Methane (CH4) is a potent greenhouse gas and its concentrations have tripled in the
atmosphere since the industrial revolution. There is evidence that global warming has …

Agricultural headwaters are positioned at the interface between terrestrial and aquatic
ecosystems and, therefore, at the margins of scientific disciplines. They are deemed devoid …

The increase in atmospheric methane (CH 4) level directly contributes to approximately one-
fifth of global mean temperature rise since preindustrial era, only next to CO 2. Global …

Rivers are considered as an important source of methane (CH 4) to the atmosphere, but our
understanding for the methanogenic pathway in rivers and its linkage with CH 4 emission is …

Inland waters (rivers, lakes, and reservoirs) have been recognized as hotspots of methane
(CH 4) emissions. However, the magnitude and spatiotemporal pattern of CH 4 emissions …

Natural and constructed inland waters emit globally significant amounts of greenhouse
gasses (GHGs) into the atmosphere. As a result of human-induced alterations in the …

Artificial channels, common features of inland waters, have been suggested as significant
contributors to methane (CH4) and carbon dioxide (CO2) dynamics and emissions; …

Carbon-water interaction studies between aquatic and terrestrial ecosystems are especially
needed today in Arctic and Boreal regions, as they are facing drastic warming and …

Lakes are important component of the regional carbon cycle and a significant sources of
greenhouse gases (GHG) to the atmosphere. However, the regional variations in carbon …

Ebullition transports large amounts of the potent greenhouse gas methane (CH 4) from
aquatic sediments to the atmosphere. River beds are a main source of biogenic CH 4, but …