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- W2240584295 abstract "Sea level, the height of the ocean surface at any given location, is de�nedeither with respect to the surface of the solid Earth (relative sea level) or toa geocentric reference such as the reference ellipsoid. The former is the morerelevant quantity when considering the coastal impacts of sea level change.Relative sea level has been measured using tide gauges during the past fewcenturies and estimated for longer time spans from geological records, whilegeocentric sea level has been observed over the past two decades only usingsatellite altimetry.Changes in sea level represent an integration of many aspects of climatechange, and thus occur over a broad range of temporal and spatial scales.Many processes contribute to sea level variability and change, being associatedwith changes in the ocean, changes in the atmosphere and changes in thesolid Earth. Understanding these processes better requires a consistent andhomogeneous data base of measured sea level. It is thus a viable objective toreconstruct past sea levels by combining the long, but relatively sparse, timeseries of tide gauge observations with the shorter, but spatially dense, dataset from altimetry and/or data-assimilated ocean models. Solving this problemessentially represents an extrapolation problem. A number of methodshas been developed to this end in the past, typically based on extractingdominating patterns of sea level from the altimetry era in a �rst step." @default.
- W2240584295 created "2016-06-24" @default.
- W2240584295 creator A5078650975 @default.
- W2240584295 date "2014-01-01" @default.
- W2240584295 modified "2023-09-24" @default.
- W2240584295 title "Reconstrucing historic sea levels from tide gauges using EOF-techniques" @default.
- W2240584295 hasPublicationYear "2014" @default.
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