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Patterns in CH 4 and CO 2 concentrations across boreal rivers: Major drivers and implications for fluvial greenhouse emissions under climate change scenarios
Author(s) -
Campeau Audrey,
Giorgio Paul A.
Publication year - 2014
Publication title -
global change biology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 4.146
H-Index - 255
eISSN - 1365-2486
pISSN - 1354-1013
DOI - 10.1111/gcb.12479
Subject(s) - greenhouse gas , fluvial , boreal , environmental science , climate change , streams , atmospheric sciences , global warming , hydrology (agriculture) , methane , carbon dioxide , physical geography , ecology , geology , geography , structural basin , computer network , geotechnical engineering , computer science , biology , paleontology
It is now widely accepted that boreal rivers and streams are regionally significant sources of carbon dioxide (CO 2 ), yet their role as methane (CH 4 ) emitters, as well as the sensitivity of these greenhouse gas (GHG) emissions to climate change, are still largely undefined. In this study, we explore the large‐scale patterns of fluvial CO 2 and CH 4 partial pressure ( p CO 2 , p CH 4 ) and gas exchange (k) relative to a set of key, climate‐sensitive river variables across 46 streams and rivers in two distinct boreal landscapes of Northern Québec. We use the resulting models to determine the direction and magnitude of C‐gas emissions from these boreal fluvial networks under scenarios of climate change. River p CO 2 and p CH 4 were positively correlated, although the latter was two orders of magnitude more variable. We provide evidence that in‐stream metabolism strongly influences the dynamics of surface water p CO 2 and p CH 4 , but whereas p CO 2 is not influenced by temperature in the surveyed streams and rivers, p CH 4 appears to be strongly temperature‐dependent. The major predictors of ambient gas concentrations and exchange were water temperature, velocity, and DOC, and the resulting models indicate that total GHG emissions (C‐CO 2 equivalent) from the entire network may increase between by 13 to 68% under plausible scenarios of climate change over the next 50 years. These predicted increases in fluvial GHG emissions are mostly driven by a steep increase in the contribution of CH 4 (from 36 to over 50% of total CO 2 ‐equivalents). The current role of boreal fluvial networks as major landscape sources of C is thus likely to expand, mainly driven by large increases in fluvial CH 4 emissions.