Sensitivity of Precipitation and Structure of Typhoon Hato to Bulk and Explicit Spectral Bin Microphysics Schemes

Table 1

Domain averages within a 210 km radius of the center of Typhoon Hato and time averages before and after landfall of important variables in the four simulations.

	Before landfall				After landfall
	Lin	WDM6	Morrison	SBM	Lin	WDM6	Morrison	SBM
Ps (mm/hr)	6.39	6.83	6.00	6.96	7.92	7.08	7.12	7.23
IWP (kg/m^2)	0.85	2.05	2.11	3.73	1.01	2.09	2.88	3.65
LWP (kg/m^2)	1.95	2.23	1.73	2.64	2.33	2.43	1.97	2.85
Convective (%)	27.93	38.54	33.81	46.3	33.19	41.2	44.87	54.67
Stratiform (%)	22.65	17.08	23.41	31.16	18.92	16.87	18.36	20.62
Mixed (%)	28.43	17.45	20.81	16.62	28.07	19.21	17.02	20.08
qc (kg/m^2)	0.5	0.36	0.43	0.1	0.56	0.39	0.45	0.1
qr (kg/m^2)	1.45	1.91	1.30	2.57	1.71	2.03	1.52	2.77
qi (kg/m^2)	0.09	0.16	0.14	0.08	0.08	0.15	0.16	0.07
qs (kg/m^2)	0.18	1.01	1.37	3.08	0.17	0.96	1.89	2.96
qg (kg/m^2)	0.59	0.91	0.60	0.62	0.75	0.99	0.82	0.66

P_s is the precipitation rate; convective, stratiform, and mixed are representative of the proportion of grids of each precipitation type to all precipitation grids; IWP and LWP are the ice water path and liquid water path, respectively; q_r, q_c, q_i, q_s, and q_g are vertical integrations of rainwater, cloud water, cloud ice, snow, and graupel, respectively.