Springs (discharge of groundwater) are common in all landscapes even if the abundance and the remaining times and sizes of aquifers differ.

If it is not deep aquifers or karst, springs are reflecting the climatic conditions (e.g. mean temperature, seasonality, precipitation) should be reflected (with some delay) in the springs.

AND

Many spring species are stenoecic and adapted to very specific conditions of temperature and water chemistry.

We did some studies on this in the past, but now i would like to develop a concept for using springs and spring species for climate change impacts because most weather stations are in settlements and not in natural ecosystems.

Are there people around with similar interests?

Carl

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