hysics=1,1,0,cudt=5,5,5,isfflx=1,ifsnow=1,icloud=1,surface_input_source=1,num_soil_layers=4,sf_urban_physics=0,0,0,/&fdda/&dynamicsw_damping=0,diff_opt=1,km_opt=4,diff_6th_opt=0,0,0,diff_6th_factor=0.12,0.12,0.12,base_temp=290.damp_opt=0,zdamp=5000.,5000.,5000.,dampcoef=0.2,0.2,0.2khdif=0,0,0,kvdif=0,0,0,non_hydrostatic=.true.,.true.,.true.,moist_adv_opt=1,1,1,scalar_adv_opt=1,1,1,/&bdy_controlspec_bdy_width=5,spec_zone=1,relax_zone=4,specified=.true.,.false.,.false.,nested=.false.,.true.,.true.,/&grib2/&namelist_quiltnio_tasks_per_group=0,nio_groups=1,/五、实习结果及分析1.模拟区域地形topography 2.模式模拟范围从模拟区域地形及范围图可以看出:绘图时刻为2010-10-16_00:00:00至2010-10-17_00:00:00,台风已经到达,附近,绘图区域选取为是合适的。此地区处于菲律宾吕宋岛附近,在西太平洋洋面上,吕宋岛位势高度稍微较高。3.模式输出skintemperature从此图可以看出:广阔的西太平洋温度较高可以达到303K,在菲律宾吕宋岛和台湾温度较低,大约为293K。4.模式输出Pressure
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