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旅游流对区域旅游开发规划具有重要指导作用,如何实现旅游流与区域经济、社会、自然环境的协调发展成为许多地区亟待思考的问题。该文借助社会网络理论和方法研究区域旅游流网络结构体系,从经济、社会、自然环境角度分析区域旅游流网络结构的环境影响因子;通过构建耦合协调度模型测量环境因子对区域旅游流网络结构的影响强度,并利用Moran指数对区域旅游流网络结构与环境的耦合协调度进行全局及局部自相关分析。最后以京津冀地区为例,探查该地区旅游流网络结构与环境的响应效果,为区域旅游流网络结构优化提供决策参考。 相似文献
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The Chang'E-1 and Chang'E-2 missions have successfully obtained a huge amount of ltmar scientific data, through the seven onboard instruments including a CCD stereo camera, a laser altimeter, an interference imag- ing spectrometer, an X-ray spectrometer, a microwave radiometer, a high-energy particle detector and a solar-wind ion detector. Most of the Chang'E data are now publicly available to the science community, and this article serves as an official guide on how these data are classified and organized, and how they can be retrieved from http://159.226.88.59:7779/CE1OutENGWeb/. This article also presents the detailed specifications of various instru- ments and gives examples of research progress made based on these instruments. 相似文献
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基于全国2 419个气象站1980—2018年逐日气象观测资料,利用Mann-Kendall突变检验、滑动t检验、空间自相关及标准差椭圆等方法,选取4个典型的极端高温指数,分析了中国极端高温事件时空格局演变特征。结果表明:① 中国近40 a来夏天日数、热夜日数、暖夜日数和暖昼日数均呈显著的上升趋势,4个指数均在20世纪80、90年代偏少,2000年以后逐渐增加,4个极端高温指数均在2000年左右发生显著变化。② 4种极端高温指数的空间自相关主要是以高?高和低?低2种空间聚集形态为主,夏天日数和热夜日数的聚集性较强,近40 a来暖夜日数和暖昼日数的空间聚集性先增强后减弱,且空间聚集性分布格局由高?高包围低?低转变为低?低包围高?高。③ 4个指数变化率最大的站点均位于南方地区,其中夏天日数变化率最大的站点呈东西向分布格局,其余3个指数变化率最大的站点呈南北向分布格局,西南、西北地区交界地带夏天日数和暖昼日数在近40 a来变化率均显著高于全国其他地区,华东沿海地区暖夜日数的变化趋势方向性分布最明显,且变化趋势高于全国其他地区。 相似文献
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在三角高程对向观测法理论的基础上,根据对向观测法的闭合差条件,提出其偶然误差特性的检验,并结合数例进行包括闭合差正负号检验、正负误差分配顺序检验、误差数值和的检验和个别误差值的检验.最后得出三角高程对向观测法闭合差具有偶然误差特性,并具有一定的正确性和现实指导意义. 相似文献
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The indirect boundary element method is used to study the 3D dynamic response of an infinitely long alluvial valley embedded in a saturated layered half-space for obli- quely incident SV waves. A wave-number transform is first applied along the valley's axis to reduce a 3D problem to a 2D plane strain problem. The problem is then solved in the section perpendicular to the axis of the valley. Finally, the 3D dynamic responses of the valley are obtained by an inverse wave-number transform. The validity of the method is con- firmed by comparison with relevant results. The differences between the responses around the valley embedded in dry and in saturated poroelastic medium are studied, and the effects of drainage conditions, porosity, soil layer stiffness, and soil layer thickness on the dynamic response are dis- cussed in detail resulting in some conclusions. 相似文献