Attributing sources of tropical cyclogenesis (TCG) bias to large-scale
circulation in global circulation models is challenging. Here, we
propose the use of empirical orthogonal functions as an approach to
understand model bias of TCG. Two leading modes of large-scale wind
circulations in the West Pacific can explain the TCG frequency and
location in both climate reanalysis and the MetUM model. In the
reanalysis, the two modes distinguish the summer monsoon trough position
and the strength of the north Pacific subtropical high. However, in the
model, the wind circulations are biased towards the positive phase of
simulated modes thus overestimating TCG in the entire Main Development
Region. This bias is further related to the north-eastward shifted
monsoon trough and a weakened subtropical high, and overly strong
tropics-subtropics connections. This approach could be deployed more
widely to other basins and models to diagnose the causes of TCG bias.