FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3106281650> ?p ?o ?g. }

• W3106281650 endingPage "592" @default.
• W3106281650 startingPage "571" @default.
• W3106281650 abstract "A significant part of the World population lives in the coastal zone, which is affected by sea level rise and extreme events. Consistent and precise new measurements are needed to assess and predict these changes. New altimeter missions equipped with Synthetic Aperture Radar (SAR) mode provide more accurate sea level heights. In this work we analyse their impacts on the estimation of the coastal sea level variability in the last 10 km. First, by analysing various standard and improved SAR altimetric products it is found that SAR altimetry will reduce the minimum usable distance from five to three kilometres. The best performance is achieved with the SAR coastal retrackers SAMOSA+ and SAMOSA++. A comparable performance is obtained in low resolution Reduced SAR (RDSAR) mode with the Spatio-Temporal Altimeter sub-waveform Retracker (STAR). In both cases, sea level heights are recovered with 4 cm accuracy up to 3 km from the coast at the Helgoland station, and the accuracy does not decrease with the distance to coast. In estuaries and coastal zones with hight tidal regimes, the discrepancy between altimetry and in-situ observations remains large (40 cm standard deviation difference (stdd) with SAR-SAM+). CryoSat-2 and Sentinel-3A have similar accuracy, despite their different repeat cycle and sampling, which require a different post-processing. The monthly coastal variability from the SAR-SAM+ product agrees most favourably with the NEMO-WAM model, with stdd 3.9 and correlation 0.90 for Sentinel-3A. Instead, the maximum departure between altimeter data products is between SAR-SAM+ and RDSAR-TALES CryoSat-2 data (stdd 2.3 and correlation 0.96). An average trend of about 3 ± 1.3 mm/yr has been detected using low resolution altimetry at ninetheen in-situ stations along the German coast over time intervals longer than 15 years. The difference of the trends of altimetry and tide gauge co-located time-series (al-tg) agrees with the GNSS rates within 1.5 mm/yr at half of the co-located locations, with error of al-tg larger than the error of the GPS rate by a factor bigger than two. The larger departure between monthly tide gauge and LRM altimetric time-series as between tide gauge and SAR altimetric time-series confirms the higher accuracy of SAR data compared to LRM. Finally, the sea level trends of the merged LRM and SAR altimetry time-series are consistent with the LRM trends." @default.
• W3106281650 created "2020-11-23" @default.
• W3106281650 creator A5005562421 @default.
• W3106281650 creator A5020174086 @default.
• W3106281650 creator A5030825955 @default.
• W3106281650 creator A5045027342 @default.
• W3106281650 creator A5047444625 @default.
• W3106281650 creator A5047897130 @default.
• W3106281650 creator A5060111105 @default.
• W3106281650 creator A5065548421 @default.
• W3106281650 creator A5078411691 @default.
• W3106281650 date "2021-07-01" @default.
• W3106281650 modified "2023-10-17" @default.
• W3106281650 title "Advances in NE-Atlantic coastal sea level change monitoring by Delay Doppler altimetry" @default.
• W3106281650 cites W1519949070 @default.
• W3106281650 cites W1674810995 @default.
• W3106281650 cites W1964087794 @default.
• W3106281650 cites W1997722977 @default.
• W3106281650 cites W2002177889 @default.
• W3106281650 cites W2003647508 @default.
• W3106281650 cites W2035109608 @default.
• W3106281650 cites W2044897744 @default.
• W3106281650 cites W2060803307 @default.
• W3106281650 cites W2095408490 @default.
• W3106281650 cites W2100914798 @default.
• W3106281650 cites W2132707066 @default.
• W3106281650 cites W2138331294 @default.
• W3106281650 cites W2170892247 @default.
• W3106281650 cites W2173246082 @default.
• W3106281650 cites W2260016662 @default.
• W3106281650 cites W2264193409 @default.
• W3106281650 cites W2291883352 @default.
• W3106281650 cites W2327709234 @default.
• W3106281650 cites W2344848504 @default.
• W3106281650 cites W2416122685 @default.
• W3106281650 cites W2470210584 @default.
• W3106281650 cites W2525711383 @default.
• W3106281650 cites W2528733679 @default.
• W3106281650 cites W2534397751 @default.
• W3106281650 cites W2556055732 @default.
• W3106281650 cites W2556164768 @default.
• W3106281650 cites W2579961960 @default.
• W3106281650 cites W2743144386 @default.
• W3106281650 cites W2765477394 @default.
• W3106281650 cites W2767072558 @default.
• W3106281650 cites W2771817195 @default.
• W3106281650 cites W2784068515 @default.
• W3106281650 cites W2793784625 @default.
• W3106281650 cites W2810491782 @default.
• W3106281650 cites W2893726365 @default.
• W3106281650 cites W2901116844 @default.
• W3106281650 cites W2906579918 @default.
• W3106281650 cites W2906963687 @default.
• W3106281650 cites W2913983560 @default.
• W3106281650 cites W2944017778 @default.
• W3106281650 cites W2945512274 @default.
• W3106281650 cites W2950599353 @default.
• W3106281650 cites W2954089295 @default.
• W3106281650 cites W2955302084 @default.
• W3106281650 cites W2963526966 @default.
• W3106281650 cites W2964171917 @default.
• W3106281650 cites W2972486713 @default.
• W3106281650 cites W3004154727 @default.
• W3106281650 cites W3011385638 @default.
• W3106281650 cites W3036870042 @default.
• W3106281650 cites W3082030783 @default.
• W3106281650 cites W4230338416 @default.
• W3106281650 doi "https://doi.org/10.1016/j.asr.2020.10.041" @default.
• W3106281650 hasPublicationYear "2021" @default.
• W3106281650 type Work @default.
• W3106281650 sameAs 3106281650 @default.
• W3106281650 citedByCount "8" @default.
• W3106281650 countsByYear W31062816502021 @default.
• W3106281650 countsByYear W31062816502022 @default.
• W3106281650 countsByYear W31062816502023 @default.
• W3106281650 crossrefType "journal-article" @default.
• W3106281650 hasAuthorship W3106281650A5005562421 @default.
• W3106281650 hasAuthorship W3106281650A5020174086 @default.
• W3106281650 hasAuthorship W3106281650A5030825955 @default.
• W3106281650 hasAuthorship W3106281650A5045027342 @default.
• W3106281650 hasAuthorship W3106281650A5047444625 @default.
• W3106281650 hasAuthorship W3106281650A5047897130 @default.
• W3106281650 hasAuthorship W3106281650A5060111105 @default.
• W3106281650 hasAuthorship W3106281650A5065548421 @default.
• W3106281650 hasAuthorship W3106281650A5078411691 @default.
• W3106281650 hasBestOaLocation W31062816501 @default.
• W3106281650 hasConcept C105795698 @default.
• W3106281650 hasConcept C111368507 @default.
• W3106281650 hasConcept C111919701 @default.
• W3106281650 hasConcept C127313418 @default.
• W3106281650 hasConcept C13280743 @default.
• W3106281650 hasConcept C142672198 @default.
• W3106281650 hasConcept C153294291 @default.
• W3106281650 hasConcept C165082838 @default.
• W3106281650 hasConcept C17534553 @default.
• W3106281650 hasConcept C205649164 @default.
• W3106281650 hasConcept C22679943 @default.
• W3106281650 hasConcept C33923547 @default.

• next