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Impacts of a reduced thermohaline circulation on transport and growth of larvae...
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Bergen Earth system model (BCM-C): model description and regional climate-carbon...
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Bergen Earth system model (BCM-C): model description and regional climate-carbon...
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Impacts of UV Irradiance and Medium-Energy Electron Precipitation on the North A...
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Interannual to decadal climate predictability in the North Atlantic: A multimode...
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The role of subpolar deep water formation and Nordic Seas overflows in simulated...
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The role of subpolar deep water formation and Nordic Seas overflows in simulated...
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The role of subpolar deep water formation and Nordic Seas overflows in simulated...
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The role of subpolar deep water formation and Nordic Seas overflows in simulated...
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The role of subpolar deep water formation and Nordic Seas overflows in simulated...
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Using simulations of the last millennium to understand climate variability seen...
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Using simulations of the last millennium to understand climate variability seen...
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Using simulations of the last millennium to understand climate variability seen...
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Using simulations of the last millennium to understand climate variability seen...
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Using simulations of the last millennium to understand climate variability seen...
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A multi-model comparison of Atlantic multidecadal variability
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The role of the Barents Sea in the climate system
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A multi-model comparison for Atlantic multidecadal variability
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Impacts of UV irradiance and medium-energy electron precipitation on the North A...
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The effects of aggressive mitigation on steric sea level rise and sea ice change...
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[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
[SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
530 Physics
11-year solar cycle
Atlantic meridional overturning circulation (AMOC)
Atlantic multidecadal variability (AMV)
Atmospheric Science
North Atlantic Oscillation
North Atlantic Oscillation (NAO)
Subpolar gyre (SPG)
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climate models
energetic particle precipitation
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