Dissolved organic carbon trends resulting from changes in atmospheric deposition chemistry
By D. Monteith, J. Stoddard, C. Evans, H. D. Wit, M. Forsius, T. Høgåsen, A. Wilander, B. Skjelkvåle, D. Jeffries, J. Vuorenmaa and 3 more. Nature, 2007
1,751 citations recorded by the source corpus.
Subfields: Atmospheric Science, Environmental Chemistry, Oceanography
View Paper: https://www.semanticscholar.org/paper/16f20e111831e19a94bb04cc992c76f6ae114283
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In Atmospheric Science
In Environmental Chemistry
- Raphael M. Kudela
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- V. Trainer
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- Thomas S. Bianchi
In Oceanography
Citations in the corpus
- The changing carbon cycle of the coastal ocean (2013, background): “Regional increases in riverine DOC concentration have been reported, with multiple mechanisms suggested 78 .”
- Harmful algal blooms and climate change: Learning from the past and present to forecast the future (2015, background): “, 2010), and the trends towards ‘‘brownification’’ of coastal waters due to increased inputs of humic matter (Hansson et al., 2013; Monteith et al., 2007).”
- Global change pressures on soils from land use and management (2016, background): “Conversely, declining sulphur deposition has been associated with increased dissolved organic carbon fluxes from organic soils (Monteith et al., 2007) and decreased soil carbon stocks in temperate forest soils (Oulehle et al., 2011; Lawrence et al., 2012).”
- Integrating plant–soil interactions into global carbon cycle models (2009, background): “…global changes due to land use changes (Smith et al. 2008), nitrogen (N) enrichment (Magnani et al. 2007; Galloway et al. 2008), sulphur deposition (Monteith et al. 2007), CO2 fertilization (Woodward 2002; Norby et al. 2005) and changes in atmospheric ozone concentration (Sitch et al. 2007) are…”
- Revealing a conservation challenge through partitioned long‐term beta diversity: increasing turnover and decreasing nestedness of boreal lake metacommunities (2013, background): “Decreasing acid deposition has been related to the recovery of organic carbon concentrations, and thus levels of water clarity, in surface waters to pre-industrial levels (Monteith et al., 2007).”
- Microbial contributions to climate change through carbon cycle feedbacks (2008, background): “, 2004), sulphur deposition (Monteith et al., 2007) and changes in atmosphere ozone concentration (Sitch et al.”
- Diet-specific biomarkers show that high-quality phytoplankton fuels herbivorous zooplankton in large boreal lakes (2014, background): “The documented increase in the terrestrial DOM concentration in freshwater ecosystems in boreal and temperate areas (e.g., Monteith et al., 2007; Couture, Houle & Gagnon, 2012) calls for detailed information on the effects of DOM on aquatic food webs in different lake ecosystems.”
- Impacts of climate change on surface water quality in relation to drinking water production. (2009, background): “, 2003) and Northern America (Monteith et al., 2007).”
- Transparency, Geomorphology and Mixing Regime Explain Variability in Trends in Lake Temperature and Stratification Across Northeastern North America (1975-2014) (2017, background): “Long-term browning trends are likely influenced by both recovery from acidification [67,68,74] and increased precipitation and storm events occurring in the NENA region [75,76].”
- Centennial‐long trends of lake browning show major effect of afforestation (2017, background): “During the last decades, dissolved organic carbon (DOC) concentrations have increased dramatically in temperate surface waters throughout the Northern hemisphere (Monteith et al. 2007), paralleled by increases in water color (Roulet and Moore 2006; Kritzberg and Ekstr€om 2012).”