Biogeochemical implications of climate change for tropical rivers and floodplains
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Consequently, anoxic zones may develop even in shallow water bodies, and stronger wind events than in the temperate zones are needed to provoke mixing of the water layers of warm lakes.
“Consequently, anoxic zones may develop even in shallow water bodies, and stronger wind events than in the temperate zones are needed to provoke mixing of the water layers of warm lakes [106].”
From Urban Stream and Wetland Restoration in the Global South—A DPSIR Analysis (2019) · cites this paper as [106]
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- Authors
- Hamilton, S. K.
- Affiliations
- Michigan State University (US)
- Corresponding author
- Hamilton, Stephen K.
- ORCID
- Hamilton, Stephen K.
- Venue
- Hydrobiologia
- Published
- 2010-01-13
- Volume
- 657
- Issue
- 1
- Pages
- 19-35
- ISSN
- 0018-8158 (ISSN-L)
- 1573-5117
- OpenAlex
- W1982693352
- Cited by
- 92
- References
- 126
- Citations by year
- 2026: 1 · 2025: 11 · 2024: 4 · 2023: 2 · 2022: 7 · 2021: 8 · 2020: 3 · 2019: 5 · 2018: 4 · 2017: 5 · 2016: 7 · 2015: 4 · 2014: 3 · 2013: 9 · 2012: 8
- FWCI
- 7.50
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Hydrobiologia (publishedVersion)
- Griffith Research Online (submittedVersion)
- Topics
- Physical Sciences › Environmental Science › Environmental Chemistry › Soil and Water Nutrient Dynamics
- Physical Sciences › Environmental Science › Environmental Chemistry › Aquatic Ecosystems and Phytoplankton Dynamics
- Physical Sciences › Environmental Science › Ecology › Peatlands and Wetlands Ecology
- Keywords
- climate change, tropical rivers, floodplain, river discharge, floodplain inundation, methane emissions, dissolved oxygen depletion, Delta, ecosystem services, climate feedbacks, deforestation, dams, hydrological change, wetlands
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