FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4387174561> ?p ?o ?g. }

• W4387174561 abstract "Abstract All realizations of the European Vertical Reference System (EVRS) computed so far are solely based on geopotential differences obtained by spirit leveling/gravimetry. As such, there are no direct connections between height benchmarks separated by large water bodies. In this study, such connections are added by means of model-based hydrodynamic leveling resulting in a new, yet unofficial realization of the EVRS. The model-derived mean water levels used in computing the hydrodynamic leveling connections were obtained from the Nemo-Nordic (Baltic Sea) and 3D DCSM-FM (northwest European continental shelf) hydrodynamic models. The impact of model-based hydrodynamic leveling on the European Vertical Reference Frame is significant, especially for France and Great Britain. Compared to a solution which only uses spirit leveling/gravimetry, the differences in these countries reach tens to hundreds of $$hbox {kgal}, hbox {mm}$$ <mml:math xmlns:mml=http://www.w3.org/1998/Math/MathML> <mml:mrow> <mml:mtext>kgal</mml:mtext> <mml:mspace /> <mml:mtext>mm</mml:mtext> </mml:mrow> </mml:math> . We also observed an improved agreement with normal heights obtained by differencing GNSS and the European gravimetric quasi-geoid 2015 (EGG2015) heights. In Great Britain, the south-north slope of 48 mm $$hbox {deg}^{-1}$$ <mml:math xmlns:mml=http://www.w3.org/1998/Math/MathML> <mml:msup> <mml:mtext>deg</mml:mtext> <mml:mrow> <mml:mo>-</mml:mo> <mml:mn>1</mml:mn> </mml:mrow> </mml:msup> </mml:math> present in the solution which uses only spirit leveling/gravimetry data reduced to 2.2 mm $$hbox {deg}^{-1}$$ <mml:math xmlns:mml=http://www.w3.org/1998/Math/MathML> <mml:msup> <mml:mtext>deg</mml:mtext> <mml:mrow> <mml:mo>-</mml:mo> <mml:mn>1</mml:mn> </mml:mrow> </mml:msup> </mml:math> . In France, the improvement is confined to the southwest. The choice of the period over which water levels are averaged has an impact on the results as it determines, among others, the set of tide gauges available to establish the hydrodynamic leveling connections. When using an averaging period that can be considered as the least preferred choice based on three established criteria, the positive impact for France has gone. For Great Britain, the estimated south-north slope became 12.6 mm $$hbox {deg}^{-1}$$ <mml:math xmlns:mml=http://www.w3.org/1998/Math/MathML> <mml:msup> <mml:mtext>deg</mml:mtext> <mml:mrow> <mml:mo>-</mml:mo> <mml:mn>1</mml:mn> </mml:mrow> </mml:msup> </mml:math> . This is larger than the slope obtained using the most preferred averaging period but still substantially lower compared to the slope associated with a solution that uses only spirit leveling/gravimetry." @default.
• W4387174561 created "2023-09-30" @default.
• W4387174561 creator A5000057095 @default.
• W4387174561 creator A5015414614 @default.
• W4387174561 creator A5019040325 @default.
• W4387174561 creator A5032097709 @default.
• W4387174561 creator A5047878082 @default.
• W4387174561 creator A5049618415 @default.
• W4387174561 creator A5058855742 @default.
• W4387174561 creator A5075314052 @default.
• W4387174561 creator A5083084191 @default.
• W4387174561 creator A5088804274 @default.
• W4387174561 creator A5090340603 @default.
• W4387174561 date "2023-09-29" @default.
• W4387174561 modified "2023-10-14" @default.
• W4387174561 title "Realizing the European Vertical Reference System using model-based hydrodynamic leveling data" @default.
• W4387174561 cites W1518006631 @default.
• W4387174561 cites W1897592127 @default.
• W4387174561 cites W1941421521 @default.
• W4387174561 cites W1969082886 @default.
• W4387174561 cites W1972452461 @default.
• W4387174561 cites W1979262708 @default.
• W4387174561 cites W1982387893 @default.
• W4387174561 cites W2005963587 @default.
• W4387174561 cites W2010405336 @default.
• W4387174561 cites W2025648334 @default.
• W4387174561 cites W2051600602 @default.
• W4387174561 cites W2071056414 @default.
• W4387174561 cites W2080421315 @default.
• W4387174561 cites W2088693790 @default.
• W4387174561 cites W2132320923 @default.
• W4387174561 cites W2294779277 @default.
• W4387174561 cites W244365331 @default.
• W4387174561 cites W2773728726 @default.
• W4387174561 cites W2789296345 @default.
• W4387174561 cites W2795908029 @default.
• W4387174561 cites W2903131677 @default.
• W4387174561 cites W2921833674 @default.
• W4387174561 cites W2964212651 @default.
• W4387174561 cites W3146988707 @default.
• W4387174561 cites W3186042752 @default.
• W4387174561 cites W4229530126 @default.
• W4387174561 cites W4232368692 @default.
• W4387174561 cites W42354747 @default.
• W4387174561 cites W4297310844 @default.
• W4387174561 cites W4312163430 @default.
• W4387174561 cites W4362131110 @default.
• W4387174561 doi "https://doi.org/10.1007/s00190-023-01778-2" @default.
• W4387174561 hasPublicationYear "2023" @default.
• W4387174561 type Work @default.
• W4387174561 citedByCount "0" @default.
• W4387174561 crossrefType "journal-article" @default.
• W4387174561 hasAuthorship W4387174561A5000057095 @default.
• W4387174561 hasAuthorship W4387174561A5015414614 @default.
• W4387174561 hasAuthorship W4387174561A5019040325 @default.
• W4387174561 hasAuthorship W4387174561A5032097709 @default.
• W4387174561 hasAuthorship W4387174561A5047878082 @default.
• W4387174561 hasAuthorship W4387174561A5049618415 @default.
• W4387174561 hasAuthorship W4387174561A5058855742 @default.
• W4387174561 hasAuthorship W4387174561A5075314052 @default.
• W4387174561 hasAuthorship W4387174561A5083084191 @default.
• W4387174561 hasAuthorship W4387174561A5088804274 @default.
• W4387174561 hasAuthorship W4387174561A5090340603 @default.
• W4387174561 hasBestOaLocation W43871745611 @default.
• W4387174561 hasConcept C11413529 @default.
• W4387174561 hasConcept C127313418 @default.
• W4387174561 hasConcept C13280743 @default.
• W4387174561 hasConcept C14279187 @default.
• W4387174561 hasConcept C14641988 @default.
• W4387174561 hasConcept C160121416 @default.
• W4387174561 hasConcept C187320778 @default.
• W4387174561 hasConcept C202453963 @default.
• W4387174561 hasConcept C2524010 @default.
• W4387174561 hasConcept C33923547 @default.
• W4387174561 hasConcept C41008148 @default.
• W4387174561 hasConcept C60229501 @default.
• W4387174561 hasConcept C76155785 @default.
• W4387174561 hasConceptScore W4387174561C11413529 @default.
• W4387174561 hasConceptScore W4387174561C127313418 @default.
• W4387174561 hasConceptScore W4387174561C13280743 @default.
• W4387174561 hasConceptScore W4387174561C14279187 @default.
• W4387174561 hasConceptScore W4387174561C14641988 @default.
• W4387174561 hasConceptScore W4387174561C160121416 @default.
• W4387174561 hasConceptScore W4387174561C187320778 @default.
• W4387174561 hasConceptScore W4387174561C202453963 @default.
• W4387174561 hasConceptScore W4387174561C2524010 @default.
• W4387174561 hasConceptScore W4387174561C33923547 @default.
• W4387174561 hasConceptScore W4387174561C41008148 @default.
• W4387174561 hasConceptScore W4387174561C60229501 @default.
• W4387174561 hasConceptScore W4387174561C76155785 @default.
• W4387174561 hasFunder F4320328233 @default.
• W4387174561 hasIssue "10" @default.
• W4387174561 hasLocation W43871745611 @default.
• W4387174561 hasOpenAccess W4387174561 @default.
• W4387174561 hasPrimaryLocation W43871745611 @default.
• W4387174561 hasRelatedWork W2044519784 @default.
• W4387174561 hasRelatedWork W2394560506 @default.
• W4387174561 hasRelatedWork W2992634337 @default.
• W4387174561 hasRelatedWork W3006016047 @default.
• W4387174561 hasRelatedWork W3013151100 @default.

• next