Articles | Volume 11, issue 4
Biogeosciences, 11, 1199–1213, 2014
Biogeosciences, 11, 1199–1213, 2014

Research article 27 Feb 2014

Research article | 27 Feb 2014

Can the heterogeneity in stream dissolved organic carbon be explained by contributing landscape elements?

A. M. Ågren et al.

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Cited articles

Ågren, A., Buffam, I., Jansson, M., and Laudon, H.: Importance of seasonality and small streams for the landscape regulation of dissolved organic carbon export, J. Geophys. Res., 112, G03003,, 2007.
Ågren, A., Haei, M., Köhler, S. J., Bishop, K., and Laudon, H.: Regulation of stream water dissolved organic carbon (DOC) concentrations during snowmelt; the role of discharge, winter climate and memory effects, Biogeosciences, 7, 2901–2913,, 2010.
Ågren, A. M., Haei, M., Blomkvist, P., Nilsson, M. B., and Laudon, H.: Soil frost enhances stream dissolved organic carbon concentrations during episodic spring snow melt from boreal mires, Glob. Change Biol., 18, 1895–1903, 2012.
Aitkenhead, J. A., Hope, D., and Billett, M. F.: The relationship between dissolved organic carbon in stream water and soil organic carbon pools at different spatial scales, Hydrol. Process., 13, 1289–1302, 1999.
Berggren, M., Laudon, H., and Jansson, M.: Hydrological control of organic carbon support for bacterial growth in boreal headwater streams, Microb. Ecol., 57, 170–178, 2009.
Final-revised paper