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Number of items: 9.

Amvrosiadi, Nino; Bishop, Kevin H; Seibert, Jan (2017). Soil moisture storage estimation based on steady vertical fluxes under equilibrium. Journal of Hydrology, 553:798-804.

Bishop, Kevin H; Seibert, Jan (2015). A primer for hydrology: the beguiling simplicity of Water's journey from rain to stream at 30. Hydrological Processes, 29(16):3443-3446.

Gebreyohannis Gebrehiwot, Solomon; Gärdenäs, Annemieke I; Bewket, Woldeamlak; Seibert, Jan; Ilstedt, Ulrik; Bishop, Kevin H (2014). The long-term hydrology of East Africa’s water tower: statistical change detection in the watersheds of the Abbay Basin. Regional Environmental Change, 14(1):321-331.

Lyon, Steve W; Nathanson, Marcus; Spans, André; Grabs, Thomas J; Laudon, Hjalmar; Temnerud, Johan; Bishop, Kevin H; Seibert, Jan (2012). Specific discharge variability in a boreal landscape. Water Resources Research, 48:W08506.

Bishop, Kevin H; Buffam, Ishi; Erlandsson, M; Fölster, J; Laudon, Hjalmar; Seibert, Jan; Temnerud, Johan (2008). Aqua Incognita: the unknown headwaters. Hydrological Processes, 22(8):1239-1242.

Ågren, Anneli; Jansson, Mats; Ivarsson, Hans; Bishop, Kevin H; Seibert, Jan (2008). Seasonal and runoff-related changes in total organic carbon concentrations in the River Öre, Northern Sweden. Aquatic Sciences, 70(1):21-29.

Buffam, Ishi; Laudon, Hjalmar; Seibert, Jan; Mörth, Carl-Magnus; Bishop, Kevin H (2008). Spatial heterogeneity of the spring flood acid pulse in a boreal stream network. Science of the Total Environment, 407(1):708-722.

Cory, Neil; Laudon, Hjalmar; Köhler, Stephan; Seibert, Jan; Bishop, Kevin H (2007). Evolution of soil solution aluminum during transport along a forested boreal hillslope. Journal of Geophysical Research, 112(G3):online.

Temnerud, Johan; Seibert, Jan; Jansson, Mats; Bishop, Kevin H (2007). Spatial variation in discharge and concentrations of organic carbon in a catchment network of boreal streams in northern Sweden. Journal of Hydrology, 342(1-2):72-87.

This list was generated on Thu Jul 18 11:23:00 2019 CEST.