Alpine Glacier Shrinkage Drives Shift in Dissolved Organic Carbon Export From Quasi‐Chemostasis to Transport Limitation-Reference-Cited by-同舟云学术

Alpine Glacier Shrinkage Drives Shift in Dissolved Organic Carbon Export From Quasi‐Chemostasis to Transport Limitation

Published:2019-08-12 Issue:15 Volume:46 Page:8872-8881
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Boix Canadell Marta¹^ORCID,Escoffier Nicolas¹²^ORCID,Ulseth Amber J.¹³^ORCID,Lane Stuart N.⁴^ORCID,Battin Tom J.¹^ORCID

Affiliation:

1. Stream Biofilm and Ecosystem Research Laboratory, School of Architecture, Civil and Environmental Engineering École Polytechnique Fédérale de Lausanne Lausanne Switzerland

2. Now at Institute of Earth Surface Dynamics (IDYST) University of Lausanne Lausanne Switzerland

3. Now at Department of Biological Sciences Sam Houston State University Huntsville TX USA

4. Institute of Earth Surface Dynamics (IDYST) University of Lausanne Lausanne Switzerland

Funder

Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL083424

Reference48 articles.

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2. Combined Flow Abstraction and Climate Change Impacts on an Aggrading Alpine River

3. Changes in Dissolved Organic Matter (DOM) Fluorescence in Proglacial Antarctic Streams

4. Barton K.(2018).MuMIn: Multi‐Model Inference.R package version1.42.1.https://CRAN.R‐project.org/package=MuMIn

5. The boundless carbon cycle

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