Coupled atmosphere-ocean model simulations
Internal atmospheric noise characteristics in twentieth century coupled atmosphere–ocean model simulations
13
Global climate simulations at 3000-year intervals for the last 21 000 years with the GENMOM coupled atmosphere–ocean model
23
Coupled atmosphere ocean climate model simulations in the Mediterranean region: effect of a high-resolution marine model on cyclones and precipitation
11
Modelling the Caspian Sea and its catchment area using a coupled regional atmosphere-ocean model (RegCM4-ROMS): model design
17
Effects of orbital forcing on atmosphere and ocean heat transports in Holocene and Eemian climate simulations with a comprehensive Earth system model
14
Estimation of oceanic subsurface mixing under a severe cyclonic storm using a coupled atmosphere–ocean–wave model
14
MetUM-GOML1: a near-globally coupled atmosphere–ocean-mixed-layer model
17
Early deglacial Atlantic overturning decline and its role in atmospheric CO 2rise inferred from carbon isotopes (13(C)
18
Simulating Southern Hemisphere extra-tropical climate variability with an idealised coupled atmosphere-ocean model
15
The modern and glacial overturning circulation in the Atlantic ocean in PMIP coupled model simulations
14
An EC-Earth coupled atmosphere–ocean single-column model (AOSCM.v1_EC-Earth3) for studying coupled marine and polar processes
21
Evaluation of a present-day climate simulation with a new coupled atmosphere-ocean model GENMOM
15
The role of atmosphere and ocean physical processes in ENSO in a perturbed physics coupled climate model
19
Medicanes in an ocean–atmosphere coupled regional climate model
13
The coupled atmosphere–chemistry–ocean model SOCOL-MPIOM
23
The Atmosphere-Ocean General Circulation Model EMAC-MPIOM
14
Modeling the ocean and atmosphere during an extreme bora event in northern Adriatic using one-way and two-way atmosphere–ocean coupling
16
Statistics of locally coupled ocean and atmosphere intraseasonal anomalies in Reanalysis and AMIP data
7
Internal oscillations of the thermohaline circulation and abrupt climate changes during the last Ice Age and perhaps in the future
135
A global assessment of marine heatwaves and their drivers
13