2.DataandMethods 1.Introduction TheNorthAtlanticOscillationandgreenhouse-gasforcing

1) Preliminary simulation results for the floating pipe and riser cases from the coupled flow-structure simulator are in a good agreement with experiments. For floating pipe case

Coupled with a predicted no-effect concentration of 0.01 mg l −1 determined for H 2 O 2 in water (Institute for Health and Consumer Protection in Finland 2003), the results of

A coupled climate model is used to explore the response of the tropical sea surface temperature (SST) to positive SST anomalies in the global extratropics.. The main model results

We then provide an ini- tial analysis of the multi-model ensemble mean and model spread in the lig127k surface temperature, precipitation, and Arctic sea ice responses as compared

In fact, in a 150-year twin experiment with the Bergen Climate Model (a fully coupled atmosphere-sea ice- ocean climate model; Furevik et al., 2003), the pole- ward flow of

The NorESM future projections predict reduction of the AMOC with 12 to 30% under different warming (RCP2.6-RCP8.5) scenarios. In the CMIP5 model intercomparison project, the

[ 1 ] A five-member ensemble with a coupled atmosphere- sea ice-ocean model is used to examine the effects of natural variability on climate projections for the Arctic.. The

We analysed 17 global climate models participating in phase 5 of the Coupled Model Intercomparison Project (CMIP5), identifying the likelihood and duration of periods with-