作者: J. H. Jungclaus , N. Keenlyside , M. Botzet , H. Haak , J.-J. Luo
DOI: 10.1175/JCLI3827.1
关键词: Environmental science 、 Climatology 、 Climate change 、 Thermohaline circulation 、 Ocean current 、 Wind stress 、 Sea ice 、 Flux 、 Sea surface temperature 、 Greenhouse gas
摘要: Abstract This paper describes the mean ocean circulation and tropical variability simulated by Max Planck Institute for Meteorology (MPI-M) coupled atmosphere–ocean general model (AOGCM). Results are presented from a version of that served as prototype Intergovernmental Panel on Climate Change (IPCC) Fourth Assessment Report (AR4) simulations. The does not require flux adjustment to maintain stable climate. A control simulation with present-day greenhouse gases is analyzed, key oceanic features, such sea surface temperatures (SSTs), large-scale circulation, meridional heat freshwater transports, ice compared observations. parameterization accounts effect currents wind stress implemented in model. largest impact this Pacific, where state significantly improved: strength trade winds associated...