The use of Bluetooth for analysing spatiotemporal dynamics of human movement at mass events: A case study of the Ghent Festivities     

Mathias Versichele  Tijs Neutens Matthias Delafontaine  Nico Van de Weghe 《Applied geography (Sevenoaks, England)》2012,32(2):208-220

In this paper, proximity-based Bluetooth tracking is postulated as an efficient and effective methodology for analysing the complex spatiotemporal dynamics of visitor movements at mass events. A case study of the Ghent Festivities event (1.5 million visitors over 10 days) is described in detail and preliminary results are shown to give an indication of the added value of the methodology for stakeholders of the event. By covering 22 locations in the study area with Bluetooth scanners, we were able to extract 152,487 trajectories generated by 80,828 detected visitors. Apart from generating clear statistics such as visitor counts, the share of returning visitors, and visitor flow maps, the analyses also reveal the complex nature of this event by hinting at the existence of several mutually different visitor profiles. We conclude by arguing why Bluetooth tracking offers significant advantages for tracking mass event visitors with respect to other and more prominent technologies, and outline some of its remaining deficiencies.  相似文献   

猪野泽中全新世干旱事件时空范围和机制     

李育  王乃昂  李卓仑  张华安  周雪花  张成琦 《地理科学》2012,(6):731-738

以亚洲季风边缘区石羊河流域终端湖猪野泽为例,结合最新的沉积物年代、岩性、指标及古湖泊岸堤研究结果,从时间和空间尺度上探讨了猪野泽中全新世干旱事件时空范围和机制。从空间上对比了猪野泽中全新世地貌及沉积物岩性和指标,并配合石羊河中、上游地区的中全新世沉积剖面进行研究。在时间尺度上分析了猪野泽和石羊河流域近百个全新世测年结果,最终得出猪野泽地区在8.0~7.0 cal ka B.P.期间存在百年尺度的干旱事件,而不是以前研究提出的距今7000~5000日历年期间2000 a尺度的干旱事件,并且这次极端干旱事件影响范围主要在石羊河中、下游地区,对石羊河上游地区影响较小。根据时空尺度分析对猪野泽中全新世干旱事件机制进行讨论,结果表明这次干旱事件主要是由流域气候条件特征和水热配比改变所引起的,而不是以前研究提出的亚洲夏季风减弱导致。  相似文献   

地球早期碳循环与大氧化事件     

朱建江  刘福来  张立飞 《岩石矿物学杂志》2022,41(2):396-412

碳是影响地球宜居性的重要元素,地表系统和地球深部之间的碳循环作用对于全球气候的变化具有非常重要的影响.现今地球主要通过俯冲作用和火山作用调节全球碳循环过程,然而地球早期的碳循环过程和现今地球存在显著的差异.本文结合前人的相关研究成果,综合探讨了地球原始碳的来源、地球早期碳循环过程及其与大氧化事件的联系等问题.地球是从太...  相似文献   

贵州省汛期短时降水时空特征分析   总被引：10，自引：2，他引：8  

彭芳  吴古会  杜小玲 《气象》2012,38(3):307-313

利用贵州区域84测站1991—2009年汛期（4—9月）逐小时降水量资料,分别定义各站点的小时降水量的强降水阈值。阈值的分布有两个高值中心,最强中心在西南部望谟站,西北部的强降水阈值较低。同时利用各站点阈值统计19年不同月份的强降水事件频数,其分布显示：4月份东部和中部偏南地区频数较高,5月份频数高值区呈东北—西南向,随后几个月逐渐向西北推进。4—6月事件频数逐渐增大,7月维持,8—9月开始减少。各月强降水事件发生时次统计表明：一天中有三个相对高值时段,23：00—02：00、05：00—08：00和17：00—20：00,而白天强降水事件很少。短时强降水事件发生时次的空间分布表明,西北部的强降水事件多数发生在傍晚到23：00,中部的强降水集中在23：00—02：00,东南部在05：00—08：00。  相似文献   

利用二维极值分布模拟我国几个代表站的强降水概率特征     

余锦华  李佳耘  丁裕国 《南京气象学院学报》2012,(6):652-657

基于中国6个代表站5-9月的逐日降水资料,利用二维Gumbel-Logistic分布,研究了中国不同区域的过程降水量和日最大强降水雨量的联合概率特征。结果表明,各代表性台站的过程雨量和强降水雨量的联合分布均符合二维Gumbel分布。强降水雨量与过程降雨量联合分布所描述的极端事件是更小的小概率事件。相同强降水雨量条件下,过程雨量越大,重现期越长当强降水雨量增大时,同一过程雨量的重现期也延长。在同级强降水雨量出现的条件下,各地过程降雨量往往是愈往南方其条件概率愈大,而其出现的过程雨量也随之增大。这为研究强降水极端状况的全方位特征做出了新的试验．也曼加客观地揭示了极端气候事件的多方面概率特征．  相似文献   

ENSO事件与中国东南沿海3月降水关系分析   总被引：1，自引：0，他引：1  

任广成  余明祥  张哲 《气象与减灾研究》2008,31(1):44-48

利用1951—2006年永安、赣州、厦门、梅州、汕头、曲江和河源7个代表站3月降水量资料,以及南方涛动指数（SOI）和北太平洋海温资料,分析了中国东南沿海3月降水的年际和年代际变化特征,及其与ENSO事件的关系。结果发现,东南沿海3月降水具有年际变化大和年代际变化明显的特征,与SOI、赤道东太平洋海温和西风漂流区海温存在显著相关。在前一年出现厄尔尼诺现象,北太平洋海温距平分布呈厄尔尼诺分布型,SOI偏低的情况下,东南沿海3月降水偏多;反之,前一年出现拉尼娜现象,北太平洋海温距平分布呈现拉尼娜分布型,SOI偏高时,东南沿海3月降水偏少。前期1月赤道东太平洋关键区海温和前期2月西风漂流区关键区海温的异常变化,对东南沿海3月降水具有很好的指示意义。当前期1月赤道东太平洋关键区海温偏高,前期2月西风漂流区关键区海温偏低时,东南沿海3月降水偏多;反之,东南沿海3月降水则偏少。  相似文献   

北京城市热岛效应的昼夜变化特征分析   总被引：26，自引：9，他引：17  

谢庄  崔继良  陈大刚  胡保昆 《气候与环境研究》2006,11(1):69-75

利用最新获取的1998年3月~2001年12月北京地区自动站资料,对北京城市热岛效应进行了细致、完整的研究。选取城区的官园站和郊区密云站的气温差作为城市热岛效应强度指标。在验证了资料可靠性的基础上,研究了热岛强度昼夜变化的年、季、月及日变化特征,以及几种极端天气事件的逐时及平均热岛强度的变化,最后制作了连续3年的月平均逐时热岛强度变化的三维立体图。  相似文献   

基于事件的时空数据模型应用研究   总被引：9，自引：4，他引：5  

王春波  张军  蒋涛 《测绘科学》2005,30(2):67-69

本文首先分析和比较了几种有代表性时空数据模型的特点和存在的局限性 ,对基于事件的时空数据模型进行了改进 ,并提出了利用亲缘继承关系进行历史回溯查询 ,根据具体的实际应用 ,在现有成熟的ARCGIS平台上进行扩展 ,验证了该模型的有效性。实践表明 :利用该模型可以有效的进行各种时间、空间和属性的互查 ;时间因素和空间对象的空间特征和属性信息分开存储管理 ,便于时空分析 ,适于进行地理事件与空间对象状态因果关系的推理 ;减小了数据的存储空间 ,以及数据的冗余度  相似文献   

Baiyun Movement: A Significant Tectonic Event on Oligocene/Miocene Boundary in the Northern South China Sea and Its Regional Implications     

Pang Xiong  Chen Changmin  Zhu Ming  He Min  Shen Jun  Lian Shiyong  Wu Xiangjie  Shao Lei 《中国地质大学学报(英文版)》2009,20(1)

A significant geologic event occurred on the Oligocene/Miocene boundary at 23.8 Ma in the northern South China Sea,which is named the Baiyun (白云) movement in this article.This event strongly affected not only the South China Sea,but also East Asia.After the Balyun event,the ridge of seafloor spreading of the South China Sea Jumped southward and rotated counterclockwise,and a strong subsidence occurred in the Baiyun sag of the Pearl River Month basin.The shelf break shifted suddenly from the south to the north of the Baiyun sag,and the deposition environment in this sag changed from continental shelf with neritic deposition to continental slope with deep-water deposition.Sediment geochemistry study indicated that the Balyun event played a key role in the rapid change of sediment provenance for the Pearl River Mouth basin.Between 32 and 23.8 Ma,the source of sediments was mainly from the granites in South China,while after 23.8 Ma some sediments might have come from the eastern Himalaya,as the Pearl River drainage extended westward after the uplift of Tibet since that time.The Baiyun event led to a great change in the drainage framework of the paleoPearl River,sediment types and the depositional environments in the Pearl River Mouth basin,and relative sea level of the northern South China Sea,as well as sedimentation and hydrocarbon accumulation in the ares.  相似文献   

SHRIMP U–Pb zircon geochronology of high-grade rocks and charnockites from the eastern Amery Ice Shelf and southwestern Prydz Bay, East Antarctica: Constraints on Late Mesoproterozoic to Cambrian tectonothermal events related to supercontinent assembly     

Xiaochun Liu  Yue Zhao  Biao Song  Jian Liu  Jianjun Cui 《Gondwana Research》2009,16(2):342

The eastern Amery Ice Shelf (EAIS) and southwestern Prydz Bay are situated near the junction between the Late Neoproterozoic/Cambrian high-grade complex of the Prydz Belt and the Early Neoproterozoic Rayner Complex. The area contains an important geological section for understanding the tectonic evolution of East Antarctica. SHRIMP U–Pb analyses on zircons of felsic orthogneisses and mafic granulites from the area indicate that their protoliths were emplaced during four episodes of ca. 1380 Ma, ca. 1210–1170 Ma, ca. 1130–1120 Ma and ca. 1060–1020 Ma. Subsequently, these rocks experienced two episodes of high-grade metamorphism at > 970 Ma and ca. 930–900 Ma, and furthermore, most of them (except for some from the Munro Kerr Mountains and Reinbolt Hills) were subjected to high-grade metamorphic recrystallization at ca. 535 Ma. Two suites of charnockite, i.e. the Reinbolt and Jennings charnockites, intrude the Late Mesoproterozoic/Early Neoproterozoic and Late Neoproterozoic/Cambrian high-grade complexes at > 955 Ma and 500 Ma, respectively. These, together with associated granites of similar ages, reflect late- to post-orogenic magmatism occurring during the two major orogenic events. The similarity in age patterns suggests that the EAIS–Prydz Bay region may have suffered from the same high-grade tectonothermal evolution with the Rayner Complex and the Eastern Ghats of India. Three segments might constitute a previously unified Late Mesoproterozoic/Early Neoproterozoic orogen that resulted from the long-term magmatic accretion from ca. 1380 to 1020 Ma and eventual collision before ca. 900 Ma between India and the western portion of East Antarctica. The Prydz Belt may have developed on the eastern margin of the Indo-Antarctica continental block, and the Late Neoproterozoic/Cambrian suture assembling Indo-Antarctica and Australo-Antarctica continental blocks should be located southeastwards of the EAIS–Prydz Bay region.  相似文献