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Reassessment of 20th century global mean sea level rise
TLDR
A 20th-century GMSL reconstruction computed using an area-weighting technique for averaging tide gauge records that both incorporates up-to-date observations of vertical land motion (VLM) and corrections for local geoid changes resulting from ice melting and terrestrial freshwater storage and allows for the identification of possible differences compared with earlier attempts is presented.
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Correlated errors in GPS position time series: Implications for velocity estimates
[1] This study focuses on the effects of time correlation in weekly GPS position time series on velocity estimates. Time series 2.5 to 13 years long from a homogeneously reprocessed solution of 275…
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Geocentric sea-level trend estimates from GPS analyses at relevant tide gauges world-wide
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Coastal sea level rise in southern Europe and the nonclimate contribution of vertical land motion
[1] In this study, we extend the advanced approach of combining tide gauge and satellite altimetry data with supplemental equations from adjacent tide gauge records of at least 30 years of common…
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Vertical land motion as a key to understanding sea level change and variability
Vertical land motions are a key element in understanding how sea levels have changed over the past century and how future sea levels may impact coastal areas. Ideally, to be useful in long‐term sea…
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Observed mean sea level changes around the North Sea coastline from 1800 to present
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Rates of sea‐level change over the past century in a geocentric reference frame
The results from a carefully implemented GPS analysis, using a strategy adapted to determine accurate vertical station velocities, are presented. The stochastic properties of our globally distributed…
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Land motion estimates from GPS at tide gauges: a geophysical evaluation
SUMMARY Space geodesy applications have mainly been limited to horizontal deformations due to a number of restrictions on the vertical component accuracy. Monitoring vertical land motion is…
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Global sea-level budget 1993–present
Abstract. Global mean sea level is an integral of changes occurring in the climate system in response to unforced climate variability as well as natural and anthropogenic forcing factors. Its…
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Uncertainty of the 20th century sea-level rise due to vertical land motion errors
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