基于骨架线的Douglas-Peucker算法改进   总被引：1，自引：0，他引：1  

陈惠荣  郑义东  关海波  徐卫明 《海洋测绘》2011,31(5):18-20

针对Douglas-Pecuker算法中以垂直距离为化简指标的不足,提出了以骨架线为化简指标的改进算法.在对曲线凸凹顶点识别基础上,通过三角网的构建实现了凸点到基线的骨架线的提取,结合Douglas-Peucker算法的一般步骤,进行了曲线化简实验和方法的比较,验证了改进算法在保持线要素形态特征上的合理性.  相似文献   

四川盆地雷暴大风雷达回波特征统计分析   总被引：1，自引：0，他引：1  

龙柯吉  康岚  罗辉  郭旭  周秋雪  费海燕  吴薇  张琪 《气象》2020,46(2):212-222

采用2009—2018年地面、高空、闪电定位、多普勒雷达资料统计出四川盆地的34次雷暴大风过程,并根据冷空气参与情况及500 hPa影响系统将其分为五种类型:混合性大风类(Ⅰ类)、深厚低槽(低涡)后部类雷暴大风(Ⅱ-1)、低槽(切变)东移类雷暴大风(Ⅱ-2)、副热带高压西侧切变类雷暴大风(Ⅱ-3)和东风扰动类雷暴大风(Ⅱ-4)。统计分析了五类过程中发生雷暴大风站点对应的雷达回波特征,包括:对流组织类型、雷达回波强度、回波顶高、垂直液态水含量、中层径向辐合、风暴移动速度、回波质心下降、低仰角风速大值区和辐散。结果表明,82%的雷暴大风站点具有风速大值区,不同类型的雷暴大风过程还有其他不同的雷达回波特征,这些特征大多可提前10 min以上。另外,当站点出现中层径向辐合、辐散、回波强度大且伴有强梯度或回波类型为飑线时,也要考虑大风是否出现。  相似文献   

高原横切变线与高原低涡关系的初步研究     

杜梅  李国平  李山山 《大气科学》2020,44(2):269-281

基于大气运动方程组及散度方程,对高原横切变线上扰动稳定性问题以及切变线诱发高原低涡的动力学机制进行了理论分析并用欧洲中心(ECMWF)ERA-interim再分析资料对其进行验证。得出高原横切变线是高原低涡产生的重要背景场,切变线以南的水汽输送与辐合对于低涡的诱发作用是大气处于不平衡状态而引起散度场调整的结果,辐合增强区有利于高原低涡生成,低涡中心对应非平衡正值中心,低涡外围为非平衡项负值区。非平衡项负值大值与水汽辐合带的重叠区对降水落区有较好的指示意义。当高原南部的西南风带向东或东北方向移动或当低涡下游出现非平衡项负值中心时,低涡亦同向移动。若高原出现气旋式环流并且环流中心与非平衡项正值中心对应时,有利于低涡生成;进一步,当低涡中心与非平衡项正值中心对应且正值中心数值不断增大时,低涡趋于发展加强。  相似文献   

Study on the Structure of a Horizontal Shear Line over the Tibetan Plateau Based on CRA-Interim Datasets and Its Comparison with ERA-Interim Datasets     

姚秀萍  张硕  包晓红  师春香  刘景卫 《热带气象学报(英文版)》2020,26(4):483-494

The CRA-Interim trial production of the global atmospheric reanalysis for 10 years from 2007 to 2016 is carried out by the China Meteorological Administration (CMA) in 2017. The structural characteristics of the horizontal shear line over the Tibetan Plateau (TPHSL) based on the CRA-Interim datasets are examined by objectively identifying the shear line, and compared with the analysis results of the European Centre for Medium-Range Weather Forecasts (ECMWF)the European Center (ECMWF) reanalysis data (ERA-Interim). The case occurred at 18UTC on July 5, 2016. The results show that both of the ERA-Interim and CRA-Interim datasets can well reveal the circulation background and the dynamic and thermal structure characteristics of TPHSL, and they have shown some similar features. The middle and high latitudes at 500 hPa are characterized by500hPa present the circulation situation of  相似文献   

CHARACTERISTICS OF THE MERIDIONALLY ORIENTED SHEAR LINES OVER THE TIBETAN PLATEAU AND ITS RELATIONSHIP WITH RAINSTORMS IN THE BOREAL SUMMER HALF-YEAR     

姚秀萍  张霞  马嘉理 《热带气象学报(英文版)》2020,26(1):93-102

In this paper, European Center for Medium-Range Weather Forecasts(ECMWF) Reanalysis-Interim(ERAInterim) data and daily precipitation data in China from May to October during 1981-2016 are used to study the climatic characteristics of the meridionally oriented shear lines(MSLs) over the Tibetan Plateau(TP). The relationship between the MSL and rainstorms in the eastern TP and neighboring areas of the TP during the boreal summer half-year is also investigated. An objective method, which uses a combination of three parameters, i.e. the zonal shear of the meridional wind, the relative vorticity and the zero line of meridional wind, is adopted to identify the shear line. The results show that there are two high-occurrence centers of MSL. One is over the central TP(near 90°E) and the other is over the steep slope area of the eastern TP. Fewer MSLs are found along the Yarlung Zangbo River over the western TP and the southern Tibet. There are averagely 42.2 MSL days in each boreal summer half-year. The number of MSL days reaches the maximum of 62 in 2014 and the minimum of 22 in 2006. July and October witness the maximum of 10.2 MSL days/year and the minimum of 4.2 MSL days/year, respectively. The annual number of the MSL days shows periodicities of 2-4 and 4-6 years, which is quite similar to those of the MSL rainstorm days. In the neighboring areas of the TP, nearly56% of the MSLs lead to rainstorms, and nearly 40% of rainstorms are caused by the MSLs, indicating a close relationship between the MSLs and rainstorms in this region.  相似文献   

曲线化简的弧比弦算法改进及其评价     

刘慧敏  樊子德  徐震  邓敏 《地理与地理信息科学》2011,27(1):45-48

地图综合是当前国际GIS和制图学领域的一个难题。化简是地图综合的一个基本操作算子,线要素是地图综合操作的主要对象,该文主要研究地图线要素的化简问题。首先,从算法的适用范围、阈值设置等方面分析了现有算法的优点,重点阐述了一种常用的弧比弦算法,并指出了其在化简过程中存在的不足。然后,基于地图曲线的空间认知特征,提出了一种改进弧比弦算法。该算法能够更好地保持曲线的特征点和曲线的几何形态,避免阈值的设置问题。在算法评价上,采用3种定量评价指标,即:偏移平均值、偏移量中值和面积变形值,对改进的弧比弦算法与现有经典算法进行了比较分析。最后,通过算例分析验证了该算法的可行性、有效性和健壮性。  相似文献   

Inhibition of fish nodavirus by gymnemagenol extracted from Gymnema sylvestre     

V.Gopiesh Khanna  K.Kannabiran  V.Sarath Babu  A.S.Sahul Hameed 《中国海洋大学学报(英文版)》2011,10(4):402-408

Viral nervous necrosis(VNN)has emerged to become a major problem in the culture of larval and juvenile marine fish worldwide.Bioactive phytochemicals isolated from commonly available medicinal plants are often screened for their efficacy in controlling fish viral diseases.Occurrence of newer viral strains and resistance to existing antiviral drugs are problems currently as-sociated with treatment of VNN,which necessitates looking for alternate sources for effective antiviral drugs.The aim of the present study was to screen antiviral potential of gymnemagenol(C30H50O4)previously extracted from leaves of Gymnema sylvestre.The fish nodavirus,grouper nervous necrosis virus(GNNV)in infected Sahul Indian Grouper Eye(SIGE)cell lines were used to study the antiviral activity of gymnemagenol under in vitro conditions.The susceptibility of the virus to gymnemagenol was confirmed by measuring the viral titre(TCID50 mL?1)in virus-infected SIGE cells every 24 h.Gymnemagenol at 20 μg mL?1 inhibited the prolifera-tion of GNNV to 53% at the end of the 6th d by inhibiting the proliferation of GNNV-infected SIGE cells.The viable SIGE cells were reduced to 47% as determined by 3-(4,5-Dimethylthiazol-2-yl)-2,5-diphenyltetrazolium bromide(MTT)assay.The viral titre(TCID50 mL?1)was also reduced to log 2.8 at the end of the 7th d in gymnemagenol-treated SIGE cells after inoculated with GNNV when compared to untreated control SIGE cell viral titre(log 4.1).Based on our results it can be concluded that gymnemagenol could be used as an antiviral agent against GNNV infection.  相似文献   

Mangkhut（1822）台风飑线在江西的影响过程分析          下载免费PDF全文

孙素琴  刘文英  刘春  毛连海 《气象与减灾研究》2021,44(1):9-15

主要利用常规气象资料和NCEP 1° ×1°再分析资料,对2018年22号超强台风Mangkhut在江西引发的飑线天气过程进行分析.结果表明:飑线在台风和副热带高压间的湿区生成,台风为此次飑线提供了有利条件.台风外围的低空急流输送充沛水汽,较强的对流有效位能和持久的地面辐合线使得初始离散对流单体组织发展成为台风飑线,而较强的低空垂直风切变为飑线的进一步发展提供了动力条件.江西省中南部中层入流环境及地面冷池等有利于雷暴大风的生成,江西省北部深厚的湿层和强烈的垂直上升运动等利于短时暴雨的发生.  相似文献   

REVIEWS OF GEOGRAPHIC SOFTWARE     

《The Professional geographer》1985,37(3):354-356

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Lateglacial and early Holocene palaeoclimatic reconstruction based on glacier fluctuations and equilibrium‐line altitudes at northern Folgefonna,Hardanger, western Norway     

Jostein Bakke  Svein Olaf Dahl  Atle Nesje 《第四纪科学杂志》2005,20(2):179-198

Northern Folgefonna (c. 23 km²), is a nearly circular maritime ice cap located on the Folgefonna Peninsula in Hardanger, western Norway. By combining the position of marginal moraines with AMS radiocarbon dated glacier‐meltwater induced sediments in proglacial lakes draining northern Folgefonna, a continuous high‐resolution record of variations in glacier size and equilibrium‐line altitudes (ELAs) during the Lateglacial and early Holocene has been obtained. After the termination of the Younger Dryas (c. 11 500 cal. yr BP), a short‐lived (100–150 years) climatically induced glacier readvance termed the ‘Jondal Event 1’ occurred within the ‘Preboreal Oscillation’ (PBO) c. 11 100 cal. yr BP. Bracketed to 10 550–10 450 cal. yr BP, a second glacier readvance is named the ‘Jondal Event 2’. A third readvance occurred about 10 000 cal. yr BP and corresponds with the ‘Erdalen Event 1’ recorded at Jostedalsbreen. An exponential relationship between mean solid winter precipitation and ablation‐season temperature at the ELA of Norwegian glaciers is used to reconstruct former variations in winter precipitation based on the corresponding ELA and an independent proxy for summer temperature. Compared to the present, the Younger Dryas was much colder and drier, the ‘Jondal Event 1’/PBO was colder and somewhat drier, and the ‘Jondal Event 2’ was much wetter. The ‘Erdalen Event 1’ started as rather dry and terminated as somewhat wetter. Variations in glacier magnitude/ELAs and corresponding palaeoclimatic reconstructions at northern Folgefonna suggest that low‐altitude cirque glaciers (lowest altitude of marginal moraines 290 m) in the area existed for the last time during the Younger Dryas. These low‐altitude cirque glaciers of suggested Younger Dryas age do not fit into the previous reconstructions of the Younger Dryas ice sheet in Hardanger. Copyright © 2005 John Wiley & Sons, Ltd.  相似文献