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991.
随着精细化降水预报的要求和发展,模式对站点定量降水预报已成为天气预报业务的主要参考依据之一。本文对乌鲁木齐区域数值天气预报系统DOGRAFS v1.0在2016年夏季全疆105个站点的24h累积降水量的预报性能进行统计检验。结果表明:(1)除山区外,全疆晴天预报准确率达到85%以上,其中南疆盆地、吐鄯托盆地晴天预报准确率达到95%以上。(2)对于小雨出现较多的站点,预报准确率达到55%以上、部分站点达到70%,同时上述区域存在15%左右的报强率;对于降水较少的南疆盆地和吐鄯托盆地整体以漏报为主,漏报率在80%以上。(3)北疆大部分地区和南疆西部山区的中雨预报准确率整体在30%左右;中雨日数较多的中天山及其两侧预报准确率约60%,该区域也存在20%左右的报强率;其他地区预报降水较实况以偏弱为主。(4)大雨及以上量级降水,模式预报整体表现为偏弱,对于大降水出现较多的地区预报平均准确率为25-30%。 相似文献
992.
利用常规观测、区域自动气象站、NCEP/NCAR再分析和雷达回波资料,对2016年6月30日山东一次阵风锋触发的强对流天气进行了分析。结果表明,此次强对流主要发生在高空槽与副热带高压相互作用、山东高低层受一致西南气流影响的环流形势下,阵风锋、地面辐合线和负变压中心所产生的抬升作用及近地面层冷空气的侵入使气温骤降是触发对流的关键因素。低层水汽充沛、湿层厚,属于上干下湿的不稳定层结。强对流发生区域处在假相当位温差(Δθse)和风暴相对螺旋度(storm relative helicity,SRH)的大值中心及其右侧位置。对流有效位能(convective available potential energy,CAPE)、850 hPa与500 hPa之间温差、大风指数、强天气威胁指数等都对此次强对流有较好的指示作用。0 ℃层高度和融化层高度较高是此次过程未出现大冰雹的原因。较强的0~3 km垂直风切变在强对流预报业务中需要注意。此次强对流过程是线状回波带前侧风暴内出现了阵风锋,阵风锋又不断触发雷暴使个别强单体风暴发展加强成为超级单体风暴,具有持续时间较短的中气旋、高悬的强回波、有界弱回波区、风暴顶辐散、窄带回波、径向速度大值区等回波特征。风暴移动速度比风暴承载层平均风速大,缩短了超级单体存在时间。此外,风暴参数与天气的强烈程度密切相关。 相似文献
993.
This study investigates the relationship between summer low-frequency rainfall over southern China and tropical intraseasonal oscillation (ISO) in the atmosphere by examining systematically the propagation features of the tropical ISO in terms of focusing on five large-scale low-frequency rainfall regimes in summer over southern China. It is demonstrated that there is a close linkage between the five rainfall regimes over southern China and the northward propagation of the tropical ISO. The moist ISO signals, which influence the low-frequency rainfall events in different regions of southern China, mainly propagate northwestward from the tropical ocean to the southeast of China. The southeast China rainfall regime is intimately associated with the moist ISO signals propagating northwestward from the equatorial mid-western Pacific Ocean. For both the Yangtze River regime and South of Yangtze River regime, the moist ISO signals over the northern South China Sea show an evident northward propagation towards the Yangtze River region, and then propagate westward. It is further found that the interaction between the northward propagation of low-latitude ISO signals and the southward propagation of high-latitude ISO signals can also make a clear influence on the low-frequency rainfall in southern China. For the Southern China regime, the moist ISO signals show a significant northward propagation from the Philippines. Moreover, for the rainless regime, southern China is under dry ISO signals’ control, and the latter shows no clear propagation to southern China. This study may provide insights for the extended-range forecasting of summer rainfall in southern China. 相似文献
994.
青藏高原那曲地区夏季一次对流云降水过程的云微物理及区域水分收支特征 总被引:4,自引:1,他引:3
第三次青藏高原科学试验针对高原夏季云和降水物理过程开展了大量观测研究,为进一步揭示高原云微物理结构、云中水分转化和区域水分收支特征,本文采用中尺度数值预报模式(WRF)并结合高原试验期间的各种观测资料,对那曲观测试验区2014年7月5~6日的一次较为典型的夏季对流云降水过程进行了数值模拟研究。结果表明WRF模式能够基本再现高原夏季对流云的发展演变过程以及降水的日变化特征。模拟结果显示高原夏季对流云中具有较高的过冷云水和霰粒子含量,冰相过程在高原云和降水的形成和发展中具有十分重要的作用,地面降水主要由霰粒子融化产生。暖雨过程对降水的直接贡献很小,但在霰胚形成中具有十分重要的作用。霰粒子胚胎的形成主要来源于冰晶与过冷雨滴的撞冻过程,雪粒子和过冷雨水的碰冻转化及过冷雨滴的均质冻结贡献相对较小。霰粒子的增长过程在12 km(-40℃)以上层主要依靠对冰晶、雪粒子的聚并收集过程,而在其下层的增长过程主要依赖对过冷云水的凇附增长,对雪粒子的聚并收集和凝华增长过程较小。高原那曲地区净水汽收支为正,日平均降水转化率可达20.75%,接近长江下游地区,高于华北、西北地区。该地区日降水再循环率为10.92%,说明局地蒸发的水汽对高原降水的水汽来源具有一定的贡献,但高原降水的90%仍然由外界输入的水汽转化形成。 相似文献
995.
996.
997.
Harry West Michael Horswell Nevil Quinn 《International journal of geographical information science》2018,32(6):1172-1193
As sea level is projected to rise throughout the twenty-first century due to climate change, there is a need to ensure that sea level rise (SLR) models accurately and defensibly represent future flood inundation levels to allow for effective coastal zone management. Digital elevation models (DEMs) are integral to SLR modelling, but are subject to error, including in their vertical resolution. Error in DEMs leads to uncertainty in the output of SLR inundation models, which if not considered, may result in poor coastal management decisions. However, DEM error is not usually described in detail by DEM suppliers; commonly only the RMSE is reported. This research explores the impact of stated vertical error in delineating zones of inundation in two locations along the Devon, United Kingdom, coastline (Exe and Otter Estuaries). We explore the consequences of needing to make assumptions about the distribution of error in the absence of detailed error data using a 1 m, publically available composite DEM with a maximum RMSE of 0.15 m, typical of recent LiDAR-derived DEMs. We compare uncertainty using two methods (i) the NOAA inundation uncertainty mapping method which assumes a normal distribution of error and (ii) a hydrologically correct bathtub method where the DEM is uniformly perturbed between the upper and lower bounds of a 95% linear error in 500 Monte Carlo Simulations (HBM+MCS). The NOAA method produced a broader zone of uncertainty (an increase of 134.9% on the HBM+MCS method), which is particularly evident in the flatter topography of the upper estuaries. The HBM+MCS method generates a narrower band of uncertainty for these flatter areas, but very similar extents where shorelines are steeper. The differences in inundation extents produced by the methods relate to a number of underpinning assumptions, and particularly, how the stated RMSE is interpreted and used to represent error in a practical sense. Unlike the NOAA method, the HBM+MCS model is computationally intensive, depending on the areas under consideration and the number of iterations. We therefore used the HBM+ MCS method to derive a regression relationship between elevation and inundation probability for the Exe Estuary. We then apply this to the adjacent Otter Estuary and show that it can defensibly reproduce zones of inundation uncertainty, avoiding the computationally intensive step of the HBM+MCS. The equation-derived zone of uncertainty was 112.1% larger than the HBM+MCS method, compared to the NOAA method which produced an uncertain area 423.9% larger. Each approach has advantages and disadvantages and requires value judgements to be made. Their use underscores the need for transparency in assumptions and communications of outputs. We urge DEM publishers to move beyond provision of a generalised RMSE and provide more detailed estimates of spatial error and complete metadata, including locations of ground control points and associated land cover. 相似文献
998.
This study examines the effectiveness of integrating geography into existing math and science curriculum to teach climate change and sea level rise. The desired outcome is to improve student performance in all three subjects. A sample of 120 fifth graders from three schools were taught the integrated curriculum over a period of two to three weeks. They were given a pretest and posttest comprised of questions measuring knowledge relevant to the lesson in terms of geography, math, science, and spatial skills. Paired-samples t-tests were conducted to determine significant differences in student performance. These t-tests indicate statistically significant improvements in all but one instance across all subjects, at all schools for both boys and girls. No statistically significant results were observed for a control group of an additional twenty-seven fifth graders. These results demonstrate the value of combining geography with math and science to improve student performance in STEM knowledge. 相似文献
999.
基于期刊论文的中国地级以上城市知识专业化研究 总被引:3,自引:2,他引:1
将287个地级以上城市(不包括港澳台地区)作为研究对象,以中国知网发布的168个学科领域期刊论文数量为数据来源,对中国地级以上城市知识专业化水平、影响因素及其与经济发展的关系进行了研究。研究发现:① 中国地级以上城市的专业化水平总体偏低,多样化水平较为明显;知识专业化水平西部地区>中部地区>东部地区;地区相对专业化指数随城市行政等级依次升高,即直辖市<副省级城市<省会城市<普通地级市。具有资源优势的城市,其知识专业化领域高度集中在以资源为基础的领域;中小城市的知识专业化领域相对较少,专业化程度高;大中城市知识专业化领域多,多样化趋势明显,但各领域的知识专业化程度相对较低。从城市等级上来看,知识专业化程度表现为五线城市>四线城市>三线城市>二线城市>一线城市。② 知识专业化水平主要受科教经济因素、人才潜力和服务业因素、工业基础因素、人口规模因素四大因素影响。③ 知识专业化与经济发展关系密切,整体呈现倒U形关系;但各区域随发展阶段不同,表现出不同的形式可以分为U形、倒U形、M形和W形4种大类型。 相似文献
1000.
The spatial mismatch situation of tourism development in Guangdong Province is analyzed by gravity model and two-dimensional matrix based on the spatial mismatch hypothesis, and the results are visualized using ArcGIS software. This study finds that varying degrees of spatial mismatch exist between the level of tourism development, abundance of tourism resources and accessibility of tourism locations in the 21 cities in Guangdong Province. The gravity centers for tourism economy, tourism resources and tourism location are (113.55° E, 23.00° N), (113.69° E, 23.21° N) and (113.74° E, 22.86° N), respectively. According to the two-dimensional combinatorial matrices, synchronous development is shown in 10 prefecture-level cities for the tourism revenue-resource abundance combination, whereas it is shown in seven prefecture-level cities for the tourism revenue-tourism location combination. Guangzhou and Shenzhen are synchronous-double high zones for both combinations, while Foshan, Qingyuan, Yangjiang, Zhongshan and Jieyang are deviating-negative mismatch zones for both combinations. Furthermore, the vast majority of prefecture-level cities within the province currently present mismatching trends in tourism development. Based on the analysis results, corresponding countermeasures and suggestions are put forward taking into account the actual situation and opportunities for further tourism development in various prefecture-level cities. 相似文献