Matches in SemOpenAlex for { <https://semopenalex.org/work/W2094298006> ?p ?o ?g. }
Showing items 1 to 90 of
90
with 100 items per page.
- W2094298006 endingPage "1283" @default.
- W2094298006 startingPage "1275" @default.
- W2094298006 abstract "Application of forward coastal sediment transport models in situations involving large temporal and spatial scales or topographically complex environments can be highly problematic since the distribution of hydrodynamic parameters is rarely adequately known. Where rocky topography is present, flow patterns may be altered and sediments trapped by topographic barriers. A frequently employed approach to these problems is the application of the statistical technique known as empirical orthogonal function (EOF) analysis. One limitation of EOF analysis of grain size and mineralogical data is that EOF is a purely geometric technique which does not allow incorporation of a priori knowledge we may have regarding the physical environment. In fact, there is no guarantee that a meaningful physical interpretation of the results of an EOF analysis actually exists. This is not true of geophysical inverse theory, which is capable of incorporating diverse forms of information and is not limited to purely geometric manipulations of data. We have formulated an inverse theoretical approach to study sediment transport which we call STI, short for source‐transport inversion. STI relaxes the nonphysical assumption of orthogonal endmembers and can handle many forms of a priori information. STI has been developed initially in the context of modeling the sediment supply and dispersal system of Monterey Bay, California. Using the geographical distribution of heavy mineralogy data, significant sources are identified and sediments traced from those sources along transport pathways. Model results are encouraging both in terms of goodness of fit between model and data and in terms of the agreement of model results with the sediment sourcing and dispersal patterns inferred in previous studies. Model results indicate that beach sediments are primarily derived from the open coast north of the bay, that a littoral cell boundary exists in the center of the bay at Moss Landing, and that beach deposits produced by paleolittoral drift during a sea level low stand lie along the 100‐m isobath." @default.
- W2094298006 created "2016-06-24" @default.
- W2094298006 creator A5026138848 @default.
- W2094298006 creator A5078230536 @default.
- W2094298006 date "1998-01-15" @default.
- W2094298006 modified "2023-09-27" @default.
- W2094298006 title "Source-transport inversion: An application of geophysical inverse theory to sediment transport in Monterey Bay, California" @default.
- W2094298006 cites W1989829506 @default.
- W2094298006 cites W1991055868 @default.
- W2094298006 cites W1997665642 @default.
- W2094298006 cites W1997741996 @default.
- W2094298006 cites W2006673484 @default.
- W2094298006 cites W2014124878 @default.
- W2094298006 cites W2015235516 @default.
- W2094298006 cites W2020354634 @default.
- W2094298006 cites W2025876705 @default.
- W2094298006 cites W2027182567 @default.
- W2094298006 cites W2029744035 @default.
- W2094298006 cites W2032327404 @default.
- W2094298006 cites W2039512128 @default.
- W2094298006 cites W2039949021 @default.
- W2094298006 cites W2044735051 @default.
- W2094298006 cites W2050013294 @default.
- W2094298006 cites W2053737950 @default.
- W2094298006 cites W2077361469 @default.
- W2094298006 cites W2123460718 @default.
- W2094298006 cites W2155539309 @default.
- W2094298006 cites W2159525271 @default.
- W2094298006 cites W2161279701 @default.
- W2094298006 cites W4214541643 @default.
- W2094298006 cites W4236218376 @default.
- W2094298006 doi "https://doi.org/10.1029/97jc01909" @default.
- W2094298006 hasPublicationYear "1998" @default.
- W2094298006 type Work @default.
- W2094298006 sameAs 2094298006 @default.
- W2094298006 citedByCount "8" @default.
- W2094298006 countsByYear W20942980062012 @default.
- W2094298006 countsByYear W20942980062013 @default.
- W2094298006 crossrefType "journal-article" @default.
- W2094298006 hasAuthorship W2094298006A5026138848 @default.
- W2094298006 hasAuthorship W2094298006A5078230536 @default.
- W2094298006 hasConcept C109007969 @default.
- W2094298006 hasConcept C111472728 @default.
- W2094298006 hasConcept C114793014 @default.
- W2094298006 hasConcept C127313418 @default.
- W2094298006 hasConcept C13724139 @default.
- W2094298006 hasConcept C138885662 @default.
- W2094298006 hasConcept C151730666 @default.
- W2094298006 hasConcept C1893757 @default.
- W2094298006 hasConcept C2779343474 @default.
- W2094298006 hasConcept C2816523 @default.
- W2094298006 hasConcept C49204034 @default.
- W2094298006 hasConcept C65589250 @default.
- W2094298006 hasConcept C75553542 @default.
- W2094298006 hasConcept C8058405 @default.
- W2094298006 hasConceptScore W2094298006C109007969 @default.
- W2094298006 hasConceptScore W2094298006C111472728 @default.
- W2094298006 hasConceptScore W2094298006C114793014 @default.
- W2094298006 hasConceptScore W2094298006C127313418 @default.
- W2094298006 hasConceptScore W2094298006C13724139 @default.
- W2094298006 hasConceptScore W2094298006C138885662 @default.
- W2094298006 hasConceptScore W2094298006C151730666 @default.
- W2094298006 hasConceptScore W2094298006C1893757 @default.
- W2094298006 hasConceptScore W2094298006C2779343474 @default.
- W2094298006 hasConceptScore W2094298006C2816523 @default.
- W2094298006 hasConceptScore W2094298006C49204034 @default.
- W2094298006 hasConceptScore W2094298006C65589250 @default.
- W2094298006 hasConceptScore W2094298006C75553542 @default.
- W2094298006 hasConceptScore W2094298006C8058405 @default.
- W2094298006 hasIssue "C1" @default.
- W2094298006 hasLocation W20942980061 @default.
- W2094298006 hasOpenAccess W2094298006 @default.
- W2094298006 hasPrimaryLocation W20942980061 @default.
- W2094298006 hasRelatedWork W1614580964 @default.
- W2094298006 hasRelatedWork W1966483575 @default.
- W2094298006 hasRelatedWork W1996370225 @default.
- W2094298006 hasRelatedWork W2053034080 @default.
- W2094298006 hasRelatedWork W2062428779 @default.
- W2094298006 hasRelatedWork W2096599809 @default.
- W2094298006 hasRelatedWork W2171475701 @default.
- W2094298006 hasRelatedWork W2320366314 @default.
- W2094298006 hasRelatedWork W2369413902 @default.
- W2094298006 hasRelatedWork W2097975749 @default.
- W2094298006 hasVolume "103" @default.
- W2094298006 isParatext "false" @default.
- W2094298006 isRetracted "false" @default.
- W2094298006 magId "2094298006" @default.
- W2094298006 workType "article" @default.