FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2049703200> ?p ?o ?g. }

• W2049703200 endingPage "149" @default.
• W2049703200 startingPage "139" @default.
• W2049703200 abstract "Abstract In nature, several types of landforms have simple shapes: as they evolve they tend to take on an ideal, simple geometric form such as a cone, an ellipsoid or a paraboloid. Volcanic landforms are possibly the best examples of this “ideal” geometry, since they develop as regular surface features due to the point-like (circular) or fissure-like (linear) manifestation of volcanic activity. In this paper, we present a geomorphometric method of fitting the “ideal” surface onto the real surface of regular-shaped volcanoes through a number of case studies (Mt. Mayon, Mt. Somma, Mt. Semeru, and Mt. Cameroon). Volcanoes with circular, as well as elliptical, symmetry are addressed. For the best surface fit, we use the minimization library MINUIT which is made freely available by the CERN (European Organization for Nuclear Research). This library enables us to handle all the available surface data (every point of the digital elevation model) in a one-step, half-automated way regardless of the size of the dataset, and to consider simultaneously all the relevant parameters of the selected problem, such as the position of the center of the edifice, apex height, and cone slope, thanks to the highly performing adopted procedure. Fitting the geometric surface, along with calculating the related error, demonstrates the twofold advantage of the method. Firstly, we can determine quantitatively to what extent a given volcanic landform is regular, i.e. how much it follows an expected regular shape. Deviations from the ideal shape due to degradation (e.g. sector collapse and normal erosion) can be used in erosion rate calculations. Secondly, if we have a degraded volcanic landform, whose geometry is not clear, this method of surface fitting reconstructs the original shape with the maximum precision. Obviously, in addition to volcanic landforms, this method is also capable of constraining the shapes of other regular surface features such as aeolian, glacial or periglacial landforms." @default.
• W2049703200 created "2016-06-24" @default.
• W2049703200 creator A5003702949 @default.
• W2049703200 creator A5035411717 @default.
• W2049703200 creator A5083080887 @default.
• W2049703200 creator A5090568460 @default.
• W2049703200 date "2014-09-01" @default.
• W2049703200 modified "2023-10-05" @default.
• W2049703200 title "Surface fitting in geomorphology — Examples for regular-shaped volcanic landforms" @default.
• W2049703200 cites W1579931904 @default.
• W2049703200 cites W1976600319 @default.
• W2049703200 cites W1985719062 @default.
• W2049703200 cites W1990590197 @default.
• W2049703200 cites W1992776973 @default.
• W2049703200 cites W1994794192 @default.
• W2049703200 cites W1995204553 @default.
• W2049703200 cites W2007265465 @default.
• W2049703200 cites W2012371198 @default.
• W2049703200 cites W2014101047 @default.
• W2049703200 cites W2046564461 @default.
• W2049703200 cites W2060455485 @default.
• W2049703200 cites W2067011246 @default.
• W2049703200 cites W2070007201 @default.
• W2049703200 cites W2082805876 @default.
• W2049703200 cites W2091125262 @default.
• W2049703200 cites W2091690770 @default.
• W2049703200 cites W2094430658 @default.
• W2049703200 cites W2095960346 @default.
• W2049703200 cites W2138823655 @default.
• W2049703200 cites W2139710065 @default.
• W2049703200 doi "https://doi.org/10.1016/j.geomorph.2014.06.009" @default.
• W2049703200 hasPublicationYear "2014" @default.
• W2049703200 type Work @default.
• W2049703200 sameAs 2049703200 @default.
• W2049703200 citedByCount "13" @default.
• W2049703200 countsByYear W20497032002015 @default.
• W2049703200 countsByYear W20497032002016 @default.
• W2049703200 countsByYear W20497032002017 @default.
• W2049703200 countsByYear W20497032002018 @default.
• W2049703200 countsByYear W20497032002020 @default.
• W2049703200 countsByYear W20497032002021 @default.
• W2049703200 countsByYear W20497032002023 @default.
• W2049703200 crossrefType "journal-article" @default.
• W2049703200 hasAuthorship W2049703200A5003702949 @default.
• W2049703200 hasAuthorship W2049703200A5035411717 @default.
• W2049703200 hasAuthorship W2049703200A5083080887 @default.
• W2049703200 hasAuthorship W2049703200A5090568460 @default.
• W2049703200 hasBestOaLocation W20497032002 @default.
• W2049703200 hasConcept C108497213 @default.
• W2049703200 hasConcept C114793014 @default.
• W2049703200 hasConcept C120806208 @default.
• W2049703200 hasConcept C127313418 @default.
• W2049703200 hasConcept C165205528 @default.
• W2049703200 hasConceptScore W2049703200C108497213 @default.
• W2049703200 hasConceptScore W2049703200C114793014 @default.
• W2049703200 hasConceptScore W2049703200C120806208 @default.
• W2049703200 hasConceptScore W2049703200C127313418 @default.
• W2049703200 hasConceptScore W2049703200C165205528 @default.
• W2049703200 hasLocation W20497032001 @default.
• W2049703200 hasLocation W20497032002 @default.
• W2049703200 hasLocation W20497032003 @default.
• W2049703200 hasOpenAccess W2049703200 @default.
• W2049703200 hasPrimaryLocation W20497032001 @default.
• W2049703200 hasRelatedWork W2007265465 @default.
• W2049703200 hasRelatedWork W2015299482 @default.
• W2049703200 hasRelatedWork W2088602912 @default.
• W2049703200 hasRelatedWork W2170616010 @default.
• W2049703200 hasRelatedWork W2365716639 @default.
• W2049703200 hasRelatedWork W2513821992 @default.
• W2049703200 hasRelatedWork W2808621182 @default.
• W2049703200 hasRelatedWork W2920958974 @default.
• W2049703200 hasRelatedWork W3138242835 @default.
• W2049703200 hasRelatedWork W4289262165 @default.
• W2049703200 hasVolume "221" @default.
• W2049703200 isParatext "false" @default.
• W2049703200 isRetracted "false" @default.
• W2049703200 magId "2049703200" @default.
• W2049703200 workType "article" @default.