Episodic flooding causes sudden deoxygenation shocks in human-dominated rivers

  • Yongqiang Zhou*
  • , Jinling Wang
  • , Lei Zhou
  • , Wei Zhi
  • , Yunlin Zhang*
  • , Boqiang Qin
  • , Fengchang Wu
  • , R. Iestyn Woolway
  • , Stephen F. Jane
  • , Erik Jeppesen
  • , David P. Hamilton
  • , Marguerite A. Xenopoulos
  • , Robert G.M. Spencer
  • , Tom J. Battin
  • , Peter R. Leavitt*
  • *Corresponding author for this work

Research output: Contribution to journal/Conference contribution in journal/Contribution to newspaperJournal articleResearchpeer-review

2 Citations (Scopus)

Abstract

Dissolved oxygen (DO) sustains river ecosystems, but the effects of hydrological extremes remain poorly understood. While high river discharge (Q) enhances aeration, floods also deliver oxygen-consuming pollutants, making net impacts uncertain. Here, we analyze daily DO and its percent saturation (DO%sat), and Q in 1156 Chinese rivers over three years. We show that DO and DO%sat decrease with rising Q in 69.1% and 55.7% of rivers, respectively. Floods (Q > 95th percentile) cause abrupt declines in both DO (19.7%) and DO%sat (16.2%) in 80.1% and 69.4% of the rivers, respectively, with the sharpest declines in agricultural and urban areas. These abrupt deoxygenation events link to increased ammonium and land-use intensity, causing more frequent hypoxia in developed regions. Contrary to initial expectations, floods often reduce oxygen levels, with faster recovery in urbanized regions. As climate change intensifies flooding, such sudden deoxygenation shocks may degrade aquatic ecosystems particularly in human-altered landscapes.

Original languageEnglish
Article number6865
JournalNature Communications
Volume16
Issue1
ISSN2041-1723
DOIs
Publication statusPublished - Jul 2025

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