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  How Sediment Supply, Sea-Level, and Glacial Isostatic Oscillations Drive Alluvial River Long-Profile Evolution and Terrace Formation

Ruby, A., McNab, F., Schildgen, T., Wickert, A., Fernandes, V. M. (2026): How Sediment Supply, Sea-Level, and Glacial Isostatic Oscillations Drive Alluvial River Long-Profile Evolution and Terrace Formation. - AGU Advances, 7, 1, e2025AV002035.
https://doi.org/10.1029/2025AV002035

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5036499.pdf (Publisher version), 28MB
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Copyright Date:
2026
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 Creators:
Ruby, Andreas1, 2, Author                 
McNab, Fergus2, Author                 
Schildgen, Taylor2, Author                 
Wickert, Andrew2, Author           
Fernandes, V. M.2, Author           
Affiliations:
1Submitting Corresponding Author, Deutsches GeoForschungsZentrum, ou_5026390              
24.6 Geomorphology, 4.0 Geosystems, Departments, GFZ Publication Database, GFZ Helmholtz Centre for Geosciences, ou_146045              

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Language(s): eng - English
 Dates: 20262026
 Publication Status: Finally published
 Pages: -
 Publishing info: -
 Table of Contents: -
 Rev. Type: -
 Identifiers: DOI: 10.1029/2025AV002035
OATYPE: Gold - DEAL Wiley
GFZPOF: p4 T5 Future Landscapes
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Title: AGU Advances
Source Genre: Journal, SCI, Scopus, oa, scopus oa 2022
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Publ. Info: -
Pages: - Volume / Issue: 7 (1) Sequence Number: e2025AV002035 Start / End Page: - Identifier: CoNE: https://gfzpublic.gfz.de/cone/journals/resource/20201104
Publisher: Wiley
Publisher: American Geophysical Union (AGU)