Dry riverbeds are contributing to climate change more than previously thought

Dr Nathan Waltham from the Tropical Water and Aquatic Eco-systems Research Centre (TropWATER) and James Cook University in Australia, joined scientists from 22 other countries who looked at 212 dry riverbeds on every continent on earth.

He said the contribution of intermittent rivers and streams to the process of carbon cycling -- the process by which carbon is circulated around the ecosystem -- is largely ignored.

"There is a substantial amount of plant litter that accumulates in dry riverbeds and when they flow again this material can breakdown rapidly. We've now estimated the potential short-term CO₂ emissions during these rewetting events."

"We believe that a single pulse of CO₂ emission upon litter rewetting contributes up to 10% of the daily CO₂ emission compared to perennial rivers and streams, particularly in temperate climates. What this means is that the contributions of intermittent rivers and streams should be included in global carbon-cycling assessments," said Dr Waltham.

The scientists found that aridity, surrounding vegetation, channel width and dry-phase duration explained most variability in the quantity and decomposability of plant litter.

He said that the new data shows the contribution of CO₂ from intermittent rivers and streams is higher than previously thought.

"Taking rivers and streams that only flow at certain times into account would improve estimates of the consequences of global climate change on carbon cycling -- given that the extent of these rivers and streams will increase, and periods of drying will become more prolonged in many regions," said Dr Waltham.

About the research

Intermittent rivers, as the name suggests, sometimes stop flowing and can dry completely. Although far less studied than permanent rivers, they could represent half of the world's river network and, in response to climate change and increasing water demands, may come to dominate the landscape in some regions.