Abstract:
This paper presents an evaluation of theWeather Research and Forecasting (WRF) model in simulating wet and dryWest African
monsoon (WAM) rainfall seasons. Three model experiments with varying selected microphysics (MP), cumulus convection
(CU), and planetary boundary layer (PBL) schemes based on previous study were performed. Each of the model combinations is
used to run four WAM seasons that consist of two wet (2008 and 2010) and two dry years (2001 and 2011). To investigate the
behavior ofWAM in the context of wet and dry years, the four seasons were used to compute composites of wet and dryWAM
seasons in terms of rainfall amount. The analyses majorly focus on the rainfall composites relative to rainfall from Global
Precipitation Climatology Project (GPCP) and Tropical Rainfall Measurement Mission (TRMM) as well as temperature, moisture,
and atmospheric circulation fields with respect to NCEP reanalyses. This study documents significant sensitivity in simulation
of the West African monsoon to the choices of the MP, CU, and PBL schemes. The simulation with the combination of
WRF single moment 5 (WSM5) MP, Yonsei University (YSU) PBL, and new Simplified Arakawa-Schubert CU (WSM5-YSUnSAS)
shows good spatial distribution pattern of rainfall and the dynamics associated with the monsoon. Quantitatively, the
combination shows less agreement in distinguishing the selected WAM seasons compared with the Goddard MP, Mellor-
Yamada-Janjic PBL, and Betts-Miller-Janjić CU (GD-MYJ-BMJ) and the WSM5, Mellor-Yamada-Nakanishi-Niino 2.5 level
and new Tiedtke CU (WSM5-MYNN-nTDK). Also, the dynamical structures of the wet and dry WAM circulation composites
are reasonably reproduced in GD-MYJ-BMJ and WSM5-YSU-nSAS. The GD-MYJ-BMJ was able to distinguish between wet
and dry years and thus underscores its potential to reproduce climate change signals in future work.
