Many of us may have visited a chalk stream on a sunny summer day, the water clear and bubbling, ducks chattering away, and pollinators busy about their work. We may have strolled past an unassuming patch of dry sediment and thought nothing of it, barren as it looked. Little did we know, it was in fact a winterbourne, a habitat harder to identify and indeed rarer than downstream chalk stream reaches with year-round flow.
What is a winterbourne?
For centuries we have known that chalk streams are often several kilometres longer in winter than in summer. In recent years, however, it has become clear that the sections that go through flowing and dry phases are home to complex wildlife communities. This transition can be attributed to increased rainfall, and the rise in groundwater levels that follows.