Spatiotemporally dense hydrological observation networks are required to provide a suitable database for modeling and planning of water resources. One important hydrological observation is the water stage, which can be retrieved using several methods. Floating and pressure gauges are very common (Morgenschweis, 2010); however, they require the installation in the water and therefore entail the risk of losing them during severe flooding. Thus, remote observation techniques, such as those based on radar or ultrasonic devices (Herschy, 2008), might be preferred in such situations because they have the advantage that they can be installed remotely. Another remote option is the application of image-based methods. In general, they can be low-cost in terms of the device compared to conventional water stage retrieval approaches if, for instance, basic camera circuit boards are used in combination with single board computers or microcontrollers. These setups also have the advantage that data processing can be performed on the spot, and only small data amounts have to be transmitted if needed, for example, via IoT infrastructures (Da Xu et al., 2014). Furthermore, camera gauges provide the benefit of potentially measuring flow velocities simultaneously by capturing short videos and tracking particles at the water surface (e.g., Eltner et al., 2020), which allows quantifying discharge with the same device eventually and thereby avoiding the installation of additional equipment. The application of camera gauges is suitable at rivers with periodic heavy debris loads or low angle river banks with large river width fluctuations leading to failure of other gauging techniques. Observing the river reach with an optical device enables capturing qualitative and quantitative information beyond the water stage or flow velocities. For instance, ephemeral rivers and extended flooded areas become observable, and snow coverage and ice growth can be assessed. Furthermore, the vegetation evolution might be monitored, or the river cross-section changes determined to ensure a continuous and reliable water stage-discharge curve. Thus, camera observations can practically support hydrological monitoring.