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Karstic rivers are hydrogeologically conditioned to have spatial and seasonal changes in their discharge <ref>MEYER, A., E.I. MEYER & C. MEYER 2003. Lotic communities of two small temporary karstic stream systems (East Westphalia, Germany) along a longitudinal gradient of hydrological intermittency. Limnologica 33 (4): 271–279. </ref>. In the high plateau of Paderborn (Paderborner Hochfläche), the left tributary of the Lippe, Alme, itself and some of its tributaries are temporary rivers due to fluctuations of groundwater levels (Hungerbrunnen).
Projects:
- Preliminary sampling at the Menne
Index
Rivers of the Lippe catchment
Temporary rivers
- Menne <ref>Meyer, A., Meyer, E. I., & Meyer, C. (2003). Lotic communities of two small temporary karstic stream systems (East Westphalia, Germany) along a longitudinal gradient of hydrological intermittency. Limnologica, 33(4), 271-279.</ref>
- Alme
- Altenau
- Ellerbach
- Sauer<ref>Meyer, A., & Meyer, E. I. (2000). Discharge regime and the effect of drying on macroinvertebrate communities in a temporary karst stream in East Westphalia (Germany). Aquatic Sciences, 62(3), 216-231.</ref>
- Talgosse <ref>Meyer, A., Meyer, E. I., & Meyer, C. (2003). Lotic communities of two small temporary karstic stream systems (East Westphalia, Germany) along a longitudinal gradient of hydrological intermittency. Limnologica, 33(4), 271-279.</ref> (?)
Perennial rivers
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