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991.
大湄公河次区域是自1992年起由亚洲开发银行启动的区域性长期合作计划涉及的区域。在大湄公河次区域经济合作数字化分析过程中,行政区划地理信息系统数据库就成为其中基础性数据库,也是应用面最宽的数据库。本文重点是在现有的行政区划地理信息系统数据库的基础上,建立大湄公河次区域中尺度行政区划地理信息系统数据库(GMS—AdmBnd)的开发标准,包括:主要技术指标,开发流程和成果质量比对指标。本论文内容的发表,将便于用户在使用该数据时根据数据库特点,了解其适用性和局限性,有针对性地加以应用。 相似文献
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统计物理学用"熵"来表示分子不规则运动的程度,信息论中则用它来度量信息量,即一个系统越是有序,信息熵就越低。在对浙江省全省城镇土地调查数据汇总统计的基础上,运用信息熵的概念对复杂的城市土地利用结构进行详细的定量分析,用信息熵和均衡度值来说明城市土地利用的特点,利用方式的多样性和复杂性,并提出提高土地利用效益的工作建议。 相似文献
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通过开发实例介绍了两种数字摄影测量系统(DPS)与测图软件的联机测图的实现过程,经对比分析提出DPS与行业测图软件之间进行联机测图通用方法。 相似文献
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Microphysical Effects of Cloud Seeding in Supercooled Stratiform Clouds Observed from NOAA Satellite
Based on the satellite retrieval methodology, the spectral characteristics and cloud microphysical properties were analyzed that included brightness temperatures of Channels 4 and 5, and their brightness temperature difference (BTD), the particle effective radius of seeded cloud track caused by an operational cloud seeding and the microphysical effects of cloud seeding were revealed by the comparisons of their differences inside and outside the seeded track. The cloud track was actually a cloud channel reaching 1.5-km deep and 14-km wide lasting for more than 80 min. The effective radius of ambient clouds was 10-15μm, while that within the cloud track ranged from 15 to 26μm. The ambient clouds were composed of supercooled droplets, and the composition of the cloud within the seeding track was ice. With respect to the rather stable reflectance of two ambient sides around the track, the visible spectral reflectance in the cloud track varied at least 10%, and reached a maximum of 35%, the reflectance of 3.7μm in the seeded track relatively decreased at least 10%. As cloud seeding advanced, the width and depth were gradually increased. Simultaneously the cloud top temperature within the track became progressively warmer with respect to the ambient clouds, and the maximum temperature differences reached 4.2 and 3.9℃at the first seeding position for Channels 4 and 5. In addition, the BTD in the track also increased steadily to a maximum of 1.4℃, compared with 0.2-0.4℃of the ambient clouds. The evidence that the seeded cloud became thinner comes from the visible image showing a channel, the warming of the cloud tops, and the increase of BTD in the seeded track. The seeded cloud became thinner mainly because the cloud top descended and it lost water to precipitation throughout its depth. For this cloud seeding case, the glaciation became apparent at cloud tops about 22 min after seeding. The formation of a cloud track in the supercooled stratiform clouds was mainly because that the seeded cloud volume glaciated into ice hydrometeors that precipitated and so lowered cloud top height. A thin line of new water clouds formed in the middle of the seeded track between 38 and 63 min after seeding, probably as a result of rising motion induced by the released latent heat of freezing. These clouds disappeared in the earlier segments of the seeded track, which suggested that the maturation of the seeding track was associated with its narrowing and eventual dissipation due to expansion of the tops of the ambient clouds from the sides inward. 相似文献
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1. Introduction Clouds are active factors in the climate system, and have significant influences on the global hydrolog- ical and thermal budgets. More and more the climate model developers and researchers have realized the im- portance to appropriately describe the interactions be- tween cloud and radiation in the atmospheric general circulation model (AGCM). It is well known that cloud is one of the contributing factors to the uncertainties in the simulation of climate by AGCM. Especiall… 相似文献
998.
泡沫潜孔锤在水文水井钻探中的应用前景 总被引:3,自引:1,他引:2
介绍了泡沫潜孔锤的结构及工作原理,阐述了其优点及在水井钻探中的应用前景。 相似文献
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