FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2895963304> ?p ?o ?g. }

• W2895963304 endingPage "3890" @default.
• W2895963304 startingPage "3881" @default.
• W2895963304 abstract "Effective natural resource planning depends on understanding the prevalence of runoff generating processes. Within a specific area of interest, this demands reproducible, straightforward information that can complement available local data and can orient and guide stakeholders with diverse training and backgrounds. To address this demand within the contiguous United States (CONUS), we characterized and mapped the predominance of two primary runoff generating processes: infiltration‐excess and saturation‐excess runoff (IE vs. SE, respectively). Specifically, we constructed a gap‐filled grid of surficial saturated hydraulic conductivity using the Soil Survey Geographic and State Soil Geographic soils databases. We then compared surficial saturated hydraulic conductivity values with 1‐hr rainfall‐frequency estimates across a range of return intervals derived from CONUS‐scale random forest models. This assessment of the prevalence of IE versus SE runoff also incorporated a simple uncertainty analysis, as well as a case study of how the approach could be used to evaluate future alterations in runoff processes resulting from climate change. We found a low likelihood of IE runoff on undisturbed soils over much of CONUS for 1‐hr storms with return intervals <5 years. Conversely, IE runoff is most likely in the Central United States (i.e., Texas, Louisiana, Kansas, Missouri, Iowa, Nebraska, and Western South Dakota), and the relative predominance of runoff types is highly sensitive to the accuracy of the estimated soil properties. Leveraging publicly available data sets and reproducible workflows, our approach offers greater understanding of predominant runoff generating processes over a continental extent and expands the technical resources available to environmental planners, regulators, and modellers." @default.
• W2895963304 created "2018-10-26" @default.
• W2895963304 creator A5008953968 @default.
• W2895963304 creator A5013915494 @default.
• W2895963304 creator A5017158062 @default.
• W2895963304 creator A5025779572 @default.
• W2895963304 creator A5036732687 @default.
• W2895963304 creator A5049096257 @default.
• W2895963304 creator A5058617531 @default.
• W2895963304 creator A5065279338 @default.
• W2895963304 creator A5080013745 @default.
• W2895963304 creator A5080810030 @default.
• W2895963304 date "2018-11-20" @default.
• W2895963304 modified "2023-09-26" @default.
• W2895963304 title "Estimating dominant runoff modes across the conterminous United States" @default.
• W2895963304 cites W1554646359 @default.
• W2895963304 cites W164985 @default.
• W2895963304 cites W1661353177 @default.
• W2895963304 cites W1693142019 @default.
• W2895963304 cites W1785069639 @default.
• W2895963304 cites W1951242150 @default.
• W2895963304 cites W1957954620 @default.
• W2895963304 cites W1965534061 @default.
• W2895963304 cites W1973090862 @default.
• W2895963304 cites W1977334113 @default.
• W2895963304 cites W1977505744 @default.
• W2895963304 cites W1981646498 @default.
• W2895963304 cites W1997732436 @default.
• W2895963304 cites W2013205315 @default.
• W2895963304 cites W2019129161 @default.
• W2895963304 cites W2024488171 @default.
• W2895963304 cites W2028629255 @default.
• W2895963304 cites W2041314474 @default.
• W2895963304 cites W2051013537 @default.
• W2895963304 cites W2055705976 @default.
• W2895963304 cites W2055883695 @default.
• W2895963304 cites W2067248001 @default.
• W2895963304 cites W2076042261 @default.
• W2895963304 cites W2077038928 @default.
• W2895963304 cites W2085971990 @default.
• W2895963304 cites W2087634623 @default.
• W2895963304 cites W2091966455 @default.
• W2895963304 cites W2092905785 @default.
• W2895963304 cites W2093838258 @default.
• W2895963304 cites W2104683921 @default.
• W2895963304 cites W2112565907 @default.
• W2895963304 cites W2114937135 @default.
• W2895963304 cites W2123950892 @default.
• W2895963304 cites W2124738823 @default.
• W2895963304 cites W2128739352 @default.
• W2895963304 cites W2133049068 @default.
• W2895963304 cites W2143481518 @default.
• W2895963304 cites W2145635192 @default.
• W2895963304 cites W2146558524 @default.
• W2895963304 cites W2150034701 @default.
• W2895963304 cites W2151903232 @default.
• W2895963304 cites W2156386141 @default.
• W2895963304 cites W2156597263 @default.
• W2895963304 cites W2176130496 @default.
• W2895963304 cites W2259843377 @default.
• W2895963304 cites W2301232409 @default.
• W2895963304 cites W2311154973 @default.
• W2895963304 cites W2315693319 @default.
• W2895963304 cites W2328573691 @default.
• W2895963304 cites W2340078995 @default.
• W2895963304 cites W2518704075 @default.
• W2895963304 cites W2603223865 @default.
• W2895963304 cites W2757726802 @default.
• W2895963304 cites W2759664037 @default.
• W2895963304 cites W2768689216 @default.
• W2895963304 cites W2782900437 @default.
• W2895963304 cites W4246259708 @default.
• W2895963304 doi "https://doi.org/10.1002/hyp.13296" @default.
• W2895963304 hasPublicationYear "2018" @default.
• W2895963304 type Work @default.
• W2895963304 sameAs 2895963304 @default.
• W2895963304 citedByCount "16" @default.
• W2895963304 countsByYear W28959633042019 @default.
• W2895963304 countsByYear W28959633042020 @default.
• W2895963304 countsByYear W28959633042021 @default.
• W2895963304 countsByYear W28959633042022 @default.
• W2895963304 countsByYear W28959633042023 @default.
• W2895963304 crossrefType "journal-article" @default.
• W2895963304 hasAuthorship W2895963304A5008953968 @default.
• W2895963304 hasAuthorship W2895963304A5013915494 @default.
• W2895963304 hasAuthorship W2895963304A5017158062 @default.
• W2895963304 hasAuthorship W2895963304A5025779572 @default.
• W2895963304 hasAuthorship W2895963304A5036732687 @default.
• W2895963304 hasAuthorship W2895963304A5049096257 @default.
• W2895963304 hasAuthorship W2895963304A5058617531 @default.
• W2895963304 hasAuthorship W2895963304A5065279338 @default.
• W2895963304 hasAuthorship W2895963304A5080013745 @default.
• W2895963304 hasAuthorship W2895963304A5080810030 @default.
• W2895963304 hasBestOaLocation W28959633042 @default.
• W2895963304 hasConcept C127313418 @default.
• W2895963304 hasConcept C187320778 @default.
• W2895963304 hasConcept C18903297 @default.
• W2895963304 hasConcept C39432304 @default.

• next