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Parsons, Anthony J., Brazier, Richard E., Wainwright, John, Powell, D. Mark (2008) Scale relationships in hillslope runoff and erosion Reply. Earth Surface Processes and Landforms, 33 (10) 1637-1638 doi:10.1002/esp.1628

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Reference TypeJournal (article/letter/editorial)
TitleScale relationships in hillslope runoff and erosion Reply
JournalEarth Surface Processes and Landforms
AuthorsParsons, Anthony J.Author
Brazier, Richard E.Author
Wainwright, JohnAuthor
Powell, D. MarkAuthor
Year2008 (September)Volume33
Issue10
PublisherWiley
DOIdoi:10.1002/esp.1628Search in ResearchGate
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Mindat Ref. ID14960064Long-form Identifiermindat:1:5:14960064:6
GUID0
Full ReferenceParsons, Anthony J., Brazier, Richard E., Wainwright, John, Powell, D. Mark (2008) Scale relationships in hillslope runoff and erosion Reply. Earth Surface Processes and Landforms, 33 (10) 1637-1638 doi:10.1002/esp.1628
Plain TextParsons, Anthony J., Brazier, Richard E., Wainwright, John, Powell, D. Mark (2008) Scale relationships in hillslope runoff and erosion Reply. Earth Surface Processes and Landforms, 33 (10) 1637-1638 doi:10.1002/esp.1628
In(2008, September) Earth Surface Processes and Landforms Vol. 33 (10) Wiley

See Also

These are possibly similar items as determined by title/reference text matching only.

Parsons, Anthony J., Brazier, Richard E., Wainwright, John, Powell, D. Mark (2006) Scale relationships in hillslope runoff and erosion. Earth Surface Processes and Landforms, 31 (11) 1384-1393 doi:10.1002/esp.1345
Parsons, Anthony J., Wainwright, John, Brazier, Richard E., Powell, D. Mark (2008) Is sediment delivery a fallacy? Reply. Earth Surface Processes and Landforms, 33 (10) 1630-1631 doi:10.1002/esp.1627
Parsons, Anthony J., Wainwright, John, Brazier, Richard E., Powell, D. Mark (2006) Is sediment delivery a fallacy?. Earth Surface Processes and Landforms, 31 (10) 1325-1328 doi:10.1002/esp.1395
Parsons, Anthony J., Wainwright, John, Mark Powell, D., Kaduk, Jörg, Brazier, Richard E. (2004) A conceptual model for determining soil erosion by water. Earth Surface Processes and Landforms, 29 (10) 1293-1302 doi:10.1002/esp.1096
Wainwright, John, Parsons, Anthony J., MĂŒller, Eva N., Brazier, Richard E., Powell, D. Mark, Fenti, Bantigegne (2008) A transport-distance approach to scaling erosion rates: 1. Background and model development. Earth Surface Processes and Landforms, 33 (5) 813-826 doi:10.1002/esp.1624
Wainwright, John, Parsons, Anthony J., MĂŒller, Eva N., Brazier, Richard E., Powell, D. Mark, Fenti, Bantigegne (2008) A transport-distance approach to scaling erosion rates: 3. Evaluating scaling characteristics ofMahleran. Earth Surface Processes and Landforms, 33 (7) 1113-1128 doi:10.1002/esp.1622
Wainwright, John, Parsons, Anthony J., MĂŒller, Eva N., Brazier, Richard E., Powell, D. Mark, Fenti, Bantigegne (2008) A transport-distance approach to scaling erosion rates: 2. sensitivity and evaluation of Mahleran. Earth Surface Processes and Landforms, 33 (6) 962-984 doi:10.1002/esp.1623
Wainwright, John, Parsons, Anthony J., MĂŒller, Eva N., Brazier, Richard E., Powell, D. Mark (2010) Standing proud: a response to ‘Soil-erosion models: where do we really stand?’ by Smith et al. Earth Surface Processes and Landforms, 35 (11) 1349-1356 doi:10.1002/esp.2047
Wainwright, John, Parsons, Anthony J., MĂŒller, Eva N., Brazier, Richard E., Powell, D. Mark (2009) Response to Kinnell's ‘Comment on “A transport-distance approach to scaling erosion rates: III. Evaluating scaling characteristics of Mahleran”’. Earth Surface Processes and Landforms, 34 (9) 1320-1321 doi:10.1002/esp.1816
Kinnell, P. I. A. (2008) Comment on ‘Scale relationships in hillslope runoff and erosion’ (Earth Surface Processes and Landforms 31: 1364-1383 (2006)) Earth Surface Processes and Landforms, 33 (10) 1632-1636 doi:10.1002/esp.1630
Wainwright, John, J. Parsons, Anthony, N. MĂŒller, Eva, E. Brazier, Richard, Mark Powell, D. (2009) Response to Hairsine's and Sander's ‘Comment on “A transport-distance based approach to scaling erosionrates”: Parts 1, 2 and 3 by Wainwrightet al.’. Earth Surface Processes and Landforms, 34 (6) 886-890 doi:10.1002/esp.1781
 
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