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All Outputs (10)

Release of dissolved organic carbon from upland peat (2002)
Journal Article
Worrall, F., Burt, T., Jaeban, R., Warburton, J., & Shedden, R. (2002). Release of dissolved organic carbon from upland peat. Hydrological Processes, 16(17), 3487-3504. https://doi.org/10.1002/hyp.1111

This study examines the release of dissolved organic carbon (DOC) from upland peat during the period of the autumn flushing. Hydroclimatic conditions were monitored in conjunction with measurements of absorbance and the E4/E6 ratio of the stream drai... Read More about Release of dissolved organic carbon from upland peat.

Torrent erosion in Lake District mountain cathments. (2002)
Book Chapter
Johnson, R., Warburton, J., & Burt, T. (2002). Torrent erosion in Lake District mountain cathments. In T. Burt, D. Thompson, & J. Warburton (Eds.), The British Uplands: Dynamics of Change (139-140). JNCC

Peat mass movements: a World and regional database. (2002)
Book Chapter
Mills, A., Warburton, J., & Higgitt, D. (2002). Peat mass movements: a World and regional database. In T. Burt, D. Thompson, & J. Warburton (Eds.), The British Uplands: Dynamics of Change (166-167). JNCC

GPS: A tool for mapping the uplands. (2002)
Book Chapter
Higgitt, D., & Warburton, J. (2002). GPS: A tool for mapping the uplands. In T. Burt, D. Thompson, & J. Warburton (Eds.), The British Uplands: Dynamics of Change (134-135). JNCC

Stability of an upland gravel-bed stream, Swinhope Burn, Northern England (2002)
Journal Article
Warburton, J., Danks, M., & Wishart, D. (2002). Stability of an upland gravel-bed stream, Swinhope Burn, Northern England. CATENA, 49(4), 309-329. https://doi.org/10.1016/s0341-8162%2802%2900046-2

Some upland gravel-bed streams often undergo frequent channel change in response to floods and changes in sediment supply. However, in others, where local conditions permit, long-term channel planform stability can be observed. This paper uses eviden... Read More about Stability of an upland gravel-bed stream, Swinhope Burn, Northern England.