Band selection using sparse nonnegative matrix factorization with the thresholded Earth’s mover distance for hyperspectral imagery classification     

Weiwei Sun  Weiyue Li  Jialin Li  Yenming Mark Lai 《Earth Science Informatics》2015,8(4):907-918

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论地球数据科学与共享     

诸云强  孙九林  王卷乐  杨雅萍 《国土资源信息化》2015,(1):3-9

地球科学大数据的到来,迫切需要通过地球数据科学系统对地学数据机理、采集处理、存储管理,特别是集成共享与挖掘分析等进行研究,以便通过大数据资源,发现和揭示数据背后隐含的地学规律和知识,促进地学科技创新。本文首先分析了地球数据科学的内涵特征,提出了地球数据科学的基础理论方法和技术体系。然后基于国家地球系统科学数据共享实践,重点研究了大数据时代下,面向地球数据科学的地学数据共享新发展。  相似文献   

新型城镇化下中国城市土地集约利用格局与机理研究   总被引：4，自引：0，他引：4  

李晓玲  修春亮  孙平军 《世界地理研究》2015,(1):60-67

基于城市土地集约利用内涵,文中从利用强度、投入水平和产出效益三个方面构建城市土地集约利用评价体系,并选取287个城市为研究单元,分析了2011年中国城市土地集约利用格局与机理。结果表明:中国城市土地集约利用水平呈现出由东向西依次递减的趋势;沿海地区、"T"字轴地区、长江流域沿线地区的城市土地集约利用水平高于其周围城市地区;城市土地集约利用水平分布的空间集聚性明显,集约利用城市和中度利用城市呈点状、间隔分布,低度利用城市和粗放利用城市呈面状、连续分布;总体来说,城市土地集约利用水平仍比较低;机理分析归结为经济因子、生态因子、社会因子和技术进步因子四个方面,并指出对现有体制进行完善是提高城市土地集约利用水平的根本途径。  相似文献   

极地冰盖物质平衡的最新进展与未来挑战          下载免费PDF全文

王慧孙波  李斐唐学远  崔祥斌王甜甜 《极地研究》2015,27(3):326-336

准确地探明冰盖物质平衡状况,对于研究全球变暖背景下海平面变化具有重要的意义,自IPCC AR4(政府间气候变化专门委员会第四次报告)以来,极地冰盖物质平衡的研究取得了很大进展。本文总结并对比了用卫星测高(雷达测高和激光测高)、物质收支测量和重力测量等方法得到的冰盖物质平衡评估结果,综述了冰盖数值模拟研究在预测冰盖未来的变化趋势以及由此对海平面造成的影响等方面取得的进展,并立足于中国当前的极地冰盖物质平衡研究现状,提出了该研究所面临的挑战。  相似文献   

Elemental composition and its environmental significance for the varicolored hills in the northern foothills of the Qilian Mountains of Sunan Yugur Autonomous County, China     

CaiXia Zhang  XiaoZe Li  Zhong Sun  JinChang Li 《寒旱区科学》2015,7(3):257-264

The varicolored hills in the northern foothills of the Qilian Mountains of northern China, in the Hexi Corridor of Gansu Province's Sunan Yugur Autonomous County, have given this region a unique geomor...  相似文献   

Influence of fines content on the anti-frost properties of coarse-grained soil     

TianLiang Wang  ZuRun Yue  TieCheng Sun  JinChuang Hua 《寒旱区科学》2015,7(4):407-413

This paper aims to determine the optimal fines content of coarse-grained soil required to simultaneously achieve weaker frost susceptibility and better bearing capacity. We studied the frost susceptibility and strength properties of coarse-grained soil by means of frost heaving tests and static triaxial tests, and the results are as follows:(1) the freezing temperature of coarse-grained soil decreased gradually and then leveled off with incremental increases in the percent content of fines; (2) the fines content proved to be an important factor influencing the frost heave susceptibility and strength properties of coarse-grained soil. With incremental increases in the percent content of fines, the frost heave ratio increased gradually and the cohesion function of fines effectively enhanced the shear strength of coarse-grained soil before freeze-thaw, but the frost susceptibility of fines weakened the shear strength of coarse-grained soil after freeze-thaw; (3) with increasing numbers of freeze-thaw cycles,the shear strength of coarse-grained soil decreased and then stabilized after the ninth freeze-thaw cycle, and therefore the mechanical indexes of the ninth freeze-thaw cycle are recommended for the engineering design values; and (4) considering frost susceptibility and strength properties as a whole, the optimal fines content of 5% is recommended for railway subgrade coarse-grained soil fillings in frozen regions.  相似文献   

Influence of flow velocity and spatial heterogeneity on DNAPL migration in porous media: insights from laboratory experiments and numerical modelling   总被引：1，自引：0，他引：1  

Fei Zheng  Yanwei Gao  Yuanyuan Sun  Xiaoqing Shi  Hongxia Xu  Jichun Wu 《Hydrogeology Journal》2015,23(8):1703-1718

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Tropical Cyclone Size Change under Ocean Warming and Associated Responses of Tropical Cyclone Destructiveness: Idealized Experiments     

Zanmin Xu  Yuan Sun  Tim Li  Zhong Zhong  Jia Liu  Chen Ma 《Acta Meteorologica Sinica》2020,34(1):163-175

The power dissipation index (PDI), which is defined as the sum of the cube of tropical cyclone (TC) maximum wind speed during TC lifetime, is widely used to estimate the TC destructive potential. However, due to the lack of high-resolution observations, little attention has been paid to the contribution of TC size change to TC destructive potential in response to ocean warming. In this study, sensitivity experiments are performed by using the high-resolution Weather Research and Forecasting (WRF) model to investigate the responses of TC size and TC destructive potential to prescribed sea surface temperature (SST) increase under the present climate condition. The results show that TC size increases with the ocean warming. Possible reasons for TC size change are investigated with a focus on the outer air-sea moisture difference (ASMD). As SST increases, ASMD in the outer zone of the TC is larger than that in the inner zone, which increases the surface entropy flux (SEF) of the outer zone. This change in the radial distribution of SEF causes the increase of tangential wind in the outer zone, which further increases SEF, resulting in a positive feedback between outer-zone SEF and outer-zone tangential wind. This feedback leads to the increase of the radius of gale-force wind, leading to the expansion of TC size. Moreover, to estimate the contribution of TC size change to TC destructiveness, we calculate TC size-dependent destructive potential (PDS) as the storm size information is available in the model outputs, as well as PDI that does not consider the effect of TC size change. We find that PDS increases exponentially as SST increases from 1 to 4°C, while PDI increases linearly; hence the former is soon much greater than the latter. This suggests that the growth effect of TC size cannot be ignored in estimating destructiveness under ocean warming.  相似文献   

内蒙古巴彦淖尔市一次强降水过程诊断分析     

孙令东  王永清  梁凤娟 《气象与环境科学》2013,36(3):34-38

运用常规气象资料和自动站实测资料,从低涡系统的演变规律及物理机制等方面对2010年9月6-9日发生在内蒙古巴彦淖尔市一次强降水过程进行诊断分析.结果表明:此过程是在中高纬稳定的大尺度环流背景下,由地面气旋、低涡和副热带高压共同作用下产生的,东移的冷空气与西南暖湿气流在巴彦淖尔市上空交绥是造成此次强降水的主要原因.充足、稳定的水汽输送和较强的水汽辐合,为此次强降水提供了充足的水汽条件.高空强烈的辐散,通过抽吸作用引起低层强烈的辐合,从而促使垂直上升运动增强,是此次降水天气发生的动力.500 hPa层以上大气层结稳定,阻挡暖湿空气向上输送,促使不稳定能量在500 hPa层以下积累,为此次强降水发生提供了足够的能量条件.850 hPa偏东风暖湿气流受阴山的阻挡和抬升,降水量增加,而山后降水量减少.乌拉山与白云查汗山形成狭长山谷,边界层东风气流穿过,狭管效应有利于此地风速增大,将大量的水汽输送到巴彦淖尔市上空.  相似文献   

江西省北部一次冰雹过程可预报性分析          下载免费PDF全文

孙素琴  刘文英  郑婧 《气象与减灾研究》2020,43(3):194-202

利用EC数值预报产品对2018年江西省北部一次降雹过程的高空形势及相关物理量预报场进行分析,结果表明：高空槽、低层切变线、地面倒槽辐合线,“上干冷下暖湿”的层结分布及冷锋前部近乎稳定层结存储的中等到强的不稳定能量,中等到强的垂直风切变,持续偏强的上升运动等,是此次冰雹天气发生的主要原因。EC数值预报模式对于天气尺度系统、中小尺度辐合线、对流有效位能及上升运动等有一定的预报能力,特别是对0 ℃和-20 ℃高度和整层的垂直环境层结预报效果很好,具有明显的“上干冷下暖湿”特征;但对于地面温度湿度预报出现系统性偏低,对低层西南急流预报较实况偏小,有其一定的局限性。  相似文献