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Temporal and Spatial Distribution Characteristics of CO Total Column over China Based on TROPOMI Measurements 基于TROPOMI测量的中国CO总柱时空分布特征
Pub Date : 2019-12-28 DOI: 10.1109/ICMO49322.2019.9076588
Yuping Ji, Xiaobo Deng, Hailei Liu, Qihong Huang, Ke Zhou, Yuyu Tao
With the global warming, CO (carbon monoxide) as an indirect greenhouse gas, plays a crucial role in the contribution of greenhouse effect. High concentration of CO in the air will do harm to people's health. Based on the CO total column data detected by the Tropospheric Monitoring Instrument (TROPOMI) on Sentinel-5 Precursor satellite, which was launched by the European Space Agency (ESA) on 13 October 2017. This study analyzes the seasonal variable characteristics of the CO total column from June 2018 to May 2019 in China and the spatial distribution of the CO total column in North China, Central China, Sichuan Basin, Qinghai-Tibet Plateau and Pearl River Delta. The high values areas are mainly located in the eastern part of China with high population activity and developed industry, while the Qinghai- Tibet Plateau area and the northwest area are generally low. Selecting the area where the CO total column was significantly enhanced in Hebei province on 24 May, 2018, and monitoring the pollution in the following days. The results show that the TROPOMI data product is a good way to show the source of pollution and has the ability to detect local hot spots.
随着全球气候变暖,CO(一氧化碳)作为一种间接温室气体,对温室效应的贡献起着至关重要的作用。空气中高浓度的一氧化碳会对人的健康有害。基于欧洲航天局(ESA)于2017年10月13日发射的Sentinel-5前驱卫星对流层监测仪器(TROPOMI)探测到的CO总柱数据。本研究分析了2018年6月- 2019年5月中国CO总柱的季节变化特征,以及华北、华中、四川盆地、青藏高原和珠江三角洲CO总柱的空间分布。高值区主要分布在人口活跃、工业发达的东部地区,而青藏高原地区和西北地区则普遍偏低。选取2018年5月24日河北省CO总柱显著增强的区域,监测其后几天的污染情况。结果表明,TROPOMI数据产品是一种很好的显示污染源的方法,具有检测局部热点的能力。
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引用次数: 0
Comparative analysis of soil moisture based on model simulation and site observation data 基于模型模拟与现场观测资料的土壤湿度对比分析
Pub Date : 2019-12-28 DOI: 10.1109/ICMO49322.2019.9076593
Xin Zhang, L. Cao, Yida Wang, Zhendong Yao, Shuling Li, Jiliang Han
It is of great significance to accurately and objectively evaluate the spatial and temporal variation characteristics of soil moisture in studies Heilongjiang Region. Combining model simulation and site observation is necessary to studying water and energy recycling at a regional scale especially. In this paper, Using the soil moisture observation at 0~10 cm layer from the automatic soil moisture monitoring stations and Manual observation data as a guide. Based on the surface soil moisture data of 10 cm provided by CLDAS-V2.0 ( CMA Land Data Assimilation System Version2.0 ) developed by the National Meteorological Information Center, the spatiotemporal difference of model simulated data in Heilongjiang province was compared and analyzed. The correlation coefficient(R), mean relative deviation, root-meansquare error (RMSE), mean relative error (MRE) and mean absolute error (MAE)of the simulated data and the observed data were calculated, Comprehensive evaluation the applicability of soil moisture data from simulated data in Heilongjiang Region. In this paper using soil data in the main growth period of crops, summer is selected as the research period for preliminary evaluation and analysis, The research period is from May to August,2018 to 2019, the time series length was 244days. Using the NetCDF toolbox of ArcGIS to get 0 ~ 10 cm soil moisture data of the grid where the observation station is located by CLDAS-V2.0. The results showed that: Although the data from model products were generally slightly higher than the observation data, station observation and model products data show a good consistency. The paper would help us make effective use of model products in soil moisture related studies with a view to testing CLDAS V2.0 for Ability to describe soil humidity.
准确、客观地评价黑龙江地区土壤水分时空变化特征具有重要意义。在区域尺度上研究水能循环尤其需要模型模拟与现场观测相结合。本文以自动土壤水分监测站0~10 cm层土壤水分观测资料和人工观测资料为指导。利用国家气象信息中心开发的CLDAS-V2.0 (CMA Land data Assimilation System Version2.0)提供的10 cm表层土壤水分数据,对比分析了黑龙江省模式模拟数据的时空差异。计算模拟数据与观测数据的相关系数(R)、平均相对偏差、均方根误差(RMSE)、平均相对误差(MRE)和平均绝对误差(MAE),综合评价模拟数据在黑龙江地区土壤湿度数据的适用性。本文利用作物主生期土壤数据,选择夏季作为研究期进行初步评价分析,研究期为2018 - 2019年5 - 8月,时间序列长度为244天。利用ArcGIS的NetCDF工具箱,利用CLDAS-V2.0软件获取观测站所在网格0 ~ 10 cm土壤湿度数据。结果表明:虽然模型产品数据普遍略高于观测数据,但站内观测数据与模型产品数据具有较好的一致性。本文将有助于我们在土壤湿度相关研究中有效地利用模型产品,以期测试CLDAS V2.0对土壤湿度的描述能力。
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引用次数: 0
Research and Application of Meteorological Data Transmission System Based on Virtual Desktop 基于虚拟桌面的气象数据传输系统研究与应用
Pub Date : 2019-12-28 DOI: 10.1109/ICMO49322.2019.9076591
Wang Lizhu, Guo Zhongli, Zhu Qian, Wu Peng, Ma Shangchang, Zhang Sujuan, Wang Min
With the development of meteorological information and the improvement of social demand for meteorology, the meteorological industry has also introduced cloud computing technology, among which the virtual desktop, as the key technology of cloud computing, has been gradually promoted and used in the meteorological service system. Based on virtual desktop technology and taking the transmission system of national surface meteorological observation station in Henan province as an example, this paper proposes a meteorological data transmission system based on virtual desktop by analyzing the problems existing in the data flow of traditional architecture. This paper expounds the design and application of the system, the economic benefit, the reliability and security of the system and the business benefit of the system, thus demonstrating the feasibility of the new architecture data flow based on virtual desktop in the meteorological business system. Virtual desktop will bring new innovation and impetus to the meteorological system, and cloud computing technology will also provide powerful technical support and guarantee for the meteorological business, providing reliable, stable and safe technical solutions and support for the development and construction of meteorological information in Henan province and the whole country.
随着气象信息的发展和社会对气象需求的提高,气象行业也引入了云计算技术,其中虚拟桌面作为云计算的关键技术,在气象服务系统中得到了逐步推广和应用。本文以虚拟桌面技术为基础,以河南省国家地面气象观测站传输系统为例,通过分析传统架构中数据流存在的问题,提出了一种基于虚拟桌面的气象数据传输系统。本文阐述了系统的设计与应用、系统的经济效益、系统的可靠性与安全性以及系统的业务效益,从而论证了基于虚拟桌面的新架构数据流在气象业务系统中的可行性。虚拟桌面将为气象系统带来新的创新和动力,云计算技术也将为气象业务提供强大的技术支撑和保障,为河南省乃至全国气象信息化发展建设提供可靠、稳定、安全的技术解决方案和支撑。
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引用次数: 1
A Study of Solar Method Azimuth 太阳方法方位角的研究
Pub Date : 2019-12-28 DOI: 10.1109/ICMO49322.2019.9085307
Wang Xin, Zhang Fugui, W. Xuejun, Zhou Honggen
The antenna performance parameter of weather radar, an extremely significant part of radar constant, which directly influences the measurement accuracy of radar echo intensity. Therefore, antenna test always be considered as an important step in radar inspection and calibration. But, a high placement position required to the new generation weather radar and a iron tower installation needed to the far-field test, are always both brings great inconvenience in the regular or irregular examination of antenna. This paper discusses the method of testing weather radar antenna by using the sun as a signal source, relevant principles or methods in detail, and algorithm of solar optical angular diameter. Improves the solar method azimuth beam width correction algorithm through analyzing the phonomenon that the azimuth beam width changed with the solar elevation angle in solar method. Analyzes the measurement error and accuracy of the sun method by measuring a antenna of X-band weather radar in Chengdu University of Information Technology. The results show that the antenna beam width measurement becomes more stable and the measurement accuracy shows greatly improved by using the azimuth beam width correction algorithm in solar method. Compared with the antenna far-field test, the solar method presents the advantages of low cost, simple operation and high measurement accuracy, and has a wide application prospect in the field of weather radar antenna testing.
气象雷达的天线性能参数是雷达常数中极为重要的组成部分,它直接影响雷达回波强度的测量精度。因此,天线测试一直被认为是雷达检测和校准的重要步骤。但是,新一代气象雷达需要较高的放置位置和远场测试需要铁塔的安装,都给天线的定期或不定期检查带来了极大的不便。本文详细论述了以太阳为信号源测试气象雷达天线的方法、相关原理或方法,以及太阳光学角直径的计算方法。通过分析太阳法方位波束宽度随太阳仰角变化的现象,改进了太阳法方位波束宽度校正算法。通过对成都信息工程大学某x波段气象雷达天线的测量,分析了太阳法的测量误差和精度。结果表明,采用太阳法中的方位角波束宽度校正算法后,天线波束宽度测量更加稳定,测量精度大大提高。与天线远场测试相比,太阳法具有成本低、操作简单、测量精度高等优点,在气象雷达天线测试领域具有广阔的应用前景。
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引用次数: 0
The Linkages between Atmospheric Boundary Layer and PM 2.5 from Different Region in China 中国不同区域大气边界层与pm2.5的关系
Pub Date : 2019-12-01 DOI: 10.1109/ICMO49322.2019.9026117
Mengyun Lou, Qing Zhou, J. Jin, Yanfen Peng, Rui Dai, Yong Zhang, Jianping Guo
Planetary boundary layer (PBL) – aerosol interaction is one of a major causes for the deterioration of air quality. Elucidating the relationship between pollution–PBL becomes essential for improving the prediction of air quality. Ground-based air quality and meteorological data, in combination with L-band high resolution (1-sec) radiosonde measurements from 2014 to 2017, were used to study the fine structures of PBL, and the correlations between boundary layer height (BLH) and PM2.5 from different region in China.There is a significant difference in the PBL–PM2.5 interaction in different regions. On the inner-annual timescale, the strongest negative correlation is observed over the North China Plain (NCP) with highly polluted conditions, followed by the Yangtze River Delta (YRD). Meanwhile, the air quality of Qinghai-Tibet Plateau (TBP) is relatively clean, where it shows the lowest negative correlation coefficient. The correlation coefficient are 0.34, -0.25 and -0.18 for the NCP, the YRD and the TBP. In the heavily polluted region, the pollutant–PBL–meteorology is closely related, indicating that their interaction is most obvious. Under clean conditions, no distinct interaction can be found between BLH and PM2.5 in the TBP, whereas the meteorological conditions show a greater impact on the development of PBL.The PBL-pollution interaction depends in the degree of pollution and the background value of BLHs, and the relationship between PM2.5 and BLHs is nonlinear, which is more obvious with high concentration of pollutants or the low BLHs. Of course, this relationship is also significantly affected by other meteorological variables.
行星边界层与气溶胶的相互作用是导致大气质量恶化的主要原因之一。阐明污染与pbl之间的关系对于改善空气质量的预测至关重要。利用2014 - 2017年的地面空气质量和气象资料,结合l波段高分辨率(1秒)探空测量,研究了中国不同地区边界层的精细结构,以及边界层高度(BLH)与PM2.5的相关性。不同地区的PBL-PM2.5相互作用存在显著差异。在年内时间尺度上,华北平原(NCP)的负相关最强,其次是长江三角洲(YRD)。与此同时,青藏高原(TBP)空气质量相对清洁,负相关系数最低。NCP、YRD和TBP的相关系数分别为0.34、-0.25和-0.18。在重污染地区,污染物-多氯联苯-气象关系密切,相互作用最为明显。在清洁条件下,TBP中BLH与PM2.5之间没有明显的相互作用,气象条件对PBL的发展影响较大。pbl与污染的相互作用取决于污染程度和blh的背景值,PM2.5与blh的关系是非线性的,在污染物浓度较高或blh较低时更为明显。当然,这种关系也受到其他气象变量的显著影响。
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引用次数: 0
Research on the Calibration Technology of Visibility Based on Artificial Simulated Environment 基于人工模拟环境的能见度标定技术研究
Pub Date : 2019-12-01 DOI: 10.1109/ICMO49322.2019.9025897
Jinhua Chu, X. Tang, Hua Wang
Visibility is one of the basic elements of ground meteorological observation, which has an important impact on aviation, navigation, road traffic and military activities. There is no uniform test environment and reference standard in the calibration of forward scattering visibility meter, which leads to great difference in measurement results. This paper introduces a calibration method of visibility meter based on artificial simulated environment, and develops a visibility environment simulated square cabin, which can achieve artificial simulated visibility from 10m to 30km by using ultrasonic fog making and air purification technology. Furthermore, the air circulation technology is used to accelerate the water vapor mixing and eliminate the error caused by the water mist inhomogeneity. The transmission visibility measurement system is taken as the reference standard and the forward scattering visibility meter system constant is calibrated. Finally, the visibility calibration in the range of 50m ~ 10 km is realized. The analysis shows that the horizontal visibility nonuniformity of the shelter is between-1.7 % ~ 1.8 %, which meets the environmental requirements for calibration of forward scattering visibility meter. In the simulated visibility range of 50 m~10 km, the relative error of visibility measurement between the calibrated forward scattering visibility meter and the reference standard is between -1.6 % ~ 5.1 %, and controlled within ± 10 %.
能见度是地面气象观测的基本要素之一,对航空、航海、道路交通和军事活动具有重要影响。前向散射能见度仪的标定没有统一的测试环境和参考标准,导致测量结果差异较大。本文介绍了一种基于人工模拟环境的能见度计标定方法,并研制了一种能见度环境模拟方舱,利用超声波造雾和空气净化技术,可实现10m ~ 30km的人工模拟能见度。此外,采用空气循环技术加速水蒸气混合,消除水雾不均匀性带来的误差。以透射式能见度测量系统为参考标准,对前向散射式能见度仪系统常数进行标定。最后,实现了50m ~ 10km范围内的能见度标定。分析表明,掩体水平能见度不均匀性在- 1.7% ~ 1.8%之间,满足前向散射能见度仪标定的环境要求。在50 m~10 km的模拟能见度范围内,标定后的前向散射能见度仪与参考标准的相对误差在- 1.6% ~ 5.1%之间,控制在±10%以内。
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引用次数: 1
Interference Suppression Based on Single-channel Blind Source Separation in Weather Radar 基于气象雷达单通道盲源分离的干扰抑制
Pub Date : 2019-12-01 DOI: 10.1109/ICMO49322.2019.9025992
Chuanzhi Wang, Xiaohua Zhu, Xuehua Li
The interference suppression is an eternal issue in radar system. In this paper, we first proposed a novel single-channel blind source separation (SBSS) algorithm which overcomes the limitation of traditional BSS method, and then the novel SBSS algorithm was performed to weather radar in interference suppression. The proposed SBSS method is inspired by the recently proposed variational mode decomposition (VMD) and the theory of sparse component analysis (SCA). The VMD algorithm was implemented to decompose the single-channel signal into two-channel signals and the improved SCA method was utilized to signal separation with under-determined situation. The numerical results of SBSS demonstrate that the source signals are preeminently retrieved from a single observed mixture. The algorithm is successfully applied to Doppler weather radar with interference of bird. Simulation results showed that the meteorology echo signal and interference signal are obviously separated. In addition, the SBSS algorithm also can be applied to multipath separation, signal denoising and some other situation.
干扰抑制是雷达系统中一个永恒的问题。本文首先提出了一种新的单通道盲源分离(SBSS)算法,克服了传统盲源分离方法的局限性,并将该算法应用于气象雷达的干扰抑制。该方法的灵感来自于最近提出的变分模态分解(VMD)和稀疏分量分析(SCA)理论。采用VMD算法将单通道信号分解为双通道信号,并利用改进的SCA方法进行欠确定情况下的信号分离。SBSS的数值结果表明,源信号可以很好地从单个观测混合物中提取出来。该算法成功地应用于有鸟类干扰的多普勒天气雷达。仿真结果表明,气象回波信号与干扰信号明显分离。此外,SBSS算法还可以应用于多径分离、信号去噪等场合。
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引用次数: 1
Characteristic Analysis of X-band Dual Polarization Radar in a Hail Process 一次冰雹过程中x波段双偏振雷达特征分析
Pub Date : 2019-12-01 DOI: 10.1109/ICMO49322.2019.9025844
L. Feifei, Chen Shiying, Bu Zhichao, W. Xiaopeng, L. Jie
According to X-band dual-polarized radar data from Beijing area, the authors analyzed the radar echo characteristics of a strong convective hail cloud which used the algorithm for identifying hail and polarization characteristics. The results show that the convective cloud has a distinct V- shaped gap, and the vertex of the gap is facing the radar station. The strong echo structure at the vertex of the gap is compact. The echo top is 13 km, and the maximum reflectivity factor is 57.5 dBZ. Around the V-shaped gap, the differential reflectance factors which are far from the radar station show negative value, indicating that this area is a hail area; the differential reflectance factors which are near the radar station show positive value, indicating that this area has a heavy raindrop. The reflectivity factors at 19:18, 19:48, 20:09, and 20:30 were selected, and the vertical profile was made along the lower inflow direction and the core of strongest reflectance factor. The vertical profile exhibits typical echo characteristics such as WER, BWER and echo overhang. The differential reflectivity factors and correlation coefficients have obvious stratification characteristics, which reflect the precipitation particles within clouds rising continually under the influence of low-level inflow airflow and the upper ice particles moving to the right side of the WER with the upper horizontal airflow and then dropping gradually. This process verifies the evolution of hail rising and falling.
根据北京地区x波段双极化雷达资料,分析了利用该算法识别冰雹和极化特征的强对流雹云雷达回波特征。结果表明:对流云有明显的V形缝隙,缝隙顶点正对雷达站;间隙顶点处强回波结构致密。回波顶为13 km,最大反射系数为57.5 dBZ。在v型缝隙周围,远离雷达站的差反射率因子为负值,表明该区域为冰雹区;雷达站附近的差反系数为正值,表明该区域有强降水。选取19:18、19:48、20:09、20:30的反射率因子,沿较低入流方向和反射率因子最强的核心进行垂向剖面。垂向剖面表现出典型的回波特征,如反相、反相和回波悬垂。差反射率因子和相关系数具有明显的分层特征,反映了云内降水粒子在低层入流气流的影响下不断上升,上层冰粒随上层水平气流向WER右侧移动后逐渐下降。这一过程验证了冰雹上升和下降的演变过程。
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引用次数: 0
Temporal and Spatial Distribution Characteristics of Annual Precipitation in Chengdu 成都市年降水时空分布特征
Pub Date : 2019-12-01 DOI: 10.1109/ICMO49322.2019.9026149
Zhang Yi, Shangchang Ma, Panpan Zhao
At present, meteorologists have studied the laws of climate change throughout China and applied the results to many meteorological fields. The Chengdu area is located on the border of the northwestern plateau of Sichuan and the Sichuan Basin. The climate and environment are diverse. In order to understand the temporal and spatial characteristics of the precipitation field in Chengdu, and to predict the development trend of precipitation in Chengdu in a short time, this article uses 44a hourly precipitation data of 12 ground stations in Chengdu as reference materials. The two-dimensional interpolation method is used to fill in the missing data. The empirical orthogonal function analysis method is used to study the spatial distribution of precipitation fields, and the changing trend of precipitation in Chengdu area in 44a is analyzed by moving average. The results show that there are two main spatial types of annual precipitation in Chengdu. First, the changes in precipitation in Chengdu are highly consistent, that is, the city is either rainy or drizzle throughout the year. Second, the change pattern of precipitation in the northwest and southeast regions of Chengdu is opposite, that is, there is more rainfall in the northwest region and less rainfall in the southeast region, or less rainfall in the northwest region and more rainfall in the southeast region. It can be obtained from the time coefficient that the number of years of the modal one distribution model accounts for 54.5% of the total years, which is consistent with the cumulative variance contribution rate of the modal one, which can explain that the modal one is the main spatial type of precipitation field in Chengdu. The annual precipitation in Chengdu is generally decreasing.
目前,气象学家已经研究了中国各地的气候变化规律,并将研究结果应用于许多气象领域。成都地区位于四川西北高原和四川盆地的交界处。气候和环境是多样的。为了了解成都降水场的时空特征,预测成都短时间内降水的发展趋势,本文以成都12个地面站44a逐时降水数据为参考资料。采用二维插值法对缺失数据进行填充。采用经验正交函数分析方法研究了降水场的空间分布,并采用移动平均分析了成都地区44a降水的变化趋势。结果表明,成都市年降水主要存在两种空间类型。首先,成都的降水变化具有高度的一致性,即该城市全年不是多雨就是毛毛雨。其次,成都西北与东南地区降水变化格局相反,即西北地区降雨多,东南地区降雨少,或西北地区降雨少,东南地区降雨多。由时间系数可知,模态1分布模式的年数占总年数的54.5%,这与模态1的累积方差贡献率一致,说明模态1是成都降水场的主要空间类型。成都年降水量总体呈减少趋势。
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引用次数: 0
Research on Monitoring Downburst by Using Array Weather Radar 阵列气象雷达监测下爆的研究
Pub Date : 2019-12-01 DOI: 10.1109/ICMO49322.2019.9025883
Fangping Li, Shuqing Ma, Ling Yang, Fan Xia
The downburst is a short-time and smallscale strong convective weather system, which develops and dissipates extremely fast, and produces strong wind shear near the ground, and has a serious impact on the safety of aircrafts. The Array Weather Radar covers the elevation angle between 0 and 90 °, only takes 12s for a full volume scan, and can obtain high spatial and temporal resolution detection data. In order to improve the monitoring and early warning capability of the downburst, in this paper, a micro-downburst and a convective precipitation detected by the Array Weather Radar at Changsha Huanghua Airport in Hunan Province is analyzed by using the unit area equivalent potential value change and the echo characteristics of the AWR during the 15 minutes before the downburst happened. The data from airport ground automatic stations are analyzed and verified. The results show that the Array Weather Radar has significant advantages in monitoring short-time andsmall-scale weather systems such as downbursts. The convective process on May 20 2018 produced a local downdraft with the surface maximum wind speed of 11.6 m/s, and the release ratio of equivalent potential energy per unit area was over 30%; The water vapor starts to condense near the zero layer of the atmosphere and forms several storm cells The coalescence growth of the storm cells leads to form a new storm and accelerates the development of the new storm. The mid-level radial convergence and near-surface divergence of the echo are consistent with the wind speed and direction changes of the surface automatic meteorological station. The increases of the dew point temperature and pressure from automatic weather station have a certain indicative effect on the downdraft of storm. The AWR can give the warning information of 13 minutes before the surface wind speed reaches its maximum valve, and improve the monitoring and early warning on short-time small-scale weather systems such as downbursts by analyzing the effective potential energy release ratio per unit area.
降暴是一种短时小尺度强对流天气系统,发展和消散速度极快,在近地面产生强烈的风切变,对飞机安全造成严重影响。阵列气象雷达俯仰角范围为0 ~ 90°,全体扫描时间仅为12s,可获得高时空分辨率的探测数据。为了提高对降暴的监测和预警能力,利用单位面积等效势值变化和AWR回波特征,对湖南长沙黄花机场阵列气象雷达探测到的一次微降暴和一次对流降水进行了分析。对机场地面自动站的数据进行分析和验证。结果表明,阵列气象雷达在短时小尺度天气系统(如下暴)监测中具有显著优势。2018年5月20日对流过程产生局地下沉气流,地表最大风速为11.6 m/s,单位面积等效势能释放比大于30%;水汽在大气零层附近开始凝结,形成若干个风暴单体,风暴单体的合并生长导致形成新的风暴,并加速了新风暴的发展。回波的中层径向辐合和近地面辐散与地面自动气象站的风速和风向变化一致。自动气象站露点温度和露点压力的升高对暴雨下沉气流有一定的指示作用。AWR可以在地面风速达到最大阀值前13分钟给出预警信息,通过分析单位面积有效势能释放比,提高对降暴等短时间小尺度天气系统的监测预警能力。
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引用次数: 0
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2019 International Conference on Meteorology Observations (ICMO)
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