Undervalued dry riverbeds: A key factor in equating intermittent river CO 2 emissions to perennial rivers.

Publisher: Pergamon Press Country of Publication: England NLM ID: 0105072 Publication Model: Print-Electronic Cited Medium: Internet ISSN: 1879-2448 (Electronic) Linking ISSN: 00431354 NLM ISO Abbreviation: Water Res Subsets: MEDLINE

Original Publication: Oxford, Pergamon Press.

Rivers*/chemistry ; Carbon Dioxide*/analysis ; Environmental Monitoring*/methods; China ; Carbon Cycle

Intermittent rivers in semiarid and arid regions, constituting over half of the world's rivers, alternate the carbon cycle interactions among the biosphere, hydrosphere, and atmosphere. Inadequate quantification of flow duration and river water surface area, along with overlooked CO 2 emissions from dry riverbeds, result in notable inaccuracies in global carbon cycle assessments. High-resolution remote sensing images combined with intensive field measurements and hydrological modelling were used to estimate and extract the flow duration, river water surface area and dry riverbed area of Huangfuchuan, an intermittent river watershed that acts as a major tributary of the Yellow River in semiarid Northwest China. CO 2 emission rates and partial pressures in water and air across the watershed were in-situ measured. In 2018, the flow duration of Huangfuchuan increased from less than 5 days in the first-order tributary to 150 days in the sixth-order mainstream. River water surface area estimated by remote sensing extraction plus the hydrodynamic model simulation varied from 3.9 to 88.6 km ² under 5 %-95 % discharge frequencies. CO 2 emissions from the water-air interface and dry riverbed in 2018 were estimated at 582.3 × 10 ³ and 355.2 × 10 ³ ton, respectively. The estimated total annual emission (937.5 × 10 ³ ton) aligns closely with the range of emissions (67.3 × 10 ³ -1377.2 × 10 ³ ton) calculated for the water-air interface alone, derived using DEM river length and hydraulic geometry method. This similarity can be attributed to the overestimation of flow duration and flow velocity, as well as the over- or under-estimation of river water surface area and slope. The new method proposed in this study has large potential to be applied in estimating CO 2 emissions from data-scarce intermittent rivers located in mountainous regions and provides a standardized solution in the estimation of CO 2 emission. Results of this research reveal the spatiotemporal distribution of CO 2 emissions along an intermittent river system and highlight the substantial role of dry riverbed in carbon cycle.
Competing Interests: Declaration of competing interest The authors declare the following financial interests/personal relationships which may be considered as potential competing interests: Chao Qin, Baosheng Wu, Mengzhen Xu, Lishan Ran reports financial support was provided by National Natural Science Foundation of China. Chao Qin reports financial support was provided by China Postdoctoral Science Foundation. If there are other authors, they declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.
(Copyright © 2024. Published by Elsevier Ltd.)

Keywords: CO(2) emission; Flow duration; Intermittent river; Mountainous river; River surface extraction

142M471B3J (Carbon Dioxide)

Date Created: 20240608 Date Completed: 20240623 Latest Revision: 20240623

20240624

10.1016/j.watres.2024.121859

38851114