According to a paper in Water Resources Research (2016) by Painter et al., the ATS model prioritizes depositing snowfall in topographic depressions during snow distribution. Only when these depressions are filled to a certain depth does the snow begin to distribute more evenly across non-depressed areas.
However, I’ve encountered an issue in my watershed simulation. My basin has very high topographic relief—the elevation of the river channels is often tens of meters lower than the surrounding terrain. At the same time, the snowfall amount in the region is not sufficient to allow accumulation in non-depressed areas. As a result, in my simulation, only the area directly over the river channel shows substantial snow accumulation, while other regions have little to no snow cover. This likely deviates from real-world conditions in the watershed.
I would like to know which parameters or variables I could adjust to improve this situation. Any suggestions would be greatly appreciated!
Chen,