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精细化下垫面对海南地区气象场模拟的影响 被引量:4

Impacts of High-Resolution Land Surface Data on MeteorologicalField Simulation over Hainan
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摘要 使用WRF(Weather Research and Forecasting)模式对2013年海南地区气象场进行了模拟研究,并对比分析使用不同精度的陆面资料[WRF默认的陆面资料(土地利用、植被覆盖度、地形和土壤类型),2013年MODIS(Moderate Resolution Imaging Spectroradiometer)土地利用和植被覆盖度资料,SRTM3(Shuttle Radar Topography Mission)地形资料,HWSD(Harmonized World Soil Database)土壤类型资料]对WRF模式模拟结果的影响。结果表明:采用WRF模式默认或高精度的陆面资料都能够较为准确地模拟出当地气象场的时空分布特征;采用高精度且时效性更好的陆面资料可显著地改进WRF模式对2 m温度和2 m相对湿度的模拟,冬(夏)季的均方根误差(RMSE)分别降低了7.2%(6.5%)和6.1%(7.7%),准确率(HR)分别提高了3.7%(2.8%)和3.2%(2.9%);陆面资料的分辨率及时效性对风场模拟的影响较不敏感,总体上WRF模式仍能较为准确地模拟出研究区域内风场的特征,更新陆面资料后WRF模拟冬(夏)季的风速的RMSE降低了3.8%(4.5%),HR提升了2.1%(2.9%)。 Hainan province which located in the southernmost part of China is an important special economic zone and experimental zone of free trade.However,the studies of underlying surface impact on weather prediction in Hainan is fewer than other places.To understand the impact of underlying surface on numerical weather prediction,the WRF(Weather Research and Forecasting)model is used to simulate the meteorological field over Hainan in 2013.The comparison between default land surface data(land use,vegetation fraction,terrain,and soil type)and new high-resolution land surface data,i.e.Moderate Resolution Imaging Spectroradiometer(MODIS)land use data in 2013 processed based on IGBP(International geosphere biosphere program)classification standard,vegetation fraction data calculated based on MODIS normalized difference vegetation index(NDVI)in 2013,Shuttle Radar Topography Mission 3(SRTM3)terrain data and Harmonized World Soil Database(HWSD)soil type data is investigated through numerical sensitivity tests to analyze the impact on meteorological field simulations.The study is divided into four parts.The first part is the introduction;The second part mainly introduces the research area,data sources,model design and evaluation methods;The third part compares the simulation results of using new high-resolution land surface data with the WRF default land surface data and evaluates the simulation results;Then the fourth part is about the result and discussion.The result indicates that using default or new high-resolution land surface data can both simulate the temporal-spatial distribution of regional meteorological fields.Using the new high-resolution land surface data can improve the simulated results of 2 m temperature and 2 m relative humidity,with the Root Mean Square Error(RMSE)reduced by 7.2%(6.5%)and 6.1%(7.7%)in spring(summer),and the Hit Rate(HR)increased by 3.7%(2.8%)and 3.2%(2.9%)in spring(summer).The impact of high-resolution land surface on 10 m wind speed simulation seems smaller than that on 2 m temperature and 2 m relative humidity.10 m wind speed error reduces slightly after using high-resolution land surface data,with the RMSE reduced by 3.8%(4.5%)and HR increased by 2.1%(2.9%)in spring(summer).Compared to other underlying surface data,land use data has more significant impact on near-surface meteorological fields simulation.In general,using the high-resolution land surface data in Hainan can improve the accuracy of WRF model and reduce the simulation error.This study can deepen the understanding of numerical forecast products for forecasters,improve the accuracy of weather forecast,and provide theoretical basis for Seismic Prevention and Disaster Mitigation.
作者 张晨炜 何建军 赖欣 梁甜 刘奕麟 杨薇 车慧正 龚山陵 ZHANG Chenwei;HE Jianjun;LAI Xin;LIANG Tian;LIU Yilin;YANG Wei;CHE Huizheng;GONG Sunling(School of Atmospheric Sciences,Chengdu University of Information Technology,Chengdu 610225,Sichuan,China;State Key Laboratory of Severe Weather&Key Laboratory of Atmospheric Chemistry of CMA,Chinese Academy of Meteorological Sciences,Beijing 100081,China;School of Geographic Sciences,East China Normal University,Shanghai 200241,China;Meteorological station of Hainan Meteorological Bureau,Haikou 570203,Hainan,China)
出处 《高原气象》 CSCD 北大核心 2022年第3期775-789,共15页 Plateau Meteorology
基金 国家自然科学基金项目(41975131,41705080) 海南省南海气象防灾减灾重点实验室开放基金项目(SCSF201802) 气象灾害教育部重点实验室&气象灾害预报预警与评估协同创新中心开放课题(KLME201804) 中国科学院寒旱区陆面过程与气候变化重点实验室开放基金项目(LPCC2017007)。
关键词 WRF模式 精细化 土地利用 植被覆盖度 模式评估 WRF high-resolution land use vegetation fraction model assessment
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