Climate change and agricultural adaptation to it influence wind, water, harvest and tillage erosion in many ways. The interactions are complex and, for the most part, only partially understood and quantified. Very often, climate change leads to more erosion, but the opposite is also possible. However, chang es in erosion rates over time do not necessarily indicate a climate-change influence, as is often mistakenly assumed. Land-use changes are much more significant and influential. More process research is therefore needed to identify and quantify the diverse effects of these interacting drivers. It is undisputed, however, that climate change exacerbates the effects of soil buffer loss caused by erosion, as dry and wet periods become more pronounced and require greater buffering. It is therefore necessary to reduce all forms of erosion, especially tillage erosion, which is usually the second most important form of erosion in agriculture. In addition, the frequency of gravitational mass movements changes substantially, which can have a major impact on agriculture, especially in mountainous regions.