Headwaters are hotspots of carbon dioxide (CO2) evasion from rivers. While emerging
evidence suggests that groundwater contributes disproportionately to CO2 in headwater …

Gas exchange across the air–water boundary of streams and rivers is a globally large
biogeochemical flux. Gas exchange depends on the solubility of the gas of interest, the gas …

The evasions of methane (CH 4) and carbon dioxide (CO 2) from inland waters represent
substantial fluxes of greenhouse gases into the atmosphere, offsetting a large part of the …

Gas exchange across the air–water interface drives the flux of climate-relevant gases and is
critical for biogeochemical processes in aquatic ecosystems. Despite the presence of …

Evasion of greenhouse gases (GHG) from fluvial systems is now recognized as a significant
component of the global carbon cycle. However, the magnitudes of GHG fluxes remain …

Headwater streams can be important sources of carbon dioxide (CO2) and methane (CH4)
to the atmosphere. However, the influence of groundwater–stream connectivity on the …

Globally, inland waters emit over 2 Pg of carbon per year as carbon dioxide, of which the
majority originates from streams and rivers. Despite the global significance of fluvial carbon …

Inland waters, including streams and rivers, are active components of the global carbon
cycle. Despite the large areal extent of the world's mountains, the role of mountain streams …

Warming in mountains is known to intensify aridity and threaten water availability globally. Its
impacts on water quality, however, have remained poorly understood. Here we collate long …

Most reservoirs in subtropical areas experience periodic variations in the thermal structure of
their water columns, with times of strong thermal stratification being succeeded by periods of …