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Source: InCites
Abstract
eutrophication artificial aquatic ecosystems Peel-Harvey estuarine system greenhouse gas emissions winter storms and-ocean aquatic continuum
Humans are altering coastal regions directly (land‐use, drainage) and indirectly (climate change). Alterations potentially create positive climate feedback loops by enhancing production and emission of aquatic greenhouse gases (GHGs) CO<sub>2</sub> , N<sub>2</sub> O, and CH<sub>4</sub> . We tested this hypothesis by measuring dissolved CO<sub>2</sub> , N<sub>2</sub> O, and CH<sub>4</sub> concentrations across the anthropogenic aquatic continuum (farm ponds, ditches, irrigation drains, streams, tidal rivers, and estuaries) and continuously during a winter storm. Combining measurements with hydrodynamic modeling enabled us to parameterize physical gas transfer uncertainties, revealing artificial waterways contributed disproportionately to emissions. Ditches and drains cover 5% of water surface area but produced >50% of emissions (2–11 Mmol d <sup>−1</sup> CO <sub>2</sub> ‐equivalents). But storms inverted this pattern by increasing estuary emissions 16‐fold (5.0 Mmol d <sup>−1</sup> CO <sub>2</sub> ‐equivalent), suggesting storm patterns could control both sources and magnitudes of aquatic GHG emissions. Findings show overlooked artificial drains and hard‐to‐measure storms will increasingly define the aquatic offsets of landscape carbon budgets.
Details
Title
Drainage Ditches (“Hot Spots”) and Storms (“Hot Moments”) Define Aquatic Greenhouse Gas (CO2 , CH4 , N2O) Emissions From the Land‐to‐Ocean Aquatic Continuum
Creators
Naomi S. Wells - Southern Cross University
Mustefa Yasin Reshid - Southern Cross University
Karl Hennig - Department of Water and Environmental Regulation
Matthew Hipsey - The University of Western Australia
Peisheng Huang - The University of Western Australia
Bradley D. Eyre - Southern Cross University
Publication Details
Geophysical research letters, Vol.52(15), pp.1-13
Publisher
Wiley-Blackwell Publishing, Inc.; WASHINGTON
Number of pages
13
Grant note
Research was funded through the Australian Research Council (LP150100451) led by Fiona Valesini (Murdoch University); NSW was funded by the Royal Society Te Apārangi (LIU2102).