FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4207021402> ?p ?o ?g. }

• W4207021402 endingPage "127494" @default.
• W4207021402 startingPage "127494" @default.
• W4207021402 abstract "Rainfall represents the main driving force of runoff and soil erosion. Previous studies usually focused on the effects of general rainfall characteristics at event scale on runoff and soil erosion, but the effects of rainfall intensity fluctuation at intra-event scale, i.e., the temporal distribution of intensity bursts across the rainfall profile, have always been difficult to be characterized. In this study, the rainfall intensity profile was disaggregated into high-intensity zone and low-intensity zone using the average rainfall intensity as threshold, and a series of indicators were proposed to describe the features of rainfall intensity fluctuation. Field observations of runoff and soil loss in six grass-cover plots under natural rainfall conditions were conducted from 2011 to 2016 in the Loess Plateau of China. The main rainfall indicators influencing runoff coefficient (RC), sediment concentration (SC) and soil loss coefficient (SLC) were identified using the principal component analysis, and runoff and soil loss regression models were developed using data from 2011 to 2013 to predict RC, SC and SLC during 2014–2016. The results indicated that the natural rainfall events displayed strong intensity fluctuations (e.g., aggregation, intermittency, and variability), with approximate 78% of rainfall amount occurring in only 27% of rainfall duration. Most of the proposed rainfall intensity fluctuation indicators were significantly correlated with RC, SC and SLC (p < 0.05). The average intensity of rainfall peaks (Iap) and rainfall duration of high-intensity zone (RDh) were the main variables to simulate RC, and the average intensity of high-intensity zone (Iah) and relative amplitude of rainfall intensity (Ram) controlled SC and SLC. The models considering rainfall intensity fluctuation had good performances in predicting RC, SC and SLC with higher R2 values (0.64 vs 0.46), lower RMSE values (0.66 vs 0.76) and higher NSE values (0.54 vs 0.42) compared to the models only considering general rainfall characteristics. The prediction accuracy of SLC was higher than that of RC and that of SC was lowest. These results gain an insight into the marked influence of rainfall intensity fluctuation in generating and predicting runoff and soil loss, and shed light on exploring rainfall-erosion relationships." @default.
• W4207021402 created "2022-01-26" @default.
• W4207021402 creator A5002965595 @default.
• W4207021402 creator A5016816683 @default.
• W4207021402 creator A5027810506 @default.
• W4207021402 creator A5041847889 @default.
• W4207021402 creator A5042048777 @default.
• W4207021402 date "2022-04-01" @default.
• W4207021402 modified "2023-10-18" @default.
• W4207021402 title "Quantifying the effects of rainfall intensity fluctuation on runoff and soil loss: From indicators to models" @default.
• W4207021402 cites W1589356161 @default.
• W4207021402 cites W1632951317 @default.
• W4207021402 cites W1966352714 @default.
• W4207021402 cites W1987044514 @default.
• W4207021402 cites W2005628997 @default.
• W4207021402 cites W2012912804 @default.
• W4207021402 cites W2017880758 @default.
• W4207021402 cites W2030972496 @default.
• W4207021402 cites W2061744401 @default.
• W4207021402 cites W2078951193 @default.
• W4207021402 cites W2081036841 @default.
• W4207021402 cites W2098193917 @default.
• W4207021402 cites W2116178548 @default.
• W4207021402 cites W2131276455 @default.
• W4207021402 cites W2201108801 @default.
• W4207021402 cites W2294494133 @default.
• W4207021402 cites W2400114638 @default.
• W4207021402 cites W2409146422 @default.
• W4207021402 cites W2592079076 @default.
• W4207021402 cites W2594004682 @default.
• W4207021402 cites W2606074045 @default.
• W4207021402 cites W2766615506 @default.
• W4207021402 cites W2783807805 @default.
• W4207021402 cites W2909214044 @default.
• W4207021402 cites W2977223161 @default.
• W4207021402 doi "https://doi.org/10.1016/j.jhydrol.2022.127494" @default.
• W4207021402 hasPublicationYear "2022" @default.
• W4207021402 type Work @default.
• W4207021402 citedByCount "11" @default.
• W4207021402 countsByYear W42070214022023 @default.
• W4207021402 crossrefType "journal-article" @default.
• W4207021402 hasAuthorship W4207021402A5002965595 @default.
• W4207021402 hasAuthorship W4207021402A5016816683 @default.
• W4207021402 hasAuthorship W4207021402A5027810506 @default.
• W4207021402 hasAuthorship W4207021402A5041847889 @default.
• W4207021402 hasAuthorship W4207021402A5042048777 @default.
• W4207021402 hasConcept C107054158 @default.
• W4207021402 hasConcept C114793014 @default.
• W4207021402 hasConcept C121332964 @default.
• W4207021402 hasConcept C123157820 @default.
• W4207021402 hasConcept C127313418 @default.
• W4207021402 hasConcept C151730666 @default.
• W4207021402 hasConcept C153294291 @default.
• W4207021402 hasConcept C159390177 @default.
• W4207021402 hasConcept C185515318 @default.
• W4207021402 hasConcept C187320778 @default.
• W4207021402 hasConcept C18903297 @default.
• W4207021402 hasConcept C39432304 @default.
• W4207021402 hasConcept C50477045 @default.
• W4207021402 hasConcept C62520636 @default.
• W4207021402 hasConcept C76886044 @default.
• W4207021402 hasConcept C86803240 @default.
• W4207021402 hasConcept C93038891 @default.
• W4207021402 hasConceptScore W4207021402C107054158 @default.
• W4207021402 hasConceptScore W4207021402C114793014 @default.
• W4207021402 hasConceptScore W4207021402C121332964 @default.
• W4207021402 hasConceptScore W4207021402C123157820 @default.
• W4207021402 hasConceptScore W4207021402C127313418 @default.
• W4207021402 hasConceptScore W4207021402C151730666 @default.
• W4207021402 hasConceptScore W4207021402C153294291 @default.
• W4207021402 hasConceptScore W4207021402C159390177 @default.
• W4207021402 hasConceptScore W4207021402C185515318 @default.
• W4207021402 hasConceptScore W4207021402C187320778 @default.
• W4207021402 hasConceptScore W4207021402C18903297 @default.
• W4207021402 hasConceptScore W4207021402C39432304 @default.
• W4207021402 hasConceptScore W4207021402C50477045 @default.
• W4207021402 hasConceptScore W4207021402C62520636 @default.
• W4207021402 hasConceptScore W4207021402C76886044 @default.
• W4207021402 hasConceptScore W4207021402C86803240 @default.
• W4207021402 hasConceptScore W4207021402C93038891 @default.
• W4207021402 hasLocation W42070214021 @default.
• W4207021402 hasOpenAccess W4207021402 @default.
• W4207021402 hasPrimaryLocation W42070214021 @default.
• W4207021402 hasRelatedWork W1977554050 @default.
• W4207021402 hasRelatedWork W2007894603 @default.
• W4207021402 hasRelatedWork W2019688636 @default.
• W4207021402 hasRelatedWork W2038224349 @default.
• W4207021402 hasRelatedWork W2100357556 @default.
• W4207021402 hasRelatedWork W2367173121 @default.
• W4207021402 hasRelatedWork W2388837396 @default.
• W4207021402 hasRelatedWork W2945501434 @default.
• W4207021402 hasRelatedWork W3160598910 @default.
• W4207021402 hasRelatedWork W2494919088 @default.
• W4207021402 hasVolume "607" @default.
• W4207021402 isParatext "false" @default.
• W4207021402 isRetracted "false" @default.
• W4207021402 workType "article" @default.