Arctic Amplification in the Community Earth System Models (CESM1 and CESM2)

Author:

Chylek Petr1,Folland Chris234,Klett James D.5,Lesins Glen6,Dubey Manvendra K.1

Affiliation:

1. Los Alamos National Laboratory, Earth and Environmental Sciences, Los Alamos, NM 87545, USA

2. School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ, UK

3. Department of Earth Sciences, University of Gothenburg, 41320 Gothenburg, Sweden

4. Centre for Applied Climate Sciences, University of Southern Queensland, Toowoomba, QLD 4350, Australia

5. PAR Associates, Las Cruces, NM 88011, USA

6. Department of Physics and Atmospheric Science, Dalhousie University, Halifax, NS B3H 4R2, Canada

Abstract

We compare the Arctic amplification (AA) produced by the two Community Earth System Models CESM1 and CESM2, members of the CEMIP5 (Coupled Models Intercomparison Project phase 5) and CEMIP6 collections, respectively. We find that the CESM1 model reproduces the recent high values of the AA deduced from the observed temperature much better than the CESM2. The correlation coefficient within the 1970–2012 time period between CESM1-simulated AA and the observed one is 0.47, while the CESM2 simulation leads to an anticorrelation of r = −0.53. Even the more successful model (CESM1) is not able to reproduce recent high AA values of 4–5. The main cause of this failure is the model’s overestimate of the rate of increase in the mean global temperature in years post 1990. When the CESM1 model’s simulated trend of the mean global temperature is replaced in the expression for the AA by the observed temperature trend, the correlation coefficient increases from 0.47 to 0.75. The CESM1 model is among the best north American models in AA simulation while the CESM2 model is among the least successful.

Publisher

MDPI AG

Subject

Atmospheric Science,Environmental Science (miscellaneous)

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