Assessments of the WRF model in simulating 2021 extreme rainfall episode in Malaysia

被引:2
|
作者
Chen, Yixiao [1 ]
Chan, Andy [2 ]
Ooi, Chei Gee [3 ]
Li, Li [4 ]
Teo, Fang Yenn [1 ]
机构
[1] Univ Nottingham Malaysia, Fac Engn Sci, Jalan Broga, Semenyih 43500, Selangor Darul, Malaysia
[2] Robert Gordon Univ, Sch Engn, Aberdeen AB10 7GJ, Scotland
[3] Univ Kebangsaan Malaysia, Insitute Climate Change, Bangi 43600, Selangor Darul, Malaysia
[4] Shanghai Univ, Sch Environm & Chem Engn, Shanghai 200444, Peoples R China
关键词
WRF model; Extreme rainfall; Flooding; Biomass burning; Tropical depression; Peninsular Malaysia; REGIONAL AIR-QUALITY; ATMOSPHERIC BOUNDARY-LAYER; BIOMASS BURNING HAZE; PARAMETERIZATION SCHEMES; ANTHROPOGENIC AEROSOLS; SOUTHEAST-ASIA; HEAVY RAINFALL; PART I; EMISSIONS; IMPACTS;
D O I
10.1007/s11869-023-01442-w
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
An episode of extreme monsoonal flood event has severely affected the East and West coast of Peninsular Malaysia from 16th to 18th December 2021. The extreme rainfall was documented to be associated to Tropical Depression 29 and Typhoon Rai. In addition, biomass burning aerosols were suspected to be capable of intensifying the precipitation. Thus, the main causes of this extreme event are studied with model evaluation being carried out with biomass burning as one of the possible reasons and variables. From the sensitivity analysis on the PBL scheme for the model physics, QNSE scheme is tested to be the best scheme to simulate the episode compared with MYJ and ACM2 and used in the model assessment. The performances of ARW (WRF-ARW), BB (WRF-Chem with biomass burning), and NOBB (WRF-Chem without biomass burning) have been assessed in the reproduction of the precipitation pattern and tropical depression. Simulation results indicate that ARW shows an overall better performance for most meteorological variables with better performance in reproducing the surface-level pressure and wind speed. Model scenarios of ARW and BB produced similar tropical depression spatial distributions but differ in magnitude, where the tropical depression in ARW is stronger during the study period over East coastline. All models overestimate the precipitation intensity, but ARW is much better correlated with observation data followed by NOBB and BB. The findings show that biomass burning aerosols have only a minor impact on intensifying or delaying the rainfall event. Therefore, tropical depression over Peninsular Malaysia is shown to be the main causation to this extreme event in 2021. The model could be applied for the future flood risk management in Malaysia to provide information on decision making.
引用
收藏
页码:257 / 281
页数:25
相关论文
共 50 条
  • [41] Simulation of an extreme heavy rainfall event over Chennai, India using WRF: Sensitivity to grid resolution and boundary layer physics
    Srinivas, C., V
    Yesubabu, V
    Prasad, D. Had
    Prasad, K. B. R. R. Hari
    Greeshma, M. M.
    Baskaran, R.
    Venkatraman, B.
    ATMOSPHERIC RESEARCH, 2018, 210 : 66 - 82
  • [42] Evaluation of WRF model performance with different microphysics schemes for extreme rainfall prediction in Lagos, Nigeria: Implications for urban flood risk management
    Oluwatobi Oyegbile
    Andy Chan
    Maggie Ooi
    Parvez Anwar
    Abdullahi Ali Mohamed
    Li Li
    Bulletin of Atmospheric Science and Technology, 2024, 5 (1)
  • [43] Extreme Rainfall Projections for Malaysia at the End of 21st Century Using the High Resolution Non-Hydrostatic Regional Climate Model (NHRCM)
    Ngai, Sheau Tieh
    Sasaki, Hidetaka
    Murata, Akihiko
    Nosaka, Masaya
    Chung, Jing Xiang
    Juneng, Liew
    Supari
    Salimun, Ester
    Tangang, Fredolin
    SOLA, 2020, 16 : 132 - 139
  • [44] Simulating Arctic Ice Clouds during Spring Using an Advanced Ice Cloud Microphysics in the WRF Model
    Keita, Setigui Aboubacar
    Girard, Eric
    Raut, Jean-Christophe
    Pelon, Jacques
    Blanchet, Jean-Pierre
    Lemoine, Olivier
    Onishi, Tatsuo
    ATMOSPHERE, 2019, 10 (08)
  • [45] An evaluation of the WRF physical parameterizations for extreme rainfall simulation in the Yangtze River Middle Reaches Urban Agglomeration
    Luo, Yuhua
    Zhang, Ming
    Cao, Qian
    Wang, Lunche
    URBAN CLIMATE, 2024, 58
  • [46] Numerical Simulations of Heavy Rainfall over Central Korea on 21 September 2010 Using the WRF Model
    Ui-Yong BYUN
    Jinkyu HONG
    Song-You HONG
    Hyeyum Hailey SHIN
    Advances in Atmospheric Sciences, 2015, 32 (06) : 855 - 869
  • [47] A Possible Dynamic Mechanism for Rapid Production of the Extreme Hourly Rainfall in Zhengzhou City on 20 July 2021
    Yin, Jinfang
    Gu, Haodong
    Liang, Xudong
    Yu, Miao
    Sun, Jisong
    Xie, Yanxin
    Li, Feng
    Wu, Chong
    JOURNAL OF METEOROLOGICAL RESEARCH, 2022, 36 (01) : 6 - 25
  • [48] Numerical simulations of heavy rainfall over central Korea on 21 September 2010 using the WRF model
    Ui-Yong Byun
    Jinkyu Hong
    Song-You Hong
    Hyeyum Hailey Shin
    Advances in Atmospheric Sciences, 2015, 32 : 855 - 869
  • [49] Numerical simulations of heavy rainfall over central Korea on 21 September 2010 using the WRF model
    Byun, Ui-Yong
    Hong, Jinkyu
    Hong, Song-You
    Shin, Hyeyum Hailey
    ADVANCES IN ATMOSPHERIC SCIENCES, 2015, 32 (06) : 855 - 869
  • [50] Evaluation of WRF Microphysics and Cumulus Parameterization Schemes in simulating a heavy rainfall event over Yangtze River Delta
    Kan, Yu
    Liu, Chaoshun
    Liu, Yanan
    Zhou, Cong
    REMOTE SENSING AND MODELING OF ECOSYSTEMS FOR SUSTAINABILITY XII, 2015, 9610