
7], permafrost degradation [
8], and anthropogenic disturbances such as road construction [
9]. Although the physical basis of slope failure is well understood, forecasting the precise timing and location of failure remains challenging.
Monitoring unstable slopes typically relies on a combination of in situ instrumentation, periodic GNSS surveys, and passive remote sensing [
10,
11]. Interferometric Synthetic Aperture Radar (InSAR) has transformed detection of millimeter-scale deformation over large areas [
12,
13,
14,
15], while terrestrial and airborne LiDAR yield high-resolution characterizations of landslide morphology, displacement fields, and volumetric change [
16,
17]. Despite these advances, conventional monitoring approaches can be limited by revisit interval, cloud cover, cost, and the advanced analytical expertise required for interpretation. Furthermore, hazardous terrain and weather often restrict access for field personnel, complicating consistent data acquisition.
Remotely piloted aircraft systems (RPAS) have become essential tools in landslide research because they permit rapid deployment and provide centimeter-level spatial resolution. RPAS photogrammetry and LiDAR have been used extensively to map slope failures [
18,
19], detect precursory cracking [
20], quantify solifluction [
21], and support rapid emergency assessment [
22]. However, such conventional RPAS operations have relied on in situ acquisitions: pilots and observers typically must travel to or near the hazardous site, often under restrictive conditions (weather windows, access constraints, flight regulations). This limits the ability to obtain frequent or event-triggered observations, which are critical for understanding slope dynamics and precursory signals. In addition, deploying a team to conduct in situ data acquisitions often incurs substantial logistical and financial costs, especially when sites are remote, mountainous, or require complex travel arrangements.
Drone-in-a-box (DIAB) systems, also referred to as Robot-as-a-Service (RaaS) platforms, offer a potential solution to these challenges by enabling fully or semi-autonomous launch, recovery, charging, and data off-loading from compact, self-contained ground stations. Their technical foundations lie in advances in precision landing, automated battery replenishment or replacement, and environmental hardening, allowing systems to remain on site for months at a time. The RPAS component of DIAB systems offers a complementary advantage because their non-invasive, low-impact operation allows repeated monitoring where traditional field access is difficult or undesirable. A synthesis of decade of docking-station research, highlighted positioning systems, wireless charging, autonomous battery exchange, and protective storage modules as core components of modern DIAB infrastructure [
23]. Recent technological progress has accelerated commercial adoption, with operational systems such as Optimus (American Robotics, Sparks MD, USA) [
24], Drone Network (Avy, Amsterdam, Netherlands) [
25], HubX (Sphere Drones, Sydney, Australia) [
26], Energy Robotics BVLOS DIAB (Energy Robotics, Darmstadt, Germany) [
27], X10 (Skydio, San Mateo, CA, USA) [
28], and the Dock series (DJI, Shenzhen, China) [
29,
30,
31]. Such DIAB systems have been deployed primarily in industrial and public-safety contexts, including automated overhead transmission-line inspections, thermal-hotspot and gas detection at solar farms and refineries, open pit mine monitoring [
32,
33], and radiological monitoring where human exposure must be minimized [
34]. Innovations such as solar-powered charging stations further extend use in remote or infrastructure-poor regions [
26,
35].
Despite this commercial momentum, DIAB implementation remains underrepresented in the peer-reviewed academic literature. Most research focuses on individual technical components such as precision-landing algorithms (e.g., visual marker–based guidance, infrared beacon trackers [
36,
37,
38]), robust controller design [
39], or power-management strategies including wireless charging and automated battery swapping [
35,
40,
41]. Studies that evaluate complete DIAB systems under real operational conditions, particularly in environmental monitoring, natural hazards, long-term deformation tracking, or remote scientific deployments, are noticeably scarce.
Therefore, the objective of this study is to present a technology demonstration of the DJI Dock 2 drone-in-a-box system [
42] for remote, low-maintenance monitoring of an active landslide in complex mountainous terrain. This demonstration represents one of the first academic evaluations of DIAB technology for natural-hazard monitoring and highlights opportunities and limitations for its future scientific and operational use.
2. Materials and Methods
2.1. Study site
The study site for this technology demonstration is the Miles Ridge landslide near kilometer 1818 on the Alaska Highway, 50 km south of the town of Beaver Creek in the Yukon Territory, Canada (
Figure 1). The area is geologically active due to a combination of factors including lithology, slope steepness, high regional seismicity [
43], proximity to the Denali Fault, and degradation of permafrost under warming conditions. The ~400 m wide landslide head scarp is situated along the crest of Miles Ridge, which lies at the foot of the rugged St. Elias Mountains. The top of the ridge is at an elevation of ~1480 m ASL, rising ~780 m above the White River valley and Shakwak Trench below. The landslide extends a horizontal distance of ~580 m in length and a vertical distance of ~370 m and lies on a northeast-facing slope that averages 34° in steepness [
44]. For our study, the straight-line distance between the head scarp (furthest point of interest) and the installation of the Dock 2 was 2.55 km (1.37 NM) (
Figure 1). The landslide and surrounding area to be monitored was 15 ha. The landslide is located within a package of volcanic and highly altered ultramafic rocks which are bounded between a set of faults considered to be within the Denali Fault system [
44]. The Denali Fault itself is a major right-lateral strike slip fault that runs in a northwest-southeast direction along the base of Miles Ridge, approximately 1.5 km to the northeast of the landslide.
No evidence of landslide activity on Miles Ridge was found in 1988 aerial photographs [
44]. The White River First Nation first observed slope movement at the site in the early 1990s and reported further changes following the November 3, 2002, M7.9 Denali Fault earthquake, which was one of the largest inland earthquakes in North America [
45,
46]. The region remains highly seismically active; for example, [
43] reported more than 40,000 earthquakes between 2010 and 2023.
A set of rebar monuments and wooden stakes were installed on site in 2007 to monitor ground deformation through subsequent ground-based differential GPS surveys [
44]. The site was resurveyed once in 2010 but was not revisited since then due to the high cost of helicopter access and because of site safety concerns including the presence of slumping and fresh tension cracks above the head scarp [
47], rockfall periodically observed 2.5 km away from Yukon Discovery Lodgings, and small debris flows on the lower portion of the landslide [
44]. These combined factors make this an ideal site for RPAS-based surveying.
2.2. DJI Dock 2 and Matrice 3TD
The DJI Dock 2 is a fully integrated DIAB system designed for automated operations. It is primarily composed of two hardware components: the Dock itself, which provides weather-resistant housing, automated charging, and environmental monitoring, and the Matrice 3D/3TD aircraft, a compact quadrotor drone developed specifically for the Dock 2. Together, these components enable remote, and repeatable data collection missions through cloud-based or local scheduling and monitoring.
2.2.1. Dock 2
The Dock weighs approximately 34 kg and is rated IP55 for dust and water ingress protection. It can operate within a temperature range of −25 °C to 45 °C [
42]. As described in [
48] installation requires continuous AC power (see
Section 2.3.2) and a stable Ethernet-based network connection (see
Section 2.3.3). An internal lead-acid backup battery provides sufficient power for the aircraft to return and land in the event of a power outage. The Dock also includes an integrated weather station that continuously monitors internal and external air temperature, humidity, precipitation, and wind speed. Both the rainfall and wind-speed gauges are self-heating. Thermal regulation inside the Dock is achieved via a solid-state thermoelectric cooler (TEC) that provides both heating and cooling to maintain the aircraft and its battery within a safe operating temperature range. Heating strips along the Dock’s cover seam prevent freezing during cold weather. Dual internal and external cameras enable visual monitoring of aircraft take-offs and landings.
When the aircraft lands, the V-shape of the landing platform allows it to slide into the correct position for closure of the Dock doors. A wireless charging module under the landing platform charges the aircraft battery from 20-90% in ~32 min. To facilitate landing, the Dock employs an image-based recognition system supplemented with Real-Time Kinematic (RTK) positioning, which also functions as an RTK base station for flight operations. The positional accuracy of the RTK base station is specified as 1 cm + 1 ppm (RMS) horizontally and 2 cm + 1 ppm (RMS) vertically [
42]. Given that the crest of Miles Ridge was located 2.55 km from the Dock installation, the distance-dependent term contributes up to an additional 2.5 mm to the total, resulting in expected base station positional accuracies of approximately 1.26 cm horizontally and 2.26 cm vertically (1σ) at the furthest point.
The aircraft used with the Dock 2 was a DJI Mavic 3TD (
Table 1), hereafter referred to as M3TD. As described in [
42] it is equipped with both vision and infrared sensing systems for six direction obstacle avoidance. It also incorporates DJI AirSense, which alerts the remote pilot to nearby crewed aircraft broadcasting Automatic Dependent Surveillance–Broadcast (ADS-B) signals within approximately 10 km of the M3TD (REF). The onboard GNSS + RTK modules support GPS, GLONASS, BeiDou, and Galileo global navigation satellite constellations. Communication between the aircraft and the Dock 2 is through the DJI OcuSync 3 Enterprise digital transmission system. The integrated M3TD payload has three imaging sensors [
42]:
A wide-angle RGB camera with a 1/1.32-inch CMOS sensor (48 MP effective; 8064 × 6048 pixels) with an f/1.7 lens and 84° field of view (FOV);
A telephoto RGB camera incorporating a 1/2-inch CMOS sensor (12 MP effective; 4000 × 3000 pixels) with an f/4.4 lens and 15° FOV supporting 8x mechanical (56x hybrid zoom); and
A radiometrically calibrated thermal infrared camera based on an uncooled vanadium-oxide (VOₓ) microbolometer with 12 µm pixel pitch, 61° FOV, and thermal sensitivity ≤ 50 mK @ f/1.0.
Although the telephoto camera (162 mm format equivalent) offers considerable imaging potential, its photographs are not RTK-precision geotagged and are therefore unsuitable for high-accuracy mapping applications. Consequently, only the wide-angle camera was used for mapping.
Table 1.
Main characteristics of the DJI Mavic 3DT [
42].
Table 1.
Main characteristics of the DJI Mavic 3DT [
42].
| Characteristic |
Value |
| Takeoff weight (kg) |
1.41 |
| Maximum flight speed (m/s) in normal mode |
15 (forward), 12 (backward), 10 (sideways) |
| Service ceiling (ft ASL) | (m ASL) |
13,123 | 4,000 |
| Maximum ascent speed (ft/min) | (m/s) |
1,181 | 6 |
| Dimensions without propellers (mm) |
335 (L) × 398 (W) × 153 (H) |
| Operating temperature (°C) |
-20 - 45 |
| Maximum wind resistance (in flight) (m/s) |
12 |
| Maximum wind resistance (takeoff/landing) (m/s) |
8 |
| Maximum flight time/hover time (min) |
50/40 |
| Maximum operating radius (km) |
10 |
| Ingress protection |
IP54 |
2.3. Installation
The installation was designed to remain fully functional and secure under variable weather conditions, prevent access by wildlife or unauthorized individuals, meet signal-quality requirements, and retain the flexibility to be relocated between sites. Prior to installation, a DJI Mavic 3 Enterprise drone was used to perform the built-in Dock Site Evaluation routine within the Pilot 2 flight control application. This routine uses the aircraft’s onboard camera to verify that no obvious signal obstructions exist within a 20° field of view from the proposed installation location. If an obstacle is detected, it must satisfy the distance (d) constraint (Eqn 1) [
48]:
where h is the height of the obstacle.
During the site evaluation, the aircraft also conducts a GNSS signal quality survey. To satisfy the above-mentioned criteria, the Dock 2 was installed on top of a standard 40 ft (L) × 8 ft (W) × 8.5 ft (H) shipping container (
Figure 2). The elevated position eliminated the need for a safety fence.
2.3.1. Physical installation
To provide a stable and transportable platform for the Dock 2 installation, a custom wooden base was constructed to fit the top of the shipping container. The base was built from two pieces of 2×6 lumber (5×15 cm), the standard dimensional size commonly used in Canada and the USA. Their standard length of 240 cm (8 ft) matched the width of the container (
Figure 2:A). The two beams were joined by four 80 cm crosspieces (
Figure 2:B) of the same material to form a baseplate onto which the Dock 2 and its peripherals were mounted. The ends of the lumber were secured to the container using Everbilt steel strap hooks (
Figure 2:C) that clamp onto the container’s edges, preventing wind-induced movement of the installation. The Dock 2 (
Figure 2:D) was fastened to the wooden baseplate with twelve 5 cm deck screws. A self-tapping screw was used to attach the Dock 2 ground wire (
Figure 2:E) to the top of the separately grounded container. The container had been independently grounded; however, if it had not been, a dedicated ground wire and grounding rod would have been required [
48].
2.3.2. Power
The Dock 2 requires external AC power (maximum power draw of 1000 W) connected to a dedicated 2-pole 16 A circuit breaker and protected by a 40 kA surge suppression device [
48]. Although the installation manual recommends 15 AWG copper-core cable for runs under 100 m, a 10/3 Romex (10 AWG) cable was used instead to reduce voltage drops. The 10 AWG line was connected to a dedicated 2-pole 30 A circuit breaker in a nearby electrical panel, supplying power to a waterproof outdoor receptacle mounted on top of the container (
Figure 2:G). From this receptacle, 15 AWG wire was routed to the Dock 2 via its standard power connector. The receptacle also supplied power to a Starlink satellite internet system and a security camera (see below) via 12-gauge, heavy-duty 15 A outdoor extension cords. Because the power plugs for the modem and camera were not waterproof, their connections to the extension cords were enclosed within waterproof electrical boxes mounted to the baseplate (
Figure 3).
2.3.3. Network
The Dock 2 requires a low-latency Ethernet connection using IPv4 protocols and a minimum Cat 6-rated cable for proper operation[
48]. The built-in 4G wireless backup was not utilized, as the landslide site lies outside any cellular data coverage area. Instead, the system was connected to a Starlink-powered satellite internet network, providing a stable high-bandwidth link for remote monitoring and control (
Figure 2:I). A Sancable RJ45 surge protector, housed in a waterproof electrical box, was installed in-line between the Dock 2 and the Starlink modem to safeguard against lightning-induced power fluctuations (
Figure 3C). The Starlink modem and power supply were enclosed within a Pelican 1550 case secured to the baseplate with three screws (see
Section 2.3.1,
Figure 2:H). A 5 cm side opening allowed the Cat 8 Ethernet and power cables to pass through, and the case top was covered in white plastic to reduce the chance of the modem or power supply overheating. The Starlink Performance Gen-2 terminal was attached to a standard pallet placed nearby on the roof of the container to maximize sky visibility (
Figure 2:I). A second Ethernet connection from the Starlink modem linked to an HXVIEW 4K PTZ (Pan-Tilt-Zoom) outdoor security camera with 30× optical zoom, oriented toward Miles Ridge (
Figure 2:L). Given that the pilot-in-command was at times located ~ 4,000 km from the Dock system, real-time situational awareness of meteorological conditions on Miles Ridge and potential local air traffic (e.g., helicopters), as well as reliable communication with visual observers, was critical. Accordingly, a video camera with integrated audio was installed. The camera provided real-time monitoring of weather and airspace conditions and enabled two-way audio and video communication with a visual observer.
Provided that the power supply is already established (e.g., circuit breaker installed), the hardware installation can be finished in less than a day, using a forklift to lift the Dock 2 onto the container roof.
2.3.4. Position calibration and alternative landing site
During installation, the absolute position of the Dock 2 was established through manual calibration [
48]. Because the deployment site is outside of network RTK coverage, absolute positioning was determined using an Emlid RS2 GNSS receiver (Emlid Tech KFT, Budapest, Hungary). The Dock cover was opened and the RS2 was mounted on a tripod centered above the RTK positioning marker on the internal platform above the electrical cabinet. A plumb bob suspended from the tripod ensured precise collinearity between the antenna phase center and the marker. GNSS observations were recorded over a 12.5-hour session and post-processed using Natural Resources Canada’s Precise Point Positioning (PPP) service [
49]. The derived coordinates with total uncertainties of 2.3 cm (X), 3.3 cm (Y), and 2.8 cm (Z), were then used to manually calibrate the Dock’s absolute position (accounting for the vertical offset between the RS2 and marker). An alternate emergency landing site, required when the aircraft cannot land in the Dock, was designated within the grass field beside the shipping container.
2.4. Flight Planning
2.4.1. FlightHub 2
Flight planning, deployment with remote pilot oversight and preliminary analysis were all conducted via the FlightHub 2 cloud computing platform [
50]. FlightHub 2’s information security management system is certified to the ISO/IEC 27001 standard which ensures preservation of confidentiality, information integrity, and data availability.
2.4.2. Flight plan development
To remain compliant with the Canadian Aviation Regulations, Part IX 901.25(1)(a), the flights needed to remain below 400 ft (122 m) AGL. Flights above this altitude require a Special Flight Operations Certificate, in this situation under Standard Scenario 3 (STSC-003) [
51]. The area around Miles Ridge is in Class G (uncontrolled) airspace. The nearest registered aerodromes are Beaver Creek (CYXQ) 48.9 km to the north, Burwash (CYDB) 106.7 km to the south and Horsfeld Alaska (4Z5) 32.4 km to the west. The property where the Dock was installed has a private airstrip, which is an unregistered aerodrome (i.e., not registered with Transport Canada) that does not appear in the Canada Flight Supplement. During the Dock installation, the airstrip was in use by two helicopters, transporting equipment and staff for mineral exploration
One of the initial flight planning challenges involved the nearly 800 m elevation difference between the installation site and the target landslide area (
Figure 4). The terrain model used in FlightHub 2 is based on the platform’s built-in global elevation dataset (provider and specifications not publicly disclosed). Comparisons with multiple independent digital elevation models revealed elevation discrepancies of up to 15 m and this area is not covered by territorial airborne LiDAR data. Consequently, to accurately determine the elevation of the forest canopy on a small ridge between the installation site and the base of Miles Ridge, a photogrammetric survey was conducted using the M3TD.
The built-in mapping mission templates, such as the Slope Mapping mode, automatically optimize flight-line spacing and camera-triggering intervals; however, they do not permit customized transit altitudes between the Dock and the survey area. If such a mission type had been used, the M3TD would have ascended to the take-off altitude and traveled directly toward the mapping area at that height. Given that the highest portion of the mission is located at approximately 1300 m height above ellipsoid (HAE), the aircraft would have transited toward the landslide area at roughly 650 m above ground level (AGL). Upon completing the mapping at the base of the slope (~1000 m HAE), the return-to-home path would have been at approximately 300 m AGL; both scenarios exceeded the maximum permitted flight altitude. Likewise, a waypoint mission defined at a custom altitude cannot be combined with a mapping mission, as is possible in third-party flight planning software such as UgCS (SPH Engineering, Riga, Latvia). However, within UgCS, other critical flight planning parameters such as aircraft yaw (discussed below) are not preserved upon export to FlightHub 2, thereby negating interoperability between the two platforms for this application.
To overcome these limitations, the entire mission was planned as a waypoint mission, with flight-line spacing and waypoint coordinates first determined in ArcGIS Pro (v 3.5). The mission layout was then manually recreated in FlightHub 2 and refined by adjusting the position and altitude of each waypoint and specifying custom waypoint actions. This approach ensured that the aircraft maintained an altitude less than 122 m AGL throughout the mission. The entire mission was flown at a programmed ground speed of 10 m/s, corresponding to the maximum sideways flight speed of the M3TD (
Table 1). During the survey, the aircraft ascended to the highest elevation (~1337 m HAE; waypoint 6) and traversed the landslide surface laterally in a cross-slope pattern, flying sideways and backward downslope while maintaining the camera’s orientation toward the slope (
Figure 5). The wide-angle camera was configured to trigger once per second between waypoints 5–19, and the gimbal pitch angle was varied between flight lines to ensure full coverage of the landslide surface. During transit from take-off to waypoint 6, and again between waypoints 20–25, the aircraft flew forward to and from the survey area. Under ideal wind conditions, the flight duration was estimated at 10 min with a total travel distance of 5,789 m and 290 photographs to be acquired (
Figure 5). Upon returning to the home point, once inside the Dock 2, the M3TD automatically transfers the photographs to the Dock’s internal hard drive which then uploads them directly to FlightHub 2. Given that this was a technology-demonstration project with limited prior knowledge of wind and turbulence conditions at altitude, flight lines were intentionally kept well back from the ridge. With repeated flights and improved understanding of the site’s atmospheric behaviour, future missions could be planned to position the aircraft closer to the ridge crest.
2.5. Model evaluation
The data acquisition window extended from mid-July to early September 2025. After each flight, 3D mesh models (B3DM – Batched 3D Model format) were generated in FlightHub 2 for immediate quality control online. Although FlightHub 2 includes built-in online visualization and limited analytical tools, the outputs from the analytical tools (e.g., cross sections) cannot be downloaded. Consequently, to evaluate temporal consistency, models were processed locally with DJI Terra v.5.0.2 (DJI, Shenzhen, China), producing both a solid mesh in .i3s (Indexed 3D Scene Layer) format which is compatible with GIS software and a point cloud in .las format. The .i3s files from three acquisition dates were converted to .las in ArcGIS Pro v.3.5.3 (ESRI, Redlands, CA) since the i3s format stores geometry in a tiled, compressed, multiresolution structure optimized for visualization without direct access to elevation values (as a raster would). Finally, temporal consistency was assessed by comparing cross-sections of the landslide surface using the resulting low-density ArcGIS Pro generated .las files in QT Modeler v.8.4.3.1.1 (Applied Imagery, Chevy Chase, MD). The ArcGIS Pro generated .las files were used for the cross-sections instead of the originals because in Terra, construction of the mesh model includes extensive point cloud cleaning (e.g., outlier removal), triangulation, smoothing, and decimation before the original RGB photographs are reprojected onto the surface to create the mesh product; the original .las files do not have this preprocessing applied.
3. Results
A total of five full model acquisitions were carried out according to the final flight plan between July 13 and September 7, 2025 (
Table 2). Except for the July 13
th acquisition at 19:55 local time, all flights were conducted in the early afternoon near solar noon to maximize slope illumination and minimize wind. The highest altitude reached by the aircraft between waypoints 6 and 7 (
Figure 5) was 1337.9 m HAE. Flight logs indicated that DJI OccuSync transmission strength remained in the Strong (highest) and Very Good (second highest) categories throughout all missions. OccuSync is the digital wireless transmission system responsible for command/control, telemetry, and real-time video downlink. The segment of the flight experiencing the strongest winds varied between acquisitions (
Figure 6). The sustained higher wind speeds observed on July 13 were expected, as the later flight time coincided with stronger winds at higher altitudes in the evening. At this latitude, sunset on July 13
th was at 23:53:04, which ensured sufficient remaining daylight to undertake a mapping mission.
Because the camera was programmed to take photographs every second between waypoints 5 and 19, the total number of images collected during each mission ranged from 297 to 301 (
Table 2), slightly above the estimated 290 (
Figure 5). Similarly, the total flight time exceeded the planned duration by approximately 90 seconds. One exception is the flight on July 14
th, where the pilot paused the mission near waypoint 23 due to an incoming crewed helicopter that landed on the airfield, adding nearly 90 sec to the total flight time. To prevent the aircraft spending excessive time at high altitude while attempting to reach precise waypoint positions under high-wind conditions, as would occur if photographs were triggered at fixed distance intervals, the 1-second time-based triggering mode reduced the number of required waypoints and helped keep the overall flight time to a minimum. For all flights the aircraft battery was > 50% upon landing.
An initial assessment of morphological characteristics such as slope at the head scarp indicate a close agreement with the 34˚ reported by [
44] (
Figure 7). An assessment of elevation transects from the July 13, July 14, and September 7 datasets reveals close correspondence across all, indicating that the models are well co-registered (
Figure 8). The transects show tight clustering of points with no systematic vertical offsets, demonstrating both a temporal stability of the terrain and a high repeatability of the DIAB acquisition workflow. The high similarity of the July 13
th and 14
th profiles illustrate reproducibility despite differences in illumination conditions. No consistent or systematic geomorphic change is detected along any transect, although the first ~50 m of transect A shows a noticeable deviation of ~2 m in the September dataset, which may reflect small-scale surface topographic differences towards the lower third of the landslide such as accumulation of rock fall. Slightly increased scatter in transect B is consistent with rougher surface materials, and the overall sparser point density in transect C is indicative of edge-of-block uncertainty.
4. Discussion
Effective deployment of DIAB systems in mountainous environments requires careful consideration of both environmental conditions and operational constraints. Although the Dock 2 is designed to automate routine RPAS flights, real-world performance is strongly shaped by local wind regimes, terrain complexity, and software capabilities. The installation described here was straightforward to implement, remained functional and secure under variable summer weather conditions, prevented access by wildlife or unauthorized individuals, met signal-quality requirements, and retained the flexibility to be relocated between sites. The resulting five datasets showed high reproducibility and accurate co-registration (
Figure 8), enabling future analyses of terrain features and potential changes.
One of the greatest uncertainties during flight planning was the lack of prior knowledge of wind conditions along the steep elevation gradient.
Figure 6 demonstrates that wind speeds were lowest near the valley floor and increased progressively with altitude toward the ridge, consistent with orographic wind amplification, mountain–plain circulation, and terrain-channeling effects. Mid-slope and uppermost flight lines exhibited the highest variability on three flights and the strongest winds on two dates, confirming that the ridge environment is structurally turbulent. Despite the increased platform motion expected under such conditions, the M3TD maintained stable navigation and adhered to its planned route (
Figure 6). The July 13
th flight displayed especially sharp spatial gradients in wind speed, indicative of more turbulent evening atmospheric conditions. Unexpectedly, several of the higher-altitude flight segments exhibited periods of very low wind speeds across all acquisition dates (
Figure 6). Importantly, these results highlight that valley-level wind measurements are not necessarily representative of conditions at altitude. Despite these environmental constraints, the system demonstrated strong operational resilience and maintained mission continuity across flights.
Steep, complex topography also posed challenges for flight planning, particularly in the absence of recent, high-accuracy elevation data such as airborne LiDAR. Maintaining safe clearances above ground within regulations requires careful manual adjustments to flight paths. Enhancements to FlightHub 2 such as allowing fully customizable waypoint altitudes for transit to and from mapping areas would substantially facilitate route planning in mountainous terrain. Such capabilities would better accommodate abrupt elevation changes, reduce terrain-following uncertainty, and facilitate deployment in similar environments without the need for advanced GIS analytical skills in flight planning. In addition, analyses generated within FlightHub 2, such as volume-change calculations and elevation transects, are currently available only as visual products or embedded reports. Allowing users to export these outputs in standard formats (e.g., GeoTIFF, shapefiles, CSV) would greatly enhance the scientific and operational value by enabling independent validation and integration with geospatial workflows.
Because of the terrain and environmental challenges, the flight plan used in this study remained conservative, limiting the aircraft’s proximity to the head scarp and minimizing time spent at higher altitudes. As a result, the uppermost portions of the models including features such as tension cracks near the ridge head [
47] are less well resolved than features lower on the slope. Greater spatial detail could be achieved in future operations by positioning flight paths closer to the ridge crest, though this would increase exposure to wind shear and stronger terrain-driven winds. Alternatively, the zoom camera could be used to obtain high-resolution single-frame photographs.
During an attempt to collect evening infrared data (at ~24:18), wind conditions that initially appeared acceptable at the Dock location (3-5 m/s | 10.8-18 km/hr) intensified rapidly as the aircraft climbed with sustained wind speed in the 9-11 m/s (32.4 – 39.6 km/hr) range. By approximately 1100 m ASL, sustained winds exceeded 12 m/s (43.2 km/hr) and reached the severe-wind threshold (13.2–13.6 m/s | 47.5 – 49 km/hr), triggering a return-to-home and preventing completion of the mission. Future operations could attempt to further evaluate the utility of the IR camera, if weather conditions at altitude remain suitable for safe operations. Importantly, the failsafe response functioned exactly as designed, ensuring aircraft safety despite rapidly deteriorating conditions.
In most conventional drone operations, pilots rely on handheld controllers whose physical sticks and buttons support well-ingrained muscle memory, including the rapid execution of memory-item actions during emergencies. In contrast, FlightHub 2 currently requires remote pilots to issue critical commands using a keyboard and mouse. Relearning how to fly and react under pressure in this interface can be daunting, and achieving the same level of confidence and instinctive response requires dedicated practice and training.
Operating a DIAB system remotely also introduces a different kind of psychological workload compared to serving as a pilot-in-command on site. Without direct sensory cues such as hearing the aircraft, observing weather shifts, or visually confirming obstacles remote pilots must rely entirely on telemetry, video feeds, automated safeguards and remote information from on-site visual observers. This increases cognitive demand and can amplify stress, particularly in complex environments like mountains or rapidly changing weather conditions. However, as DIAB technologies mature, situational-awareness tools improve, and standardized operational frameworks become more widespread, these challenges may diminish. Over the next decade, remotely managed DIAB missions may become routine, and the psychological gap between on-site and remote operations may narrow as experience, trust in systems, and automation continue to evolve. Just as importantly, as these platforms accumulate a verifiable safety record demonstrating reliability across diverse environments and use cases, operators will gain greater confidence in both the technology and the operational workflows. This growing body of evidence will help shift DIAB operations from being perceived as novel and high-risk to becoming a standardized, trusted component of routine aerial data collection.
For users to adopt complex, infrastructure-dependent systems such as DIAB platforms, they must perceive clear advantages over existing workflows. Adoption requires more than technological capability; end-users must see improvements in efficiency, safety, data quality, or operational reliability. Automated systems that alter established practices also demand new approaches to regulatory compliance, data management, and maintenance. Demonstrating practical benefits such as reduced site visits, improved temporal resolution, and enhanced personnel safety is therefore essential.
Given these considerations, the Dock 2 performed very well during this technology demonstration. More recent DIAB systems, such as the Dock 3 [
31], incorporate built-in battery systems that eliminate the need for hard-wired electrical connections and greatly simplify field installation. This increased mobility enables rapid deployment directly from vehicles and is especially advantageous in remote areas lacking electrical infrastructure. Similarly, Sphere Drones’ HubX platform [
26] provides a trailer-mounted, solar-powered solution compatible with both the original Dock [
29] and the Dock 2 [
42], offering comparable flexibility for off-grid or semi-permanent installations.
Ultimately, the scientific value of this technology demonstration must be assessed using the photogrammetric models from a geological standpoint to determine whether their resolution and temporal consistency are sufficient to capture subtle precursory features such as crack propagation, differential settlement, or changes in surface roughness and moisture that may precede slope failure at Miles Ridge. Determining this capability is essential for evaluating whether DIAB-based monitoring could contribute meaningfully to landslide early warning systems.
5. Conclusions
The deployment of the Dock 2 in this mountainous environment demonstrated that DIAB systems can operate reliably even under variable weather and challenging terrain. Despite strong, spatially variable winds, steep slopes, and a large elevation gradient, the system maintained stable flight paths, produced highly reproducible models, and met the operational demands of a remote mountain site.
Looking ahead, as battery technology advances, DIAB systems will become less dependent on fixed power infrastructure, with autonomous solar charging enabling true stand-alone operation. This will make the systems more portable, easier to deploy from vehicles, and capable of functioning in increasingly remote or off-grid environments. Enhancements such as more flexible flight-planning controls and improved data-export tools will further support operations in complex landscapes. As DIAB systems build a verifiable safety record and pilots gain experience with remote-only interfaces, these platforms have strong potential to become integral components of continuous landslide monitoring and other geohazard applications. With continued advances in situational awareness and detect-and-avoid capabilities satisfying regulatory frameworks, they may also become fully accepted within the broader aviation community.
Author Contributions
Conceptualization, M.K, O.L., J.S. and P.L.; methodology, M.K., O.L. and J.P.A-M.; formal analysis, M.K.; investigation, all authors.; writing—original draft preparation, M.K., O.L., J.P.A-M.; writing—review and editing, all authors.; funding acquisition, J.S., M.K., J.P.A-M, P.L. All authors have read and agreed to the published version of the manuscript.
Funding
This research was funded by a Natural Sciences and Engineering Research Council of Canada’s (NSERC) Alliance Program grant (ALLRP 586350-2), an NSERC Discovery grant (RGPIN-2022-05288) and the Yukon Geological Survey.
Institutional Review Board Statement
Not applicable.
Informed Consent Statement
Not applicable.
Data Availability Statement
The raw data supporting the conclusions of this article will be made available by the authors on request following an embargo from the date of publication to allow for completion of graduate theses.
Acknowledgments
We thank Amanda Harris from the Yukon Discovery Lodgings for providing a location to install our equipment as well as ongoing logistical support throughout the data collection. We further thank Stephen Scheunert and Paul Mondor for access to a test site and logistical support in Quebec prior to deployment in the Yukon, as well as Kyle Miller from DJI Enterprise and Jason Rule from Transport Canada for helpful flight planning insights. We also thank the National Research Council of Canada’s Integrated Aerial Mobility Program (IAM) for support of the NSERC Alliance Partnership.
Conflicts of Interest
Author P.L. was employed by the Yukon Geological Survey. The remaining authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.
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