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

In the majority of existing studies, streams are conceived as static objects that occupy
predefined regions of the landscape. However, empirical observations suggest that stream …

The ever‐changing hydroclimatic conditions of the landscape induce ceaseless variations in
the wet channel length (L) and the streamflow (Q) of a catchment. Here we use a perceptual …

Dynamic changes in the active portion of stream networks represent a phenomenon
common to diverse climates and geologic settings. However, mechanistically describing …

Despite recent evidence suggesting that groundwater inputs of dissolved inorganic carbon
(DIC) to rivers can contribute substantially to the fluvial evasion of carbon dioxide (CO2) …

Understanding the expansion and contraction dynamics of flowing drainage networks is
important for many research fields like ecology, hydrology, and biogeochemistry. This study …

Introduction Dissolved organic matter (DOM) composition varies over space and time, with a
multitude of factors driving the presence or absence of each compound found in the complex …

Streams and rivers are 'active pipelines' where high rates of carbon (C) turnover can lead to
globally important emissions of carbon dioxide (CO 2) and methane (CH 4) from surface …

A large portion of terrestrially derived carbon outgasses as carbon dioxide (CO 2) from
streams and rivers to the atmosphere. Particularly, the amount of CO 2 outgassing from …

Rivers are important sources of the carbon dioxide (CO 2) released into the atmosphere;
however, research on CO 2 emission from riverine headwater regions is sparse, particularly …