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171.
分步迭代的多光谱遥感水体信息高精度自动提取 总被引:17,自引:4,他引:13
以LANDSAT卫星遥感数据为信息源, 在归一化差异水指数(NDWI)计算的基础上, 采用“全域—局部”的分步迭代空间尺度转换机制, 将全域分割、全域分类、局部分割与分类等计算过程有机地结合起来, 分阶段地融合了水体信息提取所需的不同层次知识, 并建立迭代算法实现了水体最佳边缘的逐步逼近, 获得了高精度的水体信息提取。通过对青藏高原试验区湖泊信息提取的实验表明, 该方法除了能够实现对复杂多样的水体信息进行高精度自动提取外, 还可有效避免与阴影等信息的混淆。 相似文献
172.
近年来,天气和气候业务对国外数据种类和时效要求不断提高,为解决大量数据的收集分发压力以及管理问题,设计并实现了基于流程控制的国际气象通信数据收集管理系统。系统应用数据收集器Logstash、Inotify监听机制与分析平台Kibana等技术,支持多种通信协议,扩展Scrapy网络爬虫功能,通过流程控制、任务调度等方式实现大量数据快速高效收集和集成管理,有效提高数据并行处理能力和可扩展性,且设计了全流程监视,保障数据时效。系统已经上线提供服务,为业务/科研用户提供全球观测数据、国外卫星数据和数值预报产品等300余种,日收集数据量约2 TB。 相似文献
173.
外商直接投资与经济增长的关系研究——基于分省和分区数据的检验 总被引:1,自引:0,他引:1
论文分别以分省和分区(东、中、西部)1992~2004年的面板数据,利用我们修正过的De Mello模型和更为稳健的模型检验方法,研究了我国利用外商直接投资对经济增长的影响作用。研究结果发现,利用分省数据的模型证明了FDI对我国经济增长的正向积极作用,这一点与其他研究结果相同,但是利用分区数据的研究表明,虽然我国西部仍然是FDI作用最弱的区域,但是东部与中部比较,GDP增长率变动对FDI增长率变动的敏感性不明显,有别于中部,这在一定程度上可以说明东部地区存在FDI过密和外商投资产业的过度竞争问题。 相似文献
174.
李世敏 《广东海洋大学学报》2006,26(5):134-136
在英汉两种文化里,许多词语承载着各自的联想意义,这些联想意义有的部分相同,有的不同或截然相反,有的词义在两种文化中没有对应词。文化差异还表现在诸多用语如问候语、恭维语、致谢语、禁忌语等以及非言语交际手段如手势、表情等方面。外语教师不仅应把这些差异融入教学过程中,还应组织各种课外活动帮助学生了解母语和目的语的文化差异,从而提高学生的跨文化交际能力。 相似文献
175.
国外港口物流发展与闽台港口物流对接 总被引:3,自引:0,他引:3
分析福建与台湾港口物流发展现状和存在问题,以及高雄-厦门、高雄-福州海上试航和“两门两马”小三通直航发展态势,指出两岸试航的局限性和港口物流直航的必然性。综合分析鹿特丹、新加坡、安特卫普、釜山、汉堡等世界著名港口物流发展经验,提出对闽台两岸港口物流对接具有可供借鉴经验。针对闽台港口物流发展中存在问题提出了两岸港口资源整合,建立台海港口群;完善集疏运体系,促进港口物流对接;大力发展临港工业,构建环台湾海峡临港工业走廊等措施。 相似文献
176.
Chi Kin Leung 《The Professional geographer》1990,42(4):403-421
An examination of the locational characteristics of intended foreign equity joint venture (EJV) investment in China during the period 1979 to 1985 indicates that foreign EJV investment was highly concentrated in the coastal region, in the more developed areas of the provinces, and in large cities. The locational characteristics, however, differed between economic sectors and between countries of origin of investment. Although foreign EJV investment became spatially more dispersed through time, the impacts on the development of inland regions and backward areas in China remained limited. 相似文献
177.
Stereo analysis of images obtained during the 2001 flyby of Comet Borrelly by NASA's Deep Space 1 (DS1) probe allows us to quantify the shape and photometric behavior of the nucleus. The shape is complex, with planar facets corresponding to the dark, mottled regions of the surface whereas the bright, smooth regions are convexly curved. The photometric as well as textural differences between these regions can be explained in terms of topography (roughness) at and below the image resolution, without invoking significant variations in single-particle properties; the material on Borrelly's surface could be quite uniform. A statistical comparison of the digital elevation models (DEMs) produced from the three highest-resolution images independently at the USGS and DLR shows that their difference standard deviation is 120 m, consistent with a matching error of 0.20 pixel (similar to reported matching accuracies for many other stereo datasets). The DEMs also show some systematic differences attributable to manual versus automatic matching. Disk-resolved photometric modeling of the nucleus using the DEM shows that bright, smooth terrains on Borrelly are similar in roughness (Hapke roughness θ=20°) to C-type asteroid Mathilde but slightly brighter and more backscattering (single-scattering albedo w=0.056, Henyey-Greenstein phase parameter g=−0.32). The dark, mottled terrain is photometrically consistent with the same particles but with roughnesses as large as 60°. Intrinsically darker material is inconsistent with the phase behavior of these regions. Many local radiance variations are clearly related to topography, and others are consistent with a topographic explanation; one need not invoke albedo variations greater than a few tens of percent to explain the appearance of Borrelly. 相似文献
178.
The investigation of fragmented comets provides information on the physical properties and internal structure of cometary nuclei, as well as insights into the mechanisms responsible for cometary breakups. The Jupiter-family Comet 73P/Schwassmann-Wachmann 3 (73P/SW3) fragmented non-tidally into at least four components, and probably more, in the autumn of 1995. Fragment C was detected with the Wide Field Planetary Camera 2 (WFPC2) of the Hubble Space Telescope (HST) on 26 November 2001 when it was 3.26 AU from the Sun and 2.34 AU from the Earth. The high spatial resolution of the HST allowed us to separate the signal of the fragment from that of its coma, and to determine its R magnitude in the Johnson-Kron-Cousins photometric system from four images taken with the F675W filter. Assuming a spherical body with a geometric albedo of 0.04 and a linear phase coefficient of 0.04 mag deg−1 for the R band, we derived an effective radius of . The pre-breakup radius of the original nucleus was estimated to be 1.1 km, which implies that the volume of fragment C is ∼25% of the total volume of the pre-breakup nucleus. The limited temporal coverage of our observations preclude deriving an accurate shape or rotational period; our measurements are consistent with a rather spherical body but an elongated shape cannot be excluded. Fragment C was very active despite its rather large heliocentric distance, with an estimated dust production rate of (∼130 metric tons day−1). A very large fraction of the surface area of fragment C must have been sublimating to sustain such a high level of activity. Fragment C may be recovered at its next return in 2006, if it does not experience further fragmentation. 相似文献
179.
180.
本文研究了河流沉积构造、结构、石英颗粒表面特征和沉积相特征,并提出组成曲流点坝标志的两个重要要素及沉积模式。有助于认识古代岩相中点坝层序和对此模式。 相似文献