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Fog Simulation with the (WRF+PAFOG) Coupled Model Utilizing Meteorological Tower Data
Seong Soo Yum1, Wonheung Kim1, Jae-In Song1 and Chang Ki Kim2 1Department of Atmospheric Sciences, Yonsei University, Korea 2New and Renewable Energy Resource Center, Korea Institute of Energy Research, Korea
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Introduction Prediction of fog using numerical models is difficult because fog formation is usually determined by local meteorological conditions that are hard to be measured and modeled with sufficient resolution. In this study we uses the coupled system of the 1D PAFOG model and the 3D WRF model to simulate fogs formed at a southern coastal region of Korea, where the National Center for Intensive Observation of Severe Weather (NCIO) is located. Here we demonstrate how the coupled model simulation of fog can be improved with the utilization of meteorological tower data.
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The Models 3D MODEL WRF V3.7 Horizontal Resolution 18, 6, 2 km Vertical Layers 65 (top~20 km) Initial field NCEP FNL data Radiation Process RRTMg scheme (both SW & LW) PBL Process MYNN scheme Surface physics Unified Noah land-surface model Microphysics Morrison 1D MODEL (PAFOG, PArameterized FOG, Bott and Trautmann, 2002) Vertical Layers Dynamics turbulence Radiation Microphysics Vegetation PAFOG L400 (up to the model top, 2.5 km) Bott et al. (1990) 2.5 level model of Mellor and Yamada(1974) Δ-two straem approximation of Zdunkowski et al.(1982) Nickerson et al.(1986) and Chaumerloac et al. (1987) Siebert et al.(1992)
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Model Domain Coupling Method Selected Cases (2014.05.~2015.06.)
WRF_D1 WRF_D2 WRF_D3 Model Domain Coupling Method Number of Fog Cases 22 Selected Cases ( ~ )
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Study Region Location: Boseong, Korea (34.76 o N, 127.16 o E).
Instrumentation : 300 m Met. Tower (T, Td every 30 m) 300 met. tower Ka-band cloud radar Microwave Radiometer Ceilometer Parsivel2
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Average vertical profiles of Tz-T0 and RH (Met Tower)
Non-fog days Fog days
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Nudging Method Time Weighting Height Weighting Tower (t0min) (t30min)
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Skill Scores HR CSI 0.05 ± 0.12 0.11 ± 0.23 0.27 ± 0.30 0.14 ± 0.18
~ (22 cases) HR(Hit Rate) = 𝒂 𝒂+𝒄 counts Observation Yes No Forecast a b c d CSI(Critical Success Index) = 𝒂 𝒂+𝒃+𝒄 HR CSI WRF 0.05 ± 0.12 0.11 ± 0.23 WRF+PAFOG 0.27 ± 0.30 0.14 ± 0.18 (Initial _TOWER) 0.60 ± 0.48 0.23 ± 0.18 (nudging_TOWER) 0.81 ± 0.21 0.45 ± 0.22
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Skill Scores HR CSI 0.05 ± 0.12 0.11 ± 0.23 0.27 ± 0.30 0.14 ± 0.18
~ (22 cases) HR(Hit Rate) = 𝒂 𝒂+𝒄 count Observations Yes No Forecasts a b c d CSI(Critical Success Index) = 𝒂 𝒂+𝒃+𝒄 HR CSI WRF+PAFOG(nudging_TOWER) for radiation fog cases (13) 0.93 ± 0.24 0.65 ± 0.16 WRF+PAFOG(nudging_TOWER) for cases with prior precip. (9) 0.68 ± 0.24 0.26 ± 0.13 HR CSI WRF 0.05 ± 0.12 0.11 ± 0.23 WRF+PAFOG 0.27 ± 0.30 0.14 ± 0.18 (Initial _TOWER) 0.60 ± 0.48 0.23 ± 0.18 (nudging_TOWER) 0.81 ± 0.21 0.45 ± 0.22
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Time Variation of Met. Variables
A case with prior precipitation ( ) Soil moisture variation due to precipitation considered Precip.
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Skill Scores HR CSI 0.05 ± 0.12 0.11 ± 0.23 0.27 ± 0.30 0.14 ± 0.18
~ (22 cases) HR(Hit Rate) = 𝒂 𝒂+𝒄 count Observations Yes No Forecasts a b c d CSI(Critical Success Index) = 𝒂 𝒂+𝒃+𝒄 HR CSI WRF+PAFOG(nudging_TOWER) for radiation fog cases (13) 0.93 ± 0.24 0.65 ± 0.16 WRF+PAFOG(nudging_TOWER) for cases with prior precip. (9) 0.68 ± 0.24 0.26 ± 0.13 WRF+PAFOG(nudging_TOWER) for cases with prior precip. (9) (soil moisture variation considered) 0.82 ± 0.07 0.50 ± 0.08 HR CSI WRF 0.05 ± 0.12 0.11 ± 0.23 WRF+PAFOG 0.27 ± 0.30 0.14 ± 0.18 WRF+PAFOG(Initial _TOWER) 0.60 ± 0.48 0.23 ± 0.18 WRF+PAFOG(nudging_TOWER) 0.81 ± 0.21 0.45 ± 0.22
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Skill Scores HR CSI 0.05 ± 0.12 0.11 ± 0.23 0.27 ± 0.30 0.14 ± 0.18
~ (22 cases) HR(Hit Rate) = 𝒂 𝒂+𝒄 count Observations Yes No Forecasts a b c d CSI(Critical Success Index) = 𝒂 𝒂+𝒃+𝒄 HR CSI WRF+PAFOG(nudging_TOWER) for radiation fog cases (13) 0.93 ± 0.24 0.65 ± 0.16 WRF+PAFOG(nudging_TOWER) for cases with prior precip. (9) 0.68 ± 0.24 0.26 ± 0.13 WRF+PAFOG(nudging_TOWER) for cases with prior precip. (9) (soil moisture variation considered) 0.82 ± 0.07 0.50 ± 0.08 HR CSI WRF 0.05 ± 0.12 0.11 ± 0.23 WRF+PAFOG 0.27 ± 0.30 0.14 ± 0.18 (Initial _TOWER) 0.60 ± 0.48 0.23 ± 0.18 (nudging_TOWER) 0.81 ± 0.21 0.45 ± 0.22 WRF+PAFOG (nudging_TOWER) 0.88 ± 0.18 0.59 ± 0.13
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Skill Scores ~ (22 cases) HR(Hit Rate) = 𝒂 𝒂+𝒄 count Observations Yes No Forecasts a b c d CSI(Critical Success Index) = 𝒂 𝒂+𝒃+𝒄 HR CSI WRF+PAFOG(nudging_TOWER) for radiation fog case 0.93 ± 0.24 0.65 ± 0.16 WRF+PAFOG(nudging_TOWER) for precipitation effect case (not considered) 0.68 ± 0.24 0.26 ± 0.13 WRF+PAFOG(nudging_TOWER) for precipitation effect case (considered) 0.82 ± 0.07 0.50 ± 0.08 HR CSI WRF 0.05 ± 0.12 0.11 ± 0.23 WRF+PAFOG 0.27 ± 0.30 0.14 ± 0.18 (Initial _TOWER) 0.60 ± 0.48 0.23 ± 0.18 (nudging_TOWER) 0.81 ± 0.21 0.45 ± 0.22 But initial soil moisture values were fixed at minimum value for all cases! WRF+PAFOG (nudging_TOWER) 0.88 ± 0.18 0.59 ± 0.13
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Time Variation of Met. Variables
Observed Soil Moisture: m3/m3 0.266 m3/m3 0.394 m3/m3 Observed Soil Moisture: m3/m3 0.266 m3/m3 0.394 m3/m3
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Skill Scores HR CSI 0.88 ± 0.18 0.59 ± 0.13 HR CSI 0.89 ± 0.07
~ (22 cases) HR(Hit Rate) = 𝒂 𝒂+𝒄 count Observations Yes No Forecasts a b c d CSI(Critical Success Index) = 𝒂 𝒂+𝒃+𝒄 HR CSI WRF+PAFOG (nudging_TOWER) Precipitation effect considered 0.88 ± 0.18 0.59 ± 0.13 HR CSI WRF+PAFOG (nudging_TOWER) Initial soil moisture varied 0.89 ± 0.07 0.64 ± 0.13
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(Soil moisture variation)
Skill Scores ~ (22 cases) count Observations Yes No Forecasts a b c d WRF+PAFOG HR CSI 0.27 ± 0.30 0.14 ± 0.18 Nudging effect VS Soil moisture effect WRF+PAFOG (nudging_TOWER) HR CSI 0.81 ± 0.21 0.45 ± 0.22 WRF+PAFOG (Soil moisture variation) HR CSI 0.53 ± 0.35 0.27 ± 0.19
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Comparison of WRF and UM Coupled Simulations
~ (22 sea fog cases over the sea near IIA) UM_RE+PAFOG UM_LO+PAFOG WRF_CO+PAFOG WRF_NE+PAFOG MBE RMSE T -0.32 ± 0.91 1.70 ± 1.12 -0.75 ± 0.77 1.85 ± 1.16 3.20 ± 4.73 1.98 ± 1.14 3.38 ± 4.75 1.93 ± 1.38 Td 0.51 ± 0.61 1.59 ± 1.12 0.04 ± 0.74 1.44 ± 0.69 1.73 ± 2.93 1.96 ± 1.12 2.28 ± 3.06 2.03 ± 1.35 CSI rw 0.37 ± 0.34 0.22 ± 0.31 0.23 ± 0.32 0.17 ± 0.27
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Summary WRF+PAFOG coupled system was set up to use for fog simulation over the southern coastal region of Korea. With the utilization of meteorological tower data, performance of the coupled model improved significantly. For these coastal fog cases, soil moisture information was found to be critically important for better simulation. Next step is to elucidate fog formation mechanism based on the model simulation results. With proper adjustment, the coupled model system can be used as a fog prediction model during the PyeongChang Olympics.
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