FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4221105669> ?p ?o ?g. }

• W4221105669 endingPage "127688" @default.
• W4221105669 startingPage "127688" @default.
• W4221105669 abstract "Upland blanket peat is widespread in the headwaters of UK catchments, but much of it has been degraded through atmospheric pollution, vegetation change and erosion. Runoff generation in these headwaters is an important element of downstream flood risk and these areas are increasingly the focus of interventions to restore the peat ecosystem and to potentially mitigate downstream flooding. Here we use a series of multivariate analysis techniques to examine controls on storm runoff behavior within and between ten blanket peat catchments all within 5 km of one another and ranging in size from 0.2 to 3.9 ha. We find that: 1) for all 10 catchments, rainfall intensity is the dominant driver for both magnitude and timing of peak discharge, and that total and antecedent rainfall is important for peak discharge only in small storms; 2) there is considerable inter-catchment variability in: runoff coefficient, lag time, peak runoff, and their predictability from rainfall; however, 3) a significant fraction of the inter-catchment variability can be explained by catchment characteristics, particularly catchment area; and 4) catchment controls on peak discharge and runoff coefficient for small storms highlight the importance of storage and connectivity while those for large events suggest that surface flow attenuation dominates. Together these results suggest a switching rainfall-runoff behavior where catchment storage, connectivity and antecedent conditions control small discharge peaks but become increasingly irrelevant for larger storms. Our results suggest that, in the context of Natural Flood Management potential, expanding depression storage (e.g. distributed shallow water pools) in addition to existing restoration methods could increase the range of storms within which connectivity and storage remain important and that for larger storms measures which target surface runoff velocities are likely to be important." @default.
• W4221105669 created "2022-04-03" @default.
• W4221105669 creator A5004603859 @default.
• W4221105669 creator A5012346373 @default.
• W4221105669 creator A5015523648 @default.
• W4221105669 creator A5020738600 @default.
• W4221105669 creator A5027806957 @default.
• W4221105669 creator A5030845701 @default.
• W4221105669 creator A5047213536 @default.
• W4221105669 creator A5052196528 @default.
• W4221105669 creator A5069330732 @default.
• W4221105669 creator A5070434241 @default.
• W4221105669 creator A5089060962 @default.
• W4221105669 creator A5091680718 @default.
• W4221105669 date "2022-06-01" @default.
• W4221105669 modified "2023-10-06" @default.
• W4221105669 title "Rainfall intensity and catchment size control storm runoff in a gullied blanket peatland" @default.
• W4221105669 cites W1492543412 @default.
• W4221105669 cites W1575341832 @default.
• W4221105669 cites W1874333141 @default.
• W4221105669 cites W1887746348 @default.
• W4221105669 cites W1922543596 @default.
• W4221105669 cites W1966589547 @default.
• W4221105669 cites W1969128383 @default.
• W4221105669 cites W1977005193 @default.
• W4221105669 cites W1980691097 @default.
• W4221105669 cites W1986121817 @default.
• W4221105669 cites W1986424228 @default.
• W4221105669 cites W1991810074 @default.
• W4221105669 cites W1998660574 @default.
• W4221105669 cites W2000181792 @default.
• W4221105669 cites W2004898026 @default.
• W4221105669 cites W2012642395 @default.
• W4221105669 cites W2016820446 @default.
• W4221105669 cites W2021382445 @default.
• W4221105669 cites W2023656793 @default.
• W4221105669 cites W2025900644 @default.
• W4221105669 cites W2027078610 @default.
• W4221105669 cites W2032146127 @default.
• W4221105669 cites W2036920273 @default.
• W4221105669 cites W2037642718 @default.
• W4221105669 cites W2039358793 @default.
• W4221105669 cites W2044499285 @default.
• W4221105669 cites W2048240973 @default.
• W4221105669 cites W2049382750 @default.
• W4221105669 cites W2054215523 @default.
• W4221105669 cites W2056629573 @default.
• W4221105669 cites W2072552349 @default.
• W4221105669 cites W2091819522 @default.
• W4221105669 cites W2099534828 @default.
• W4221105669 cites W2107844016 @default.
• W4221105669 cites W2109375339 @default.
• W4221105669 cites W2112655628 @default.
• W4221105669 cites W2115838363 @default.
• W4221105669 cites W2116502410 @default.
• W4221105669 cites W2131393866 @default.
• W4221105669 cites W2132788415 @default.
• W4221105669 cites W2137295153 @default.
• W4221105669 cites W2142635246 @default.
• W4221105669 cites W2150845602 @default.
• W4221105669 cites W2158321802 @default.
• W4221105669 cites W2159382382 @default.
• W4221105669 cites W2159652411 @default.
• W4221105669 cites W2160707723 @default.
• W4221105669 cites W2164959551 @default.
• W4221105669 cites W2166363415 @default.
• W4221105669 cites W2168026490 @default.
• W4221105669 cites W2169568799 @default.
• W4221105669 cites W2338089160 @default.
• W4221105669 cites W2529792826 @default.
• W4221105669 cites W2595323920 @default.
• W4221105669 cites W2725171488 @default.
• W4221105669 cites W2782971760 @default.
• W4221105669 cites W2800294434 @default.
• W4221105669 cites W2896182405 @default.
• W4221105669 cites W2916067002 @default.
• W4221105669 cites W3107016899 @default.
• W4221105669 cites W3117400105 @default.
• W4221105669 cites W3132865203 @default.
• W4221105669 doi "https://doi.org/10.1016/j.jhydrol.2022.127688" @default.
• W4221105669 hasPublicationYear "2022" @default.
• W4221105669 type Work @default.
• W4221105669 citedByCount "4" @default.
• W4221105669 countsByYear W42211056692022 @default.
• W4221105669 countsByYear W42211056692023 @default.
• W4221105669 crossrefType "journal-article" @default.
• W4221105669 hasAuthorship W4221105669A5004603859 @default.
• W4221105669 hasAuthorship W4221105669A5012346373 @default.
• W4221105669 hasAuthorship W4221105669A5015523648 @default.
• W4221105669 hasAuthorship W4221105669A5020738600 @default.
• W4221105669 hasAuthorship W4221105669A5027806957 @default.
• W4221105669 hasAuthorship W4221105669A5030845701 @default.
• W4221105669 hasAuthorship W4221105669A5047213536 @default.
• W4221105669 hasAuthorship W4221105669A5052196528 @default.
• W4221105669 hasAuthorship W4221105669A5069330732 @default.
• W4221105669 hasAuthorship W4221105669A5070434241 @default.
• W4221105669 hasAuthorship W4221105669A5089060962 @default.
• W4221105669 hasAuthorship W4221105669A5091680718 @default.

• next