Toward Convective-Scale Prediction within the Next Generation Global Prediction System

被引:131
作者
Zhou, Linjiong [1 ,2 ]
Lin, Shian-Jiann [2 ]
Chen, Jan-Huey [2 ,3 ]
Harris, Lucas M. [2 ]
Chen, Xi [1 ,2 ]
Rees, Shannon L. [2 ,3 ]
机构
[1] Princeton Univ, Program Atmosphe & Ocean Sci, Princeton, NJ 08544 USA
[2] NOAA, Geophys Fluid Dynam Lab, Princeton, NJ 08540 USA
[3] Univ Corp Atmospher Res, Princeton, NJ USA
关键词
NUMERICAL WEATHER PREDICTION; HIGH-RESOLUTION VERSION; ICE-PHASE MICROPHYSICS; DYNAMICAL CORE; HORIZONTAL RESOLUTION; NCEP GFS; MODEL; PARAMETERIZATION; FORECASTS; PRECIPITATION;
D O I
10.1175/BAMS-D-17-0246.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The Geophysical Fluid Dynamics Laboratory (GFDL) has developed a new variable-resolution global model with the ability to represent convective-scale features that serves as a prototype of the Next Generation Global Prediction System (NGGPS). The goal of this prediction system is to maintain the skill in large-scale features while simultaneously improving the prediction skill of convectively driven mesoscale phenomena. This paper demonstrates the new capability of this model in convective-scale prediction relative to the current operational Global Forecast System (GFS). This model uses the stretched-grid functionality of the Finite-Volume Cubed-Sphere Dynamical Core (FV3) to refine the global 13-km uniform-resolution model down to 4-km convection-permitting resolution over the contiguous United States (CONUS), and implements the GFDL single-moment 6-category cloud microphysics to improve the representation of moist processes. Statistics gathered from two years of simulations by the GFS and select configurations of the FV3-based model are carefully examined. The variable-resolution FV3-based model is shown to possess global forecast skill comparable with that of the operational GFS while quantitatively improving skill and better representing the diurnal cycle within the high-resolution area compared to the uniform mesh simulations. Forecasts of the occurrence of extreme precipitation rates over the southern Great Plains are also shown to improve with the variable-resolution model. Case studies are provided of a squall line and a hurricane to demonstrate the effectiveness of the variable-resolution model to simulate convective-scale phenomena.
引用
收藏
页码:1225 / 1243
页数:19
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