The above heavy rain was detected by
all of the scheme experiments and simulated
particularly well with KF and GD. KF scheme
experiment simulated high intensity rainfall
from Songkhla to Narathiwat. However, the
simulated rainfall in GD scheme experiment
was reasonably accurate as well, though the
maximum intensity rainfall was located around
Surat Thani and Nakhon Si Thammarat. The
underestimation of BMJ rainfall products
might result from the limits of the Cumulus
scheme, not including a convective-scale
downdraft parameterization and not directly
generating mesoscale highs and lows.