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Simulating Arctic Ice Clouds during Spring Using an Advanced Ice Cloud Microphysics in the WRF Model

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Academic year: 2021

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Figure

Figure 1 Upper panel: Model domain (yellow contour) used in this study centered over Fairbanks with a horizontal resolution of 10 km
Table 1. Parameterizations and options used for the WRF simulations.
Table 2. Ice nucleation parameterization schemes used for the simulations. The original microphysical scheme (WRF) is based on the singular hypothesis, while WRF_np and WRF_p are based on the stochastic theory, which includes a contact angle (θ = 12 ◦ and
Table 3 presents a brief description of the four specific ISDAC flights that have been used to validate our ice nucleation parameterization
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