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Simulating the mid-Pliocene Warm Period with the CCSM4 model
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Simulating the mid-Pliocene Warm Period with the CCSM4 model
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The amplification of Arctic terrestrial surface temperatures by reduced sea-ice...
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Arctic sea ice simulation in the PlioMIP ensemble
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Arctic sea ice simulation in the PlioMIP ensemble
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Evaluating the dominant components of warming in Pliocene climate simulations
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Evaluating the dominant components of warming in Pliocene climate simulations
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Evaluating the dominant components of warming in Pliocene climate simulations
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Evaluating the dominant components of warming in Pliocene climate simulations
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Evaluating the dominant components of warming in Pliocene climate simulations
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Evaluating the dominant components of warming in Pliocene climate simulations
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Evaluating the dominant components of warming in Pliocene climate simulations
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Evaluating the dominant components of warming in Pliocene climate simulations
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Evaluating the Dominant Components of Warming in Pliocene Climate Simulations
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Twelve thousand years of dust: The Holocene global dust cycle constrained by nat...
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Evaluating the dominant components of warming in Pliocene climate simulations
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Evaluating the dominant components of warming in Pliocene climate simulations
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[SDV.EE.BIO]Life Sciences [q-bio]/Ecology
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environment/Bioclimatology
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Verlagsveröffentlichung
article
envir
geo
Geosciences
Multidisciplinary
Arctic amplification
COUPLED MODEL
Central Great-plains
Chinese Loess Plateau
Deep-sea Sediments
Earth Sciences
East-asian Monsoon
GENERAL-CIRCULATION MODEL
GEO/04 - GEOGRAFIA FISICA E GEOMORFOLOGIA
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Grain-size Records
Greenland Ice Core
High-resolution
LATE NEOGENE
Last Glacial Maximum
Late Quaternary Loess
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