Numerical simulation of the rapid intensification of Hurricane Katrina (2005): Sensitivity to boundary layer parameterization schemes

被引:24
作者
Liu, Jianjun [1 ,2 ,4 ]
Zhang, Feimin [2 ,3 ]
Pu, Zhaoxia [2 ]
机构
[1] Nanjing Univ Informat & Technol, Nanjing 210044, Jiangsu, Peoples R China
[2] Univ Utah, Dept Atmospher Sci, Salt Lake City, UT 84112 USA
[3] Lanzhou Univ, Coll Atmospher Sci, Lanzhou 73000, Gansu, Peoples R China
[4] Ningxia Meteorol Bur, Ningxia 750002, Peoples R China
基金
美国国家科学基金会;
关键词
HIGH-RESOLUTION SIMULATIONS; TROPICAL CYCLONE INTENSITY; INITIAL CONDITIONS; PART II; MODEL; CONVECTION; ATLANTIC; IMPROVEMENT; DIFFUSION; LANDFALL;
D O I
10.1007/s00376-016-6209-5
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Accurate forecasting of the intensity changes of hurricanes is an important yet challenging problem in numerical weather prediction. The rapid intensification of Hurricane Katrina (2005) before its landfall in the southern US is studied with the Advanced Research version of the WRF (Weather Research and Forecasting) model. The sensitivity of numerical simulations to two popular planetary boundary layer (PBL) schemes, the Mellor-Yamada-Janjic (MYJ) and the Yonsei University (YSU) schemes, is investigated. It is found that, compared with the YSU simulation, the simulation with the MYJ scheme produces better track and intensity evolution, better vortex structure, and more accurate landfall time and location. Large discrepancies (e.g., over 10 hPa in simulated minimum sea level pressure) are found between the two simulations during the rapid intensification period. Further diagnosis indicates that stronger surface fluxes and vertical mixing in the PBL from the simulation with the MYJ scheme lead to enhanced air-sea interaction, which helps generate more realistic simulations of the rapid intensification process. Overall, the results from this study suggest that improved representation of surface fluxes and vertical mixing in the PBL is essential for accurate prediction of hurricane intensity changes.
引用
收藏
页码:482 / 496
页数:15
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