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Critical evaluation of climate syntheses to benchmark CMIP6/PMIP4 127 ka Last In...
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Critical evaluation of climate syntheses to benchmark CMIP6/PMIP4 127 ka Last In...
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Critical evaluation of climate syntheses to benchmark CMIP6/PMIP4 127 ka Last In...
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Critical evaluation of climate syntheses to benchmark CMIP6/PMIP4 127 ka Last In...
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Critical evaluation of climate syntheses to benchmark CMIP6/PMIP4 127 ka Last In...
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NOAA/WDS Paleoclimatology - Benguela Upwelling System Hydrogen and Carbon Isotop...
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Effects of CO2 and H2S on corrosion of martensitic steels in NaCl(aq) at low tem...
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Effects of CO2 and H2S on corrosion of martensitic steels in brines at low tempe...
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Past terrestrial hydroclimate sensitivity controlled by Earth system feedbacks
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Mid-Pliocene Atlantic Meridional Overturning Circulation simulated in PlioMIP2
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Evaluation of Arctic warming in mid-Pliocene climate simulations
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Unraveling the mechanisms and implications of a stronger mid-Pliocene Atlantic M...
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Evaluation of Arctic warming in mid-Pliocene climate simulations
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A return to large-scale features of Pliocene climate: the Pliocene Model Interco...
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The Pliocene Model Intercomparison Project Phase 2: large-scale climate features...
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The Pliocene Model Intercomparison Project Phase 2: A return to large-scale feat...
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Lessons from a high-CO2 world: an ocean view from ∼ 3 million years ago
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Lessons from a high-CO 2 world: an ocean view from similar to 3 million years ag...
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Lessons from a high CO2 world : an ocean view from ~ 3 million years ago.
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Related Subjects
127 ka surface temperature time slice
CMIP6/PMIP4 Tier 1 and Tier 2 simulations
Corrosion Rate
Martensitic Carbon Steels
last interglacial
quantitative uncertainty estimates attached to relative dating and temperature reconstruction methods
CO2 Corrosion
Cold Climate Conditions
Cold climate corrosion
Corrosion Mechanism
Corrosion Scales
H2S Corrosion
Last interglacial
Quantitative uncertainty estimates attached to relative dating and temperature reconstruction methods
Sweet and Sour Corrosion
envir
geo
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