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Current Browning of Surface Waters Will Be Further Promoted by Wetter Climate

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TLDR
In this paper, the authors show that positive trends in dissolved organic carbon (OC) concentrations in 474 streams, lakes, and rivers in boreal and subarctic ecosystems in Norway, Sweden, and Finland between 1990 and 2013 are surprisingly constant across climatic gradients and catchment sizes.
Abstract
Browning of surface waters because of increasing terrestrial dissolved organic carbon (OC) concentrations is a concern for drinking water providers and can impact land carbon storage. We show that positive trends in OC in 474 streams, lakes, and rivers in boreal and subarctic ecosystems in Norway, Sweden, and Finland between 1990 and 2013 are surprisingly constant across climatic gradients and catchment sizes (median, +1.4% year–1; interquartile range, +0.8–2.0% year–1), implying that water bodies across the entire landscape are browning. The largest trends (median, +1.7% year–1) were found in regions impacted by strong reductions in sulfur deposition, while subarctic regions showed the least browning (median, +0.8% year–1). In dry regions, precipitation was a strong and positive driver of OC concentrations, declining in strength moving toward high rainfall sites. We estimate that a 10% increase in precipitation will increase mobilization of OC from soils to freshwaters by at least 30%, demonstrating the ...

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Global lake responses to climate change

TL;DR: A review of physical lake variables and their responses to climate change is presented in this paper, where the authors discuss recent and expected lake responses and look towards future research opportunities in lake monitoring and modelling.
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Environmental effects of ozone depletion, UV radiation and interactions with climate change: UNEP Environmental Effects Assessment Panel, update 2017

Germar Bernhard, +41 more
TL;DR: The present 2017 Update Report assesses some of the highlights and new insights about the interactive nature of the direct and indirect effects of UV radiation, atmospheric processes, and climate change.
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The study of carbon in inland waters—from isolated ecosystems to players in the global carbon cycle

TL;DR: In this article, the authors describe the evolution of our understanding of the carbon cycle of inland waters, from studies of individual lakes with limited attention to the surrounding landsca cation.
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The essential value of long‐term experimental data for hydrology and water management

TL;DR: In this article, long-term experimental watersheds are used as a crucial evidence base for understanding and managing the provision of clean water supplies, predicting and mitigating the effects of floods, and protecting ecosystem services provided by rivers and wetlands.
References
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Journal ArticleDOI

Plumbing the Global Carbon Cycle: Integrating Inland Waters into the Terrestrial Carbon Budget

TL;DR: In this paper, the role of inland water ecosystems in the global carbon cycle has been investigated and it is shown that roughly twice as much C enters inland aquatic systems from land as is exported from land to the sea, roughly equally as inorganic and organic carbon.
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Lakes and reservoirs as regulators of carbon cycling and climate

TL;DR: The role of lakes in carbon cycling and global climate, examine the mechanisms influencing carbon pools and transformations in lakes, and discuss how the metabolism of carbon in the inland waters is likely to change in response to climate.
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Dissolved organic carbon trends resulting from changes in atmospheric deposition chemistry.

TL;DR: It is shown that rising trends in DOC between 1990 and 2004 can be concisely explained by a simple model based solely on changes in deposition chemistry and catchment acid-sensitivity, and that the rise in DOC is integral to recovery from acidification.
Journal ArticleDOI

Natural organic matter removal by coagulation during drinking water treatment: A review

TL;DR: Most of the NOM can be removed by coagulation, although, the hydrophobic fraction and high molar mass compounds of NOM are removed more efficiently than hydrophilic fraction and the low molarmass compounds.
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