Wetland position in the landscape: Impact on water storage and flood buffering

On-going climatic changes and land-use changes may impact water storage dynamics within wetlandscapes (defined as the entire hydrological catchments of interconnected wetland systems). These dynamics are closely linked to many wetland ecosystem services including flood buffering, nutrient retention and biodiversity support. Here, we investigate if and how current water storage dynamics can differ between wetlands within the same wetlandscape. Based on continuous monitoring of water levels in multiple wetlands throughout a growing season (spring, summer, autumn) in Vattholma, Sweden, we show that there are two distinct storage behaviours depending on the position of the wetland within the landscape. Headwater wetland regions were active in temporary storage of surplus water from regular summer rains while water levels of downstream wetlands dropped to seasonal low values without responding to individual summer precipitation events. Thereby, the downstream wetlands maintained capacity to buffer extreme floods. We also found that headwater wetlands were associated with complex and patchy inundation, which causes habitat conditions to vary over short time scales both within and among these wetlands, in contrast to the prolonged low-water state of the downstream wetlands. These differences between headwater-downstream wetlands imply that the functionality of an entire wetlandscape cannot be assessed by simple extrapolation of data from monitoring stations that typically are located downstream of headwater regions. Increased understanding of these differences can support wetland management practices that target location-specific nature-based solutions and ecosystem services.

Automated summary

This study investigated the differences in water storage dynamics between wetlands within the same wetlandscape. The researchers found that wetlands in different positions exhibit two distinct storage behaviors. Headwater wetlands are able to store excess water to buffer floods, while downstream wetlands experience seasonal low water levels. The study also revealed that headwater wetlands have complex and patchy inundation patterns, while downstream wetlands are characterized by prolonged low-water states.