The ability of the ECMWF model (cycle 33) to simulate the Indian and East Asian summer
monsoons is evaluated at four different horizontal resolutions: T21, T42, T63, and T1O6.
Generally, with respect to the large-scale features of the circulation, the largest differences
among the simulations occur at T42 relative to T21. However, on regional scales, important
differences among the high-frequency temporal variability serve as a further critical rest of
the model's ability to simulate the monsoon. T106 best captures both the spatial and …

Simulation of the northern summer monsoon in the ECMWF model: sensitivity to horizontal
resolution … Simulation of the northern summer monsoon in the ECMWF model: sensitivity
to horizontal resolution …