Lakes and reservoirs as regulators of carbon cycling and climate

@article{Tranvik2009LakesAR,
  title={Lakes and reservoirs as regulators of carbon cycling and climate},
  author={Lars J. Tranvik and John A. Downing and James B. Cotner and Steven Arthur Loiselle and Robert G. Striegl and Thomas J. Ballatore and Peter Dillon and Kerri Finlay and Kenneth Fortino and Lesley B. Knoll and Pirkko Kortelainen and Tiit Kutser and S. H. H. Larsen and Isabelle Laurion and Dina M. Leech and S Leigh McCallister and Diane M. McKnight and John M. Melack and Erin P. Overholt and Jason A. Porter and Yves T. Prairie and William H. Renwick and F{\'a}bio Roland and Bradford Sherman and David W. Schindler and Sebastian Sobek and Alain Tremblay and Michael J. Vanni and Antonie Martinus Verschoor and Eddie von Wachenfeldt and Gesa A. Weyhenmeyer},
  journal={Limnology and Oceanography},
  year={2009},
  volume={54}
}
We explore 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. Furthermore, we project changes as global climate change in the abundance and spatial distribution of lakes in the biosphere, and we revise the estimate for the global extent of carbon transformation in inland waters. This synthesis demonstrates… 

Quantifying the relative importance of lake emissions in the carbon budget of a subarctic catchment

Climate change and thawing of permafrost will likely result in increased decomposition of terrestrial organic carbon and subsequent carbon emissions to the atmosphere from terrestrial and aquatic

Decrease in CO2 efflux from northern hardwater lakes with increasing atmospheric warming

This study finds that the lakes of central North America have shifted progressively from being substantial CO2 sources in the mid-1990s to sequestering CO2 by 2010, with a steady increase in annual mean pH, and attributes the observed changes in pH and CO2 uptake to an atmospheric-warming-induced decline in ice cover in spring.

Variable effects of climate change on carbon balance in northern ecosystems

  • A. Matveev
  • Environmental Science
    IOP Conference Series: Earth and Environmental Science
  • 2019
Accumulation of carbon dioxide (CO2) and methane (CH4) in the atmosphere of the planet accelerates climate change, and northern high-latitude regions are warming faster than the planetary average.

Inorganic carbon loading as a primary driver of dissolved carbon dioxide concentrations in the lakes and reservoirs of the contiguous United States

Accurate quantification of CO2 flux across the air‐water interface and identification of the mechanisms driving CO2 concentrations in lakes and reservoirs is critical to integrating aquatic systems

Temperature-controlled organic carbon mineralization in lake sediments

It is found that the mineralization of organic carbon in lake sediments exhibits a strongly positive relationship with temperature, which suggests that warmer water temperatures lead to more mineralization and less organic carbon burial.

A century of human‐driven changes in the carbon dioxide concentration of lakes

Now that evasion of carbon dioxide (CO2) from inland waters is accounted for in global carbon models, it is crucial to quantify how these fluxes have changed in the past and forecast how they may

A review of carbon sink or source effect on artificial reservoirs

  • W. PhyoeF. Wang
  • Environmental Science, Geology
    International Journal of Environmental Science and Technology
  • 2019
The inland water system is a key conduit in transporting carbon from land to ocean, but this conduit is not a neutral pipeline because it releases greenhouse gases into the atmosphere and also stores

Carbon dioxide emissions and sediment organic carbon burials across a gradient of trophic state in eleven New Zealand lakes

Lakes are known to be important to the global carbon balance as they are both CO2 sources to the atmosphere and also accumulate large amounts of carbon in their sediment. CO2 flux dynamics across the

Riverine coupling of biogeochemical cycles between land, oceans, and atmosphere

Streams, rivers, lakes, and other inland waters are important agents in the coupling of biogeochemical cycles between continents, atmosphere, and oceans. The depiction of these roles in global-scale

Sources and controls of organic carbon in lakes across the subarctic treeline

Abundant northern lakes have an intrinsic role in the transport, sequestration, and mineralization of terrestrial organic carbon. The quantity and quality of this carbon control vital aquatic
...

References

SHOWING 1-10 OF 132 REFERENCES

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

A BSTRACTBecause freshwater covers such a small fraction of the Earth’s surface area, inland freshwater ecosystems (particularly lakes, rivers, and reservoirs) have rarely been considered as

Role of lakes for organic carbon cycling in the boreal zone

We calculated the carbon loss (mineralization plus sedimentation) and net CO2 escape to the atmosphere for 79 536 lakes and total running water in 21 major Scandinavian catchments (size range 437–48

Arctic Lakes and Streams as Gas Conduits to the Atmosphere: Implications for Tundra Carbon Budgets

Current estimates of the arctic terrestrial sink for atmospheric CO2 may be 20 percent too high, according to measurements of the partial pressure of CO2 in 29 aquatic ecosystems across arctic Alaska.

Climate change decreases aquatic ecosystem productivity of Lake Tanganyika, Africa

There is evidence that climate warming is diminishing productivity in Lake Tanganyika, East Africa, and the impact of regional effects of global climate change on aquatic ecosystem functions and services can be larger than that of local anthropogenic activity or overfishing.

A Carbon Budget of a Small Humic Lake: An Example of the Importance of Lakes for Organic Matter Cycling in Boreal Catchments

It is found that the lake is a net heterotrophic ecosystem, subsidized by organic carbon inputs from the catchment and from emergent macrophyte production, and may simultaneously disperse and accumulate organic-associated radionuclides leaking from a final repository.

Dissolved organic carbon trends resulting from changes in atmospheric deposition chemistry

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.

Carbon dynamics in lakes of the boreal forest under a changing climate

Water-covered lands comprise approximately 30% of the total area of the world’s boreal forest biome. Most of these lands are peatlands (i.e., bogs and fens), which store over half of the total carbon

A catchment-scale carbon and greenhouse gas budget of a subarctic landscape

The overall catchment budget, given the size distribution of the individual ecosystem types and a first approximation of run-off as dissolved organic carbon, reveals a landscape currently with a significant sink capacity for atmospheric CO2, which is extremely sensitive to environmental changes, particularly those that affect the birch forest ecosystem.
...