Simulations for CMIP6 With the AWI Climate Model AWI‐CM‐1‐1

• Published in: Journal of Advances in Modeling Earth Systems
• Main Authors: Tido Semmler, Sergey Danilov, Paul Gierz, Helge F. Goessling, Jan Hegewald, Claudia Hinrichs, Nikolay Koldunov, Narges Khosravi, Longjiang Mu, Thomas Rackow, Dmitry V. Sein, Dmitry Sidorenko, Qiang Wang, Thomas Jung
• Format: Article in Journal/Newspaper
• Language: English
• Published: American Geophysical Union (AGU) 2020
• Subjects: global climate model; AWI climate model; Coupled Model Intercomparison Project; climate change; unstructured mesh; Physical geography; GB3-5030; Oceanography; GC1-1581; Arctic; Barents Sea; Southern Ocean; Climate change; Sea ice
• Online Access: https://doi.org/10.1029/2019MS002009; https://doaj.org/article/3735bf3495294d16b6296635b3a5d8e8

Abstract The Alfred Wegener Institute Climate Model (AWI‐CM) participates for the first time in the Coupled Model Intercomparison Project (CMIP), CMIP6. The sea ice‐ocean component, FESOM, runs on an unstructured mesh with horizontal resolutions ranging from 8 to 80 km. FESOM is coupled to the Max Planck Institute atmospheric model ECHAM 6.3 at a horizontal resolution of about 100 km. Using objective performance indices, it is shown that AWI‐CM performs better than the average of CMIP5 models. AWI‐CM shows an equilibrium climate sensitivity of 3.2°C, which is similar to the CMIP5 average, and a transient climate response of 2.1°C which is slightly higher than the CMIP5 average. The negative trend of Arctic sea‐ice extent in September over the past 30 years is 20–30% weaker in our simulations compared to observations. With the strongest emission scenario, the AMOC decreases by 25% until the end of the century which is less than the CMIP5 average of 40%. Patterns and even magnitude of simulated temperature and precipitation changes at the end of this century compared to present‐day climate under the strong emission scenario SSP585 are similar to the multi‐model CMIP5 mean. The simulations show a 11°C warming north of the Barents Sea and around 2°C to 3°C over most parts of the ocean as well as a wetting of the Arctic, subpolar, tropical, and Southern Ocean. Furthermore, in the northern middle latitudes in boreal summer and autumn as well as in the southern middle latitudes, a more zonal atmospheric flow is projected throughout the year.