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BISICLES Pine Island Glacier simulations with linear friction
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Meridional density gradients do not control the Atlantic overturning circulation
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BISICLES Pine Island Glacier simulations with linear friction
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Sensitivity of atmospheric CO2 to regional variability in particulate organic ma...
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Similar meltwater contributions to glacial sea level changes from Antarctic and...
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Similar meltwater contributions to glacial sea level changes from Antarctic and...
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Sensitivity of atmospheric CO2 to regional variability in particulate organic ma...
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Sensitivity of atmospheric CO2 to regional variability in particulate organic ma...
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Similar meltwater contributions to glacial sea level changes from Antarctic and...
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Sensitivity of atmospheric CO2 to regional variability in particulate organic ma...
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Similar meltwater contributions to glacial sea level changes from Antarctic and...
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BISICLES Pine Island Glacier simulations with linear friction
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BISICLES Pine Island Glacier simulations with nonlinear friction
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BISICLES Pine Island Glacier simulations with strongly nonlinear friction
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Quantifying the Impact of Bedrock Topography Uncertainty in Pine Island Glacier...
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The role of enhanced rock weathering deployment with agriculture in limiting fut...
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The role of enhanced rock weathering deployment with agriculture in limiting fut...
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PLASIM–GENIE v1.0: a new intermediate complexity AOGCM
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PLASIM–GENIE v1.0: a new intermediate complexity AOGCM
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Coupled climate–carbon cycle simulation of the Last Glacial Maximum atmospheric...
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boundary condition
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[SDU]Sciences of the Universe [physics]
530 Physics
author-correction
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37 Earth Sciences
Earth system model
Letter
Paris agreement temperature targets
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