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Comment on "Multiyear prediction of monthly mean Atlantic Meridional Overturning Circulation at 26.5°N".Have Aerosols Caused the Observed Atlantic Multidecadal Variability?Anomalously weak Labrador Sea convection and Atlantic overturning during the past 150 yearsRecent multivariate changes in the North Atlantic climate system, with a focus on 2005-2016Decadal prediction of the North Atlantic subpolar gyre in the HiGEM high-resolution climate modelImpact of internal variability on projections of Sahel precipitation changeA reversal of climatic trends in the North Atlantic since 2005Comment on "The Atlantic Multidecadal Oscillation without a role for ocean circulation"Decadal predictions with the HiGEM high resolution global coupled climate model: description and basic evaluationMechanisms of decadal variability in the Labrador Sea and the wider North Atlantic in a high-resolution climate modelAtlantic overturning in decline?A novel transport assimilation method for the Atlantic meridional overturning circulation at 26°NDecadal predictions of the cooling and freshening of the North Atlantic in the 1960s and the role of ocean circulationThe Importance of Wind and Buoyancy Forcing for the Boundary Density Variations and the Geostrophic Component of the AMOC at 26°NThe Interpretation and Use of Biases in Decadal Climate PredictionsPredictable Climate Impacts of the Decadal Changes in the Ocean in the 1990sCauses of the Rapid Warming of the North Atlantic Ocean in the Mid-1990sEvaluating the potential for statistical decadal predictions of sea surface temperatures with a perfect model approachForced decadal changes in the East Asian summer monsoon: the roles of greenhouse gases and anthropogenic aerosolsRecent Progress in Understanding and Predicting Atlantic Decadal Climate VariabilityA little daily dose : discovering Chinese characters through short stories
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P50
description
onderzoeker
@nl
researcher of Wikimedia softwares
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name
Jon Robson
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Jon Robson
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Jon Robson
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P1053
A-7677-2012
P1153
14036209800
P21
P3829
P4174
P496
0000-0002-3467-018X