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1.
基于高分辨率数值模式的特点,为了弥补传统站点对站点等检验方法的不足,采用基于目标诊断的空间检验方法 MODE,对上海快速更新同化系统预报的2014年3月19日强对流降水和冰雹雷达回波进行了客观检验。该方法通过在空间场中识别目标,综合考虑了空间位置、形状、面积等多种因素,采用模糊逻辑算法计算预报和观测目标的相似度。结果表明,MODE在高分辨率数值模式检验中比传统方法具有明显的优势,尤其针对雷达回波的检验有较高的实际应用价值。同时讨论了MODE方法卷积平滑半径参数的选取对高分辨模式检验结果的影响。  相似文献   

2.
鲁小琴  余晖  赵兵科 《气象》2013,39(12):1609-1615
比较了欧氏距离、相似离度、相似系数、相关系数及最优相似系数等作为气象格点场相似性度量的适用性,结果发现以“距离”为主的算法无法准确地反映环境场中的一些特定系统的位置和强度,相似检索效果较差;而相似离度、相似系数、相关系数及最优相似系数可分别考虑两个场之间的形状和强度、空间分布及变化趋势,能找到较相似的场,可供业务参考。通过将不同指标检索到的相似环境场的演变对热带气旋(Tropical Cyclone,TC)路径的影响量引入到TC路径预报中,检验其业务应用效果,发现单纯移向的预报效果好于路径预报,路径预报中相似离度的效果稍好于其他方法,而移向预报中最优系数法最好。另通过相似环境场检索,能找到由相似环境场所对应的相似历史TC,并依据不同度量性指标得到一个历史相似TC集,为台风业务、科研提供参考。  相似文献   

3.
用MICAPS平台中的T213产品场与暴雨发生的初始、中间、结束过程相对应的三维空间物理量场的相似程度,根据场相似的数量综合判别分析作出有无区域暴雨的预报。预报因子选取涡度、散度、垂直速度和水汽通量散度,空间使用850、700、500hPa,时间上选取12、24、36h预报场。该方法实现了区域暴雨预报的客观化和程序化。根据天气过程分类建立的两类模型以场平均距离为依据,作出的暴雨预报检验效果令人满意,2004—2010年的5—10月7年平均预报准确率超过33%,具有较好的实践参考指导作用。  相似文献   

4.
基于对象的诊断检验方法(MODE)受降水临界值、卷积半径、属性权重等参数的影响,合理选取卷积半径并准确表征预报场与观测场之间的空间相似度决定了MODE的应用效果。本文基于2020年夏季贵州54个降水个例,以多源融合降水(CMPA)作为实况,使用MODE和FSS评分(Fractions Skill Score)对中国气象局广东快速更新同化数值预报系统(CMA GD)24 h日降水预报进行空间检验。结果表明:卷积半径过小易造成MODE提取降水对象过多,而卷积半径过大则导致局部降水信息丢失,无法从降水场中提取到降水对象。不同卷积半径下计算的最大相似度中值(MMI)存在突变。在MMI基础上引入面积权重构造面积平均最大相似度(AMMI)。AMMI不受提取降水对象个数的影响,较MMI更具有稳定性,用于表征降水场之间的整体空间相似程度更为合理。根据对象总面积随卷积半径的变化将降水分为大范围降水和局部降水2类。大范围降水平均总面积随着卷积半径的增加而增加,AMMI随卷积半径变化不大。随着卷积半径的增加,局部降水平均总面积减小,平均AMMI有所减小。局部降水对卷积半径选取较为敏感,以观测场对象面积变化不超过10%的最大半径作为卷积半径有助于保留降水场大部分信息。  相似文献   

5.
检验全球数值预报模式的相似度等指标   总被引:1,自引:1,他引:0  
朱娟  张立凤  张铭 《气象科学》2018,38(2):221-228
本文依照泛函形式并考虑了球面经纬网格的特点,定义了用于全球数值模式效果检验的指标:距离、距平相似度和倾向相似度,给出了相应的计算方法,并以全球WRF模式为例,检验了该模式的中期预报效果。所得结论如下:指标距离、距平相似度和倾向相似度物理意义明确,易于理论分析,考虑了球面经纬网格的特点,检验准确度高,具有普适性,能方便应用于球面经纬网格输出的数值模式检验。指标距离、距平相似度的检验结果分别与传统检验指标均方根误差、距平相关系数相一致,该指标还可直接用于向量场(如风场)的整体检验。本文的全球WRF模式所做的检验表明,对本文个例,该模式的全球500 hPa中期天气形势预报在第7 d及之内皆可用,5 d及之内预报效果更佳。  相似文献   

6.
利用1975-2005年NCEP再分析资料及ECMWF预报场资料,引入相似指数综合考虑各要素场、形势场对新疆强降水天气的影响建立相似预报模型,并选取一次中等强度天气用该模型进行试报检验。结果表明,该模型综合考虑了形势场、多种物理量场的相互作用,预报效果较好。  相似文献   

7.
强度尺度方法在模式定量降水预报检验中的应用   总被引:1,自引:0,他引:1  
介绍了Casati于2004年提出的强度尺度检验技术,并将该方法应用到上海区域中尺度模式的预报检验中。结果表明,强度尺度检验技术可以提供一种从不同降水率闽值和空间尺度对模式定量降水预报进行评估的方案。该方法首先对预报场和观测场进行降水率闽值获得二进制误差场,并通过二维离散Haar小波对二进制误差场进行各个空间尺度的分解,从而评估模式在各个降水率闯值和空间尺度上的均方差和预报技巧。通过计算各空间尺度二进制误差场的均方差百分比和能量平方偏差,可分析不同的降水特征尺度误差对总体误差的贡献情况以及预报降水与观测的偏差情况。  相似文献   

8.
多时次多尺度波谱相似预报风要素   总被引:3,自引:2,他引:1  
毛卫星  许晨海  何立富  刘还珠 《气象》2005,31(10):28-31
利用1975~2004年500hPa高度和850hPa温度格点场的历史资料,分别计算出不同纬度带的超长波和长波合成波,以此作为风要素预报的基本资料。根据谐波分析原理,结合相似系数法和相似距离法建立一套多时次、多尺度波谱相似预报模型,并提出相似离度概念。经过近两年的运行试验,该预报模型运行稳定,检验结果表明,对于由风压定律制约的风要素预报具有较大的参考作用,在大尺度天气形势控制下,与当地地形、地貌结合形成的风要素预报不失为一种简便易行的风向风速预报方法。利用多时次多尺度动态相似法制作风要素预报既考虑了物理量场不同尺度的空间相似,又考虑了连续时间的过程相似,因此这对中期天气过程的预报是有意义的。  相似文献   

9.
不同类型强对流预报产品的目标对象检验与分析评价   总被引:2,自引:1,他引:1  
茅懋  戴建华  李佰平  张欣 《气象》2016,42(4):389-397
针对强对流天气时空尺度小的特点、对其预报需要关注多种要素的需求,为了挖掘预报的潜在价值,设计了目标对象检验方法:首先,分别在预报和实况中识别出强度、面积符合一定匹配条件的目标对象单体(如对流单体、强天气落区等);然后,根据识别目标对象的面积、空间距离、形态进行预报和实况间的对象匹配;接着,对预报目标对象进行等级TS评分、等级面积大小、重心偏移、交叉相关、形状对比(轴向和椭圆率)等五项指标的检验;最后,依据用户评价偏好,采用加权平均方法给出总体检验评分和面积、位置、形状方面的评价信息。通过对中国气象局短临预报业务系统SWAN等业务系统的三类短临预报业务产品(REF、QPF、对流概率预报)的检验表明:该检验方法能够量化评价预报对象在面积、位置或强度等要素上的吻合程度及对应的偏差,给出导致常规检验评分(如TS评分)较低的原因,并综合这些要素给出针对用户的评价,为预报人员提供了更多有效的检验评估信息,实现对多种类型强对流预报产品的综合检验和评价。  相似文献   

10.
基于数据库技术的 T213 产品场相似释用方法   总被引:2,自引:0,他引:2  
该文根据新业务预报流程的要求,在 MICAPS 平台中用 T213/T106 产品作场相似解释应用,制作实现了分县站点降水预报的方法.T213/T106产品要素选定了 26 个场.使用了数据库技术将 1994-2000 年共 7 a 的历史常规观测资料分析场进行存储.数据库技术可以快速地进行场相似系数的计算、排序比较和过程查找.运用相似预报原理将数值产品场到历史分析库中去查找相似的办法确定相似过程.在预报制作时设计了两种相似预报方案的输出.从全年 11 个月的评分检验来看,各站点均有 10 个月的 SS1>0,而且多数月份的 SS1 具有较高的值.可以看出该方法具有较好的客观性、稳定性及预报效果.该方法已经投入贵州省黔东南州气象台的业务运行.  相似文献   

11.
The spatial and temporal variations of daily maximum temperature(Tmax), daily minimum temperature(Tmin), daily maximum precipitation(Pmax) and daily maximum wind speed(WSmax) were examined in China using Mann-Kendall test and linear regression method. The results indicated that for China as a whole, Tmax, Tmin and Pmax had significant increasing trends at rates of 0.15℃ per decade, 0.45℃ per decade and 0.58 mm per decade,respectively, while WSmax had decreased significantly at 1.18 m·s~(-1) per decade during 1959—2014. In all regions of China, Tmin increased and WSmax decreased significantly. Spatially, Tmax increased significantly at most of the stations in South China(SC), northwestern North China(NC), northeastern Northeast China(NEC), eastern Northwest China(NWC) and eastern Southwest China(SWC), and the increasing trends were significant in NC, SC, NWC and SWC on the regional average. Tmin increased significantly at most of the stations in China, with notable increase in NEC, northern and southeastern NC and northwestern and eastern NWC. Pmax showed no significant trend at most of the stations in China, and on the regional average it decreased significantly in NC but increased in SC, NWC and the mid-lower Yangtze River valley(YR). WSmax decreased significantly at the vast majority of stations in China, with remarkable decrease in northern NC, northern and central YR, central and southern SC and in parts of central NEC and western NWC. With global climate change and rapidly economic development, China has become more vulnerable to climatic extremes and meteorological disasters, so more strategies of mitigation and/or adaptation of climatic extremes,such as environmentally-friendly and low-cost energy production systems and the enhancement of engineering defense measures are necessary for government and social publics.  相似文献   

12.
Storms that occur at the Bay of Bengal (BoB) are of a bimodal pattern, which is different from that of the other sea areas. By using the NCEP, SST and JTWC data, the causes of the bimodal pattern storm activity of the BoB are diagnosed and analyzed in this paper. The result shows that the seasonal variation of general atmosphere circulation in East Asia has a regulating and controlling impact on the BoB storm activity, and the “bimodal period” of the storm activity corresponds exactly to the seasonal conversion period of atmospheric circulation. The minor wind speed of shear spring and autumn contributed to the storm, which was a crucial factor for the generation and occurrence of the “bimodal pattern” storm activity in the BoB. The analysis on sea surface temperature (SST) shows that the SSTs of all the year around in the BoB area meet the conditions required for the generation of tropical cyclones (TCs). However, the SSTs in the central area of the bay are higher than that of the surrounding areas in spring and autumn, which facilitates the occurrence of a “two-peak” storm activity pattern. The genesis potential index (GPI) quantifies and reflects the environmental conditions for the generation of the BoB storms. For GPI, the intense low-level vortex disturbance in the troposphere and high-humidity atmosphere are the sufficient conditions for storms, while large maximum wind velocity of the ground vortex radius and small vertical wind shear are the necessary conditions of storms.  相似文献   

13.
Observed daily precipitation data from the National Meteorological Observatory in Hainan province and daily data from the National Centers for Environmental Prediction/National Center for Atmospheric Research (NCEP/NCAR) reanalysis-2 dataset from 1981 to 2014 are used to analyze the relationship between Hainan extreme heavy rainfall processes in autumn (referred to as EHRPs) and 10–30 d low-frequency circulation. Based on the key low-frequency signals and the NCEP Climate Forecast System Version 2 (CFSv2) model forecasting products, a dynamical-statistical method is established for the extended-range forecast of EHRPs. The results suggest that EHRPs have a close relationship with the 10–30 d low-frequency oscillation of 850 hPa zonal wind over Hainan Island and to its north, and that they basically occur during the trough phase of the low-frequency oscillation of zonal wind. The latitudinal propagation of the low-frequency wave train in the middle-high latitudes and the meridional propagation of the low-frequency wave train along the coast of East Asia contribute to the ‘north high (cold), south low (warm)’ pattern near Hainan Island, which results in the zonal wind over Hainan Island and to its north reaching its trough, consequently leading to EHRPs. Considering the link between low-frequency circulation and EHRPs, a low-frequency wave train index (LWTI) is defined and adopted to forecast EHRPs by using NCEP CFSv2 forecasting products. EHRPs are predicted to occur during peak phases of LWTI with value larger than 1 for three or more consecutive forecast days. Hindcast experiments for EHRPs in 2015–2016 indicate that EHRPs can be predicted 8–24 d in advance, with an average period of validity of 16.7 d.  相似文献   

14.
Based on the measurements obtained at 64 national meteorological stations in the Beijing–Tianjin–Hebei (BTH) region between 1970 and 2013, the potential evapotranspiration (ET0) in this region was estimated using the Penman–Monteith equation and its sensitivity to maximum temperature (Tmax), minimum temperature (Tmin), wind speed (Vw), net radiation (Rn) and water vapor pressure (Pwv) was analyzed, respectively. The results are shown as follows. (1) The climatic elements in the BTH region underwent significant changes in the study period. Vw and Rn decreased significantly, whereas Tmin, Tmax and Pwv increased considerably. (2) In the BTH region, ET0 also exhibited a significant decreasing trend, and the sensitivity of ET0 to the climatic elements exhibited seasonal characteristics. Of all the climatic elements, ET0 was most sensitive to Pwv in the fall and winter and Rn in the spring and summer. On the annual scale, ET0 was most sensitive to Pwv, followed by Rn, Vw, Tmax and Tmin. In addition, the sensitivity coefficient of ET0 with respect to Pwv had a negative value for all the areas, indicating that increases in Pwv can prevent ET0 from increasing. (3) The sensitivity of ET0 to Tmin and Tmax was significantly lower than its sensitivity to other climatic elements. However, increases in temperature can lead to changes in Pwv and Rn. The temperature should be considered the key intrinsic climatic element that has caused the "evaporation paradox" phenomenon in the BTH region.  相似文献   

15.
正The Taal Volcano in Luzon is one of the most active and dangerous volcanoes of the Philippines. A recent eruption occurred on 12 January 2020(Fig. 1a), and this volcano is still active with the occurrence of volcanic earthquakes. The eruption has become a deep concern worldwide, not only for its damage on local society, but also for potential hazardous consequences on the Earth's climate and environment.  相似文献   

16.
The moving-window correlation analysis was applied to investigate the relationship between autumn Indian Ocean Dipole (IOD) events and the synchronous autumn precipitation in Huaxi region, based on the daily precipitation, sea surface temperature (SST) and atmospheric circulation data from 1960 to 2012. The correlation curves of IOD and the early modulation of Huaxi region’s autumn precipitation indicated a mutational site appeared in the 1970s. During 1960 to 1979, when the IOD was in positive phase in autumn, the circulations changed from a “W” shape to an ”M” shape at 500 hPa in Asia middle-high latitude region. Cold flux got into the Sichuan province with Northwest flow, the positive anomaly of the water vapor flux transported from Western Pacific to Huaxi region strengthened, caused precipitation increase in east Huaxi region. During 1980 to 1999, when the IOD in autumn was positive phase, the atmospheric circulation presented a “W” shape at 500 hPa, the positive anomaly of the water vapor flux transported from Bay of Bengal to Huaxi region strengthened, caused precipitation ascend in west Huaxi region. In summary, the Indian Ocean changed from cold phase to warm phase since the 1970s, caused the instability of the inter-annual relationship between the IOD and the autumn rainfall in Huaxi region.  相似文献   

17.
正While China’s Air Pollution Prevention and Control Action Plan on particulate matter since 2013 has reduced sulfate significantly, aerosol ammonium nitrate remains high in East China. As the high nitrate abundances are strongly linked with ammonia, reducing ammonia emissions is becoming increasingly important to improve the air quality of China. Although satellite data provide evidence of substantial increases in atmospheric ammonia concentrations over major agricultural regions, long-term surface observation of ammonia concentrations are sparse. In addition, there is still no consensus on  相似文献   

18.
基于最新的GTAP8 (Global Trade Analysis Project)数据库,使用投入产出法,分析了2004年到2007年全球贸易变化下南北集团贸易隐含碳变化及对全球碳排放的影响。结果显示,随着发展中国家进出口规模扩张,全球贸易隐含碳流向的重心逐渐向发展中国家转移。2004年到2007年,发达国家高端设备制造业和服务业出口以及发展中国家资源、能源密集型行业及中低端制造业出口的趋势加强,该过程的生产转移导致全球碳排放增长4.15亿t,占研究时段全球贸易隐含碳增量的63%。未来发展中国家的出口隐含碳比重还将进一步提高。贸易变化带来的南北集团隐含碳流动变化对全球应对气候变化行动的影响日益突出,发达国家对此负有重要责任。  相似文献   

19.
Using the International Comprehensive Ocean-Atmosphere Data Set(ICOADS) and ERA-Interim data, spatial distributions of air-sea temperature difference(ASTD) in the South China Sea(SCS) for the past 35 years are compared,and variations of spatial and temporal distributions of ASTD in this region are addressed using empirical orthogonal function decomposition and wavelet analysis methods. The results indicate that both ICOADS and ERA-Interim data can reflect actual distribution characteristics of ASTD in the SCS, but values of ASTD from the ERA-Interim data are smaller than those of the ICOADS data in the same region. In addition, the ASTD characteristics from the ERA-Interim data are not obvious inshore. A seesaw-type, north-south distribution of ASTD is dominant in the SCS; i.e., a positive peak in the south is associated with a negative peak in the north in November, and a negative peak in the south is accompanied by a positive peak in the north during April and May. Interannual ASTD variations in summer or autumn are decreasing. There is a seesaw-type distribution of ASTD between Beibu Bay and most of the SCS in summer, and the center of large values is in the Nansha Islands area in autumn. The ASTD in the SCS has a strong quasi-3a oscillation period in all seasons, and a quasi-11 a period in winter and spring. The ASTD is positively correlated with the Nio3.4 index in summer and autumn but negatively correlated in spring and winter.  相似文献   

20.
Hourly outgoing longwave radiation(OLR) from the geostationary satellite Communication Oceanography Meteorological Satellite(COMS) has been retrieved since June 2010. The COMS OLR retrieval algorithms are based on regression analyses of radiative transfer simulations for spectral functions of COMS infrared channels. This study documents the accuracies of OLRs for future climate applications by making an intercomparison of four OLRs from one single-channel algorithm(OLR12.0using the 12.0 μm channel) and three multiple-channel algorithms(OLR10.8+12.0using the 10.8 and 12.0 μm channels; OLR6.7+10.8using the 6.7 and 10.8 μm channels; and OLR All using the 6.7, 10.8, and 12.0 μm channels). The COMS OLRs from these algorithms were validated with direct measurements of OLR from a broadband radiometer of the Clouds and Earth's Radiant Energy System(CERES) over the full COMS field of view [roughly(50°S–50°N, 70°–170°E)] during April 2011.Validation results show that the root-mean-square errors of COMS OLRs are 5–7 W m-2, which indicates good agreement with CERES OLR over the vast domain. OLR6.7+10.8and OLR All have much smaller errors(~ 6 W m-2) than OLR12.0and OLR10.8+12.0(~ 8 W m-2). Moreover, the small errors of OLR6.7+10.8and OLR All are systematic and can be readily reduced through additional mean bias correction and/or radiance calibration. These results indicate a noteworthy role of the6.7 μm water vapor absorption channel in improving the accuracy of the OLRs. The dependence of the accuracy of COMS OLRs on various surface, atmospheric, and observational conditions is also discussed.  相似文献   

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