Twentieth-Century Global-Mean Sea Level Rise: Is the Whole Greater than the Sum of the Parts?
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Temperature-driven global sea-level variability in the Common EraAttribution of global glacier mass loss to anthropogenic and natural causesProbabilistic reanalysis of twentieth-century sea-level rise.What does global mean temperature tell us about local climate?Spatial and temporal distribution of mass loss from the Greenland Ice Sheet since AD 1900.Revisiting the contemporary sea-level budget on global and regional scales.Detecting anthropogenic footprints in sea level rise.Reassessment of 20th century global mean sea level rise.Timescales for detecting a significant acceleration in sea level rise.Closing the sea level budget on a regional scale: Trends and variability on the Northwestern European continental shelf.Thresholds of sea-level rise rate and sea-level rise acceleration rate in a vulnerable coastal wetland.Sea level rise and its coastal impactsDetection of an observed 135 year ocean temperature change from limited dataProbabilistic 21st and 22nd century sea-level projections at a global network of tide-gauge sitesA Review of Recent Updates of Sea-Level Projections at Global and Regional ScalesAnthropogenic forcing dominates global mean sea-level rise since 1970Recent Changes in Land Water Storage and its Contribution to Sea Level VariationsEvolution of Mid-Atlantic Coastal and Back-Barrier Estuary Environments in Response to a Hurricane: Implications for Barrier-Estuary ConnectivityGlobal change and the groundwater management challengeRole of Perturbing Ocean Initial Condition in Simulated Regional Sea Level ChangeEffects of long-term variability on projections of twenty-first century dynamic sea levelFate of water pumped from underground and contributions to sea-level riseModeling Groundwater Depletion at Regional and Global Scales: Present State and Future ProspectsLiquid Water Flow and Retention on the Greenland Ice Sheet in the Regional Climate Model HIRHAM5: Local and Large-Scale ImpactsDoes the mid-Atlantic United States sea level acceleration hot spot reflect ocean dynamic variability?Steric sea level variability (1993–2010) in an ensemble of ocean reanalyses and objective analysesStochastic secular trends in sea level riseSensitivity, stability and future evolution of the world's northernmost ice cap, Hans Tausen Iskappe (Greenland)Analysis of the regional pattern of sea level change due to ocean dynamics and density change for 1993–2099 in observations and CMIP5 AOGCMsAre long tide gauge records in the wrong place to measure global mean sea level rise?The Twentieth-Century Sea Level Budget: Recent Progress and ChallengesTime of emergence for regional sea-level changeImpact of self-attraction and loading effects induced by shelf mass loading on projected regional sea level riseSea level changes forced by Southern Ocean windsSeasonal prediction of global sea level anomalies using an ocean–atmosphere dynamical model
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Twentieth-Century Global-Mean Sea Level Rise: Is the Whole Greater than the Sum of the Parts?
description
im Juli 2013 veröffentlichter wissenschaftlicher Artikel
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wetenschappelijk artikel
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наукова стаття, опублікована в липні 2013
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name
Twentieth-Century Global-Mean ...... ter than the Sum of the Parts?
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Twentieth-Century Global-Mean ...... ter than the Sum of the Parts?
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type
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Twentieth-Century Global-Mean ...... ter than the Sum of the Parts?
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Twentieth-Century Global-Mean ...... ter than the Sum of the Parts?
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Twentieth-Century Global-Mean ...... ter than the Sum of the Parts?
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Twentieth-Century Global-Mean ...... ter than the Sum of the Parts?
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Twentieth-Century Global-Mean ...... ter than the Sum of the Parts?
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J. A. Church
J. G. Cogley
J. M. Gregory
J. Oerlemans
L. M. Wake
M. E. Tamisiea
N. J. White
P. W. Leclercq
R. S. W. van de Wal
P304
P356
10.1175/JCLI-D-12-00319.1
P407
P50
P577
2013-07-01T00:00:00Z