Synchronous variation of dissolved organic carbon and color in lakes
By Michael M. Pace, J. Cole. 2002
256 citations recorded by the source corpus.
Subfields: Environmental Chemistry, Oceanography, Water Science and Technology
View Paper: https://www.semanticscholar.org/paper/17a6681d9a6a226ac3d5919765eb6cc5c5a7291b
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In Environmental Chemistry
In Oceanography
In Water Science and Technology
Citations in the corpus
- Effects of water color on predation regimes and zooplankton assemblages in freshwater lakes (2003, background): “The humic compounds of DOC are the major factor controlling water color in lakes (Thurman 1985; Pace and Cole 2002).”
- Does autochthonous primary production drive variability in bacterial metabolism and growth efficiency in lakes dominated by terrestrial C inputs (2005, methodology): “The lakes, which vary in area from 0.8 to 45 ha (Pace & Cole 2002), are all in a similar hydrogeographic setting, and are surrounded by wetlands and upland forests without human habitation or agriculture (Carpenter & Kitchell 1993).”
- Water color affects the stratification, surface temperature, heat content, and mean epilimnetic irradiance of small lakes (2006, background): “Water color is highly variable among lakes in northtemperate regions, with neighboring lakes of similar morphometry exhibiting large differences in water color (Pace and Cole 2002).”
- Centennial‐long trends of lake browning show major effect of afforestation (2017, background): “Similarly, variability in DOC is influenced by variation in precipitation and flow (Pace and Cole 2002; Erlandsson et al. 2008).”
- Synchrony and seasonality in bacterioplankton communities of two temperate rivers (2005, background): “For example, Pace and Cole (2002) observed synchronous changes in DOC and water color among 20 lakes in northern Michigan related to the ice-out date and spring and summer precipitation, but they found that deviations from synchrony appeared to correlate with the absence of an outlet stream.”