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Coastal sea level rise in southern Europe and the nonclimate contribution of vertical land motion

Identifieur interne : 000040 ( Main/Exploration ); précédent : 000039; suivant : 000041

Coastal sea level rise in southern Europe and the nonclimate contribution of vertical land motion

Auteurs : G. Wöppelmann [France] ; M. Marcos [Espagne]

Source :

RBID : ISTEX:11D21D56AFA75C7F531884373F19138E9C516A84

Descripteurs français

English descriptors

Abstract

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 data to investigate the relative importance of the nonclimate contribution of vertical land movement to the observed rates of sea level change along the coasts of southern Europe. The sensitivity tests proved that the advanced approach is robust and accurate at the submillimeter per year level of around 0.4 mm yr−1in estimating rates of vertical land movements. It enabled identifying stations displaying large rates of vertical land movements that must be taken into account when predicting future sea level rise and appraising the exposure to its impacts on populations and assets. The average rate of coastal climate‐related sea level rise in the Mediterranean Sea was consequently revisited to be of 1.7 mm yr−1 over the past century, whereas the Atlantic northern Iberian coast revealed a significant high rate of sea level rise in excess of 3.4 mm yr−1 for the past 70 years. Future work should consider applying this powerful approach to other geographic contexts as a useful source of supplementary data for geodynamic studies.
Advanced approach of combining tide gauge and satellite altimetry data Importance of nonclimate contributions to observed sea level rise at the coast Coherent spatial patterns of sea level rise along the European coasts inferred

Url:
DOI: 10.1029/2011JC007469


Affiliations:


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<term>Altimetric period</term>
<term>Altimetry</term>
<term>Altimetry data</term>
<term>Atlantic iberian coast</term>
<term>Atlantic stations</term>
<term>Atmospheric contribution</term>
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<term>Constraint</term>
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<term>Constraint equations</term>
<term>Contemporary tide gauge records</term>
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<term>Geoid change</term>
<term>Geoid rate term</term>
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<term>Global planet</term>
<term>Great lakes</term>
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<term>Level rise projections</term>
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<term>Martin miguez</term>
<term>Matrix form</term>
<term>Mediterranean</term>
<term>Mediterranean basin</term>
<term>Mediterranean region</term>
<term>Mediterranean stations</term>
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<term>Nonclimate contribution</term>
<term>Northern coast</term>
<term>Northern greece</term>
<term>Novel approach</term>
<term>Ocean model</term>
<term>Open oceanic conditions</term>
<term>Other hand</term>
<term>Permanent service</term>
<term>Position time series</term>
<term>Present study</term>
<term>Previous estimates</term>
<term>Previous studies</term>
<term>Psmsl</term>
<term>Relative importance</term>
<term>Rigorous comparison</term>
<term>Rovinj</term>
<term>Rudimentary comparison</term>
<term>Same models</term>
<term>Satellite</term>
<term>Satellite altimetry</term>
<term>Satellite altimetry data</term>
<term>Satellite altimetry time series</term>
<term>Seasonal signals</term>
<term>Second option</term>
<term>Selen</term>
<term>Selen model</term>
<term>Sensitivity tests</term>
<term>Southern europe</term>
<term>Southern european coasts</term>
<term>Spurious signals</term>
<term>Standard deviation</term>
<term>Standard error</term>
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<term>Supplementary data</term>
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<term>Useful source</term>
<term>Valid data</term>
<term>Variables exhibit</term>
<term>Various approaches</term>
<term>Venezia</term>
<term>Vertical crustal motion</term>
<term>Vertical land motion</term>
<term>Vertical land movement</term>
<term>Vertical land movement estimates</term>
<term>Vertical land movements</term>
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<term>Alternative approach</term>
<term>Altimetric period</term>
<term>Altimetry</term>
<term>Altimetry data</term>
<term>Atlantic iberian coast</term>
<term>Atlantic stations</term>
<term>Atmospheric contribution</term>
<term>Atmospheric correction</term>
<term>Average rate</term>
<term>Benchmark</term>
<term>Cascais</term>
<term>Case study</term>
<term>Cazenave</term>
<term>Central mediterranean</term>
<term>Classical approach</term>
<term>Climate change</term>
<term>Climate contributions</term>
<term>Closest grid point</term>
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<term>Common period</term>
<term>Confidence level</term>
<term>Constraint</term>
<term>Constraint equation</term>
<term>Constraint equations</term>
<term>Contemporary tide gauge records</term>
<term>Correlated grid point</term>
<term>Correlation coefficients</term>
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<term>Crustal displacement term</term>
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<term>Dubrovnik</term>
<term>Error bars</term>
<term>First option</term>
<term>Formal error bars</term>
<term>Future work</term>
<term>Gauge</term>
<term>General agreement</term>
<term>Geocentric</term>
<term>Geocentric satellite altimetry data cazenave</term>
<term>Geographic variability</term>
<term>Geoid change</term>
<term>Geoid rate term</term>
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<term>Global planet</term>
<term>Great lakes</term>
<term>Grid</term>
<term>High performance</term>
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<term>Iberian coast</term>
<term>Iberian coasts</term>
<term>Iberian peninsula</term>
<term>Inherent assumption</term>
<term>Intergovernmental panel</term>
<term>Lagrange multipliers</term>
<term>Land movement</term>
<term>Land movements</term>
<term>Land subsidence</term>
<term>Land uplift</term>
<term>Leros</term>
<term>Lett</term>
<term>Level change</term>
<term>Level changes</term>
<term>Level data</term>
<term>Level impacts</term>
<term>Level rise</term>
<term>Level rise projections</term>
<term>Level studies</term>
<term>Level trend</term>
<term>Level trends</term>
<term>Level variations</term>
<term>Linear trend</term>
<term>Linear trends</term>
<term>Long period</term>
<term>Long tide gauge records</term>
<term>Marcos</term>
<term>Marseille</term>
<term>Martin miguez</term>
<term>Matrix form</term>
<term>Mediterranean</term>
<term>Mediterranean basin</term>
<term>Mediterranean region</term>
<term>Mediterranean stations</term>
<term>Negative values</term>
<term>Nonclimate contribution</term>
<term>Northern coast</term>
<term>Northern greece</term>
<term>Novel approach</term>
<term>Ocean model</term>
<term>Open oceanic conditions</term>
<term>Other hand</term>
<term>Permanent service</term>
<term>Position time series</term>
<term>Present study</term>
<term>Previous estimates</term>
<term>Previous studies</term>
<term>Psmsl</term>
<term>Relative importance</term>
<term>Rigorous comparison</term>
<term>Rovinj</term>
<term>Rudimentary comparison</term>
<term>Same models</term>
<term>Satellite</term>
<term>Satellite altimetry</term>
<term>Satellite altimetry data</term>
<term>Satellite altimetry time series</term>
<term>Seasonal signals</term>
<term>Second option</term>
<term>Selen</term>
<term>Selen model</term>
<term>Sensitivity tests</term>
<term>Southern europe</term>
<term>Southern european coasts</term>
<term>Spurious signals</term>
<term>Standard deviation</term>
<term>Standard error</term>
<term>Stations display</term>
<term>Subsidence</term>
<term>Supplementary data</term>
<term>Tentative exercise</term>
<term>Thessaloniki</term>
<term>Tide</term>
<term>Tide gauge</term>
<term>Tide gauge benchmark</term>
<term>Tide gauge data</term>
<term>Tide gauge observations</term>
<term>Tide gauge record</term>
<term>Tide gauge records</term>
<term>Tide gauge sites</term>
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<term>Tide gauge trends</term>
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<term>Time span</term>
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<term>Trieste rovinj bakar split marjana split</term>
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<term>Uplift</term>
<term>Useful source</term>
<term>Valid data</term>
<term>Variables exhibit</term>
<term>Various approaches</term>
<term>Venezia</term>
<term>Vertical crustal motion</term>
<term>Vertical land motion</term>
<term>Vertical land movement</term>
<term>Vertical land movement estimates</term>
<term>Vertical land movements</term>
<term>Vertical motion</term>
<term>Vertical motions</term>
<term>Vertical velocities</term>
<term>Vigo cascais marseille venezia</term>
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<term>Year level</term>
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<div type="abstract">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 data to investigate the relative importance of the nonclimate contribution of vertical land movement to the observed rates of sea level change along the coasts of southern Europe. The sensitivity tests proved that the advanced approach is robust and accurate at the submillimeter per year level of around 0.4 mm yr−1in estimating rates of vertical land movements. It enabled identifying stations displaying large rates of vertical land movements that must be taken into account when predicting future sea level rise and appraising the exposure to its impacts on populations and assets. The average rate of coastal climate‐related sea level rise in the Mediterranean Sea was consequently revisited to be of 1.7 mm yr−1 over the past century, whereas the Atlantic northern Iberian coast revealed a significant high rate of sea level rise in excess of 3.4 mm yr−1 for the past 70 years. Future work should consider applying this powerful approach to other geographic contexts as a useful source of supplementary data for geodynamic studies.</div>
<div type="abstract">Advanced approach of combining tide gauge and satellite altimetry data Importance of nonclimate contributions to observed sea level rise at the coast Coherent spatial patterns of sea level rise along the European coasts inferred</div>
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