FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2064051203> ?p ?o ?g. }

• W2064051203 abstract "Abstract This paper is inspired by the proposition that it may be possible to extract descriptive physical parameters – in particular the ice thickness, of a sea-ice field from ocean wave information. The motivation is that mathematical theory describing wave propagation in such media has reached a point where the inherent heterogeneity, expressed as pressure ridge keels and sails, leads, thickness variations and changes of material property and draught, can be fully assimilated exactly or through approximations whose limitations are understood. On the basis that leads have the major wave scattering effect for most sea-ice [Williams, T.D., Squire, V.A., 2004. Oblique scattering of plane flexural-gravity waves by heterogeneities in sea ice. Proc. R. Soc. Lon. Ser.-A 460 (2052), 3469–3497], a model two dimensional sea-ice sheet composed of a large number of such features, randomly dispersed, is constructed. The wide spacing approximation is used to predict how wave trains of different period will be affected, after first establishing that this produces results that are very close to the exact solution. Like Kohout and Meylan [Kohout, A.L., Meylan, M.H., 2008. An elastic plate model for wave attenuation and ice floe breaking in the marginal ice zone. J. Geophys. Res. 113, C09016, doi:10.1029/2007JC004434 ], we find that on average the magnitude of a wave transmitted by a field of leads decays exponentially with the number of leads. Then, by fitting a curve based on this assumption to the data, the thickness of the ice sheet is obtained. The attenuation coefficient can always be calculated numerically by ensemble averaging but in some cases more rapidly computed approximations work extremely well. Moreover, it is found that the underlying thickness can be determined to good accuracy by the method as long as Archimedean draught is correctly provided for, suggesting that waves can indeed be effective as a remote sensing agent to measure ice thickness in areas where pressure ridges are not sizeable, i.e. away from coastal regions of high deformation." @default.
• W2064051203 created "2016-06-24" @default.
• W2064051203 creator A5025300065 @default.
• W2064051203 creator A5073317333 @default.
• W2064051203 date "2010-04-01" @default.
• W2064051203 modified "2023-09-26" @default.
• W2064051203 title "On the estimation of ice thickness from scattering observations" @default.
• W2064051203 cites W1590838666 @default.
• W2064051203 cites W1985238098 @default.
• W2064051203 cites W1992336588 @default.
• W2064051203 cites W2003032917 @default.
• W2064051203 cites W2014447896 @default.
• W2064051203 cites W2016792977 @default.
• W2064051203 cites W2027741020 @default.
• W2064051203 cites W2028443461 @default.
• W2064051203 cites W2032349099 @default.
• W2064051203 cites W2045312330 @default.
• W2064051203 cites W2060679957 @default.
• W2064051203 cites W2074954029 @default.
• W2064051203 cites W2083439512 @default.
• W2064051203 cites W2096950324 @default.
• W2064051203 cites W2123117722 @default.
• W2064051203 cites W2125121410 @default.
• W2064051203 cites W2127258275 @default.
• W2064051203 cites W2129492805 @default.
• W2064051203 cites W2136890000 @default.
• W2064051203 cites W2162739620 @default.
• W2064051203 cites W2167174042 @default.
• W2064051203 cites W4213054309 @default.
• W2064051203 doi "https://doi.org/10.1016/j.dynatmoce.2009.08.001" @default.
• W2064051203 hasPublicationYear "2010" @default.
• W2064051203 type Work @default.
• W2064051203 sameAs 2064051203 @default.
• W2064051203 citedByCount "9" @default.
• W2064051203 countsByYear W20640512032012 @default.
• W2064051203 countsByYear W20640512032013 @default.
• W2064051203 countsByYear W20640512032015 @default.
• W2064051203 countsByYear W20640512032016 @default.
• W2064051203 countsByYear W20640512032020 @default.
• W2064051203 crossrefType "journal-article" @default.
• W2064051203 hasAuthorship W2064051203A5025300065 @default.
• W2064051203 hasAuthorship W2064051203A5073317333 @default.
• W2064051203 hasConcept C114793014 @default.
• W2064051203 hasConcept C120665830 @default.
• W2064051203 hasConcept C121332964 @default.
• W2064051203 hasConcept C123750103 @default.
• W2064051203 hasConcept C127313418 @default.
• W2064051203 hasConcept C13280743 @default.
• W2064051203 hasConcept C136894858 @default.
• W2064051203 hasConcept C151730666 @default.
• W2064051203 hasConcept C161798024 @default.
• W2064051203 hasConcept C165205528 @default.
• W2064051203 hasConcept C1721004 @default.
• W2064051203 hasConcept C184652730 @default.
• W2064051203 hasConcept C191486275 @default.
• W2064051203 hasConcept C196735533 @default.
• W2064051203 hasConcept C2992272396 @default.
• W2064051203 hasConcept C32277403 @default.
• W2064051203 hasConcept C49204034 @default.
• W2064051203 hasConcept C57879066 @default.
• W2064051203 hasConcept C8058405 @default.
• W2064051203 hasConceptScore W2064051203C114793014 @default.
• W2064051203 hasConceptScore W2064051203C120665830 @default.
• W2064051203 hasConceptScore W2064051203C121332964 @default.
• W2064051203 hasConceptScore W2064051203C123750103 @default.
• W2064051203 hasConceptScore W2064051203C127313418 @default.
• W2064051203 hasConceptScore W2064051203C13280743 @default.
• W2064051203 hasConceptScore W2064051203C136894858 @default.
• W2064051203 hasConceptScore W2064051203C151730666 @default.
• W2064051203 hasConceptScore W2064051203C161798024 @default.
• W2064051203 hasConceptScore W2064051203C165205528 @default.
• W2064051203 hasConceptScore W2064051203C1721004 @default.
• W2064051203 hasConceptScore W2064051203C184652730 @default.
• W2064051203 hasConceptScore W2064051203C191486275 @default.
• W2064051203 hasConceptScore W2064051203C196735533 @default.
• W2064051203 hasConceptScore W2064051203C2992272396 @default.
• W2064051203 hasConceptScore W2064051203C32277403 @default.
• W2064051203 hasConceptScore W2064051203C49204034 @default.
• W2064051203 hasConceptScore W2064051203C57879066 @default.
• W2064051203 hasConceptScore W2064051203C8058405 @default.
• W2064051203 hasLocation W20640512031 @default.
• W2064051203 hasOpenAccess W2064051203 @default.
• W2064051203 hasPrimaryLocation W20640512031 @default.
• W2064051203 hasRelatedWork W1982370176 @default.
• W2064051203 hasRelatedWork W2002982027 @default.
• W2064051203 hasRelatedWork W2018287612 @default.
• W2064051203 hasRelatedWork W2024198799 @default.
• W2064051203 hasRelatedWork W2027741020 @default.
• W2064051203 hasRelatedWork W2032349099 @default.
• W2064051203 hasRelatedWork W2050046917 @default.
• W2064051203 hasRelatedWork W2060679957 @default.
• W2064051203 hasRelatedWork W2061305469 @default.
• W2064051203 hasRelatedWork W2062918007 @default.
• W2064051203 hasRelatedWork W2097701259 @default.
• W2064051203 hasRelatedWork W2135773240 @default.
• W2064051203 hasRelatedWork W2139300251 @default.
• W2064051203 hasRelatedWork W2167174042 @default.
• W2064051203 hasRelatedWork W2266862918 @default.
• W2064051203 hasRelatedWork W2409546036 @default.
• W2064051203 hasRelatedWork W2504936160 @default.

• next