FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2742031345> ?p ?o ?g. }

• W2742031345 endingPage "466" @default.
• W2742031345 startingPage "452" @default.
• W2742031345 abstract "This study presents measurements of blowout topography obtained with annual terrestrial laser surveys carried out over a three-year period at a single, large bowl blowout located in the Provincelands Dunes section of Cape Cod National Seashore, in Massachusetts. The study blowout was selected because its axis is aligned with northwest winds that dominate the region, and because it was seemingly interacting with a smaller saucer blowout that had recently formed on the southern rim of the primary feature. Assuming that blowouts enlarge both horizontally and vertically in response to the wind regime, the objectives of the study were to determine both the amount of horizontal growth that the blowout experiences annually and the spatial patterns of vertical change that occur within the blowout. Changes to the blowout lobe surrounding the feature were also determined for areas with sparse enough vegetation cover to allow laser returns from the sand surface. The results show that the blowout consistently expanded outward during the three years, with the greatest expansion occurring at its southeast corner, opposite the prevailing winds. The most significant occurrence was the removal, in the first year, of the ridge that separated the two blowouts, resulting in a major horizontal shift of the southern rim of the new combined blowout. This displacement then continued at a lesser rate in subsequent years. The rim also shifted horizontally along the northwest to northeast sections of the blowout. Significant vertical loss occurred along the main axis of the blowout with the greatest loss concentrated along the southeast rim. On the lobe, there were large areas of deposition immediately downwind of the high erosion zones inside the blowout. However, there were also small erosion areas on the lobe, extending downwind from eroding sections of the rim. This study shows that: 1. blowouts can experience significant areal and volumetric changes in short periods of time; 2. significant changes may occur relatively suddenly when adjacent blowouts combine into a single feature; and 3. the sediment transport paths are highly controlled by the topography. The joining of two blowouts not only creates a new larger feature, but it also releases large amounts of sediment that are then distributed across the landscape downwind, creating a potential for major changes to a landscape over the longer term." @default.
• W2742031345 created "2017-08-08" @default.
• W2742031345 creator A5043194468 @default.
• W2742031345 creator A5050875946 @default.
• W2742031345 creator A5059912303 @default.
• W2742031345 creator A5062131005 @default.
• W2742031345 creator A5085827069 @default.
• W2742031345 date "2017-10-01" @default.
• W2742031345 modified "2023-10-13" @default.
• W2742031345 title "Three years of morphologic changes at a bowl blowout, Cape Cod, USA" @default.
• W2742031345 cites W1159080871 @default.
• W2742031345 cites W1501993320 @default.
• W2742031345 cites W1524596790 @default.
• W2742031345 cites W1555985184 @default.
• W2742031345 cites W1640156343 @default.
• W2742031345 cites W1851965473 @default.
• W2742031345 cites W1920461408 @default.
• W2742031345 cites W1968477904 @default.
• W2742031345 cites W1974711719 @default.
• W2742031345 cites W1975540301 @default.
• W2742031345 cites W1976924822 @default.
• W2742031345 cites W1981202887 @default.
• W2742031345 cites W1983138004 @default.
• W2742031345 cites W1986838376 @default.
• W2742031345 cites W1986892169 @default.
• W2742031345 cites W2000363286 @default.
• W2742031345 cites W2013567663 @default.
• W2742031345 cites W2015380342 @default.
• W2742031345 cites W2016408884 @default.
• W2742031345 cites W2018043298 @default.
• W2742031345 cites W2024323224 @default.
• W2742031345 cites W2026687432 @default.
• W2742031345 cites W2029071972 @default.
• W2742031345 cites W2033518088 @default.
• W2742031345 cites W2037842519 @default.
• W2742031345 cites W2039004662 @default.
• W2742031345 cites W2039705885 @default.
• W2742031345 cites W2041127585 @default.
• W2742031345 cites W2061751814 @default.
• W2742031345 cites W2062717967 @default.
• W2742031345 cites W2066026749 @default.
• W2742031345 cites W2070481632 @default.
• W2742031345 cites W2077122818 @default.
• W2742031345 cites W2082045605 @default.
• W2742031345 cites W2084357194 @default.
• W2742031345 cites W2091557646 @default.
• W2742031345 cites W2094888434 @default.
• W2742031345 cites W2096006371 @default.
• W2742031345 cites W2100385381 @default.
• W2742031345 cites W2100418448 @default.
• W2742031345 cites W2107482389 @default.
• W2742031345 cites W2116910522 @default.
• W2742031345 cites W2131411265 @default.
• W2742031345 cites W2132290644 @default.
• W2742031345 cites W2135613720 @default.
• W2742031345 cites W2139036929 @default.
• W2742031345 cites W2144654897 @default.
• W2742031345 cites W2154523081 @default.
• W2742031345 cites W2155579859 @default.
• W2742031345 cites W2156263724 @default.
• W2742031345 cites W2158789815 @default.
• W2742031345 cites W2161964273 @default.
• W2742031345 cites W2167215358 @default.
• W2742031345 cites W2188002297 @default.
• W2742031345 doi "https://doi.org/10.1016/j.geomorph.2017.07.012" @default.
• W2742031345 hasPublicationYear "2017" @default.
• W2742031345 type Work @default.
• W2742031345 sameAs 2742031345 @default.
• W2742031345 citedByCount "28" @default.
• W2742031345 countsByYear W27420313452017 @default.
• W2742031345 countsByYear W27420313452018 @default.
• W2742031345 countsByYear W27420313452019 @default.
• W2742031345 countsByYear W27420313452020 @default.
• W2742031345 countsByYear W27420313452021 @default.
• W2742031345 countsByYear W27420313452022 @default.
• W2742031345 countsByYear W27420313452023 @default.
• W2742031345 crossrefType "journal-article" @default.
• W2742031345 hasAuthorship W2742031345A5043194468 @default.
• W2742031345 hasAuthorship W2742031345A5050875946 @default.
• W2742031345 hasAuthorship W2742031345A5059912303 @default.
• W2742031345 hasAuthorship W2742031345A5062131005 @default.
• W2742031345 hasAuthorship W2742031345A5085827069 @default.
• W2742031345 hasBestOaLocation W27420313451 @default.
• W2742031345 hasConcept C100970517 @default.
• W2742031345 hasConcept C111368507 @default.
• W2742031345 hasConcept C127313418 @default.
• W2742031345 hasConcept C151730666 @default.
• W2742031345 hasConcept C166957645 @default.
• W2742031345 hasConcept C205649164 @default.
• W2742031345 hasConcept C2777628658 @default.
• W2742031345 hasConcept C2780759522 @default.
• W2742031345 hasConcept C32277403 @default.
• W2742031345 hasConceptScore W2742031345C100970517 @default.
• W2742031345 hasConceptScore W2742031345C111368507 @default.
• W2742031345 hasConceptScore W2742031345C127313418 @default.
• W2742031345 hasConceptScore W2742031345C151730666 @default.
• W2742031345 hasConceptScore W2742031345C166957645 @default.
• W2742031345 hasConceptScore W2742031345C205649164 @default.

• next