河南省春季降水量的时空分布   总被引：1，自引：1，他引：0  

康雯瑛  焦建丽  王君  梅新建 《气象与环境科学》2008,31(Z1)

利用河南省分布均匀的60个测站1961-2006年春季降水量资料,采用线性趋势、多项武拟合、最大熵谱分析、EOF等方法对河南省春季降水量的年际、年代际变化及时空分布特征进行分析,结果显示:河南省春季降水量空间分布南北差异较大,呈现南多北少;春季旱年多于涝年,尤其4、5月偏旱的年份显著多于偏涝年;春季降水量的线性趋势不明显.年际变化具有显著的5 a振荡周期;春季及其各月降水量场第一特征向量呈现全省一致型,其方差贡献率达70%左右,全省春季同涝同旱特征显著.  相似文献   

遥感、GIS结合与区域天然滑坡调查   总被引：4，自引：0，他引：4       下载免费PDF全文

单新建  李焯芬等 《地质论评》2001,47(6):648-652

以香港大屿山岛中部为试验研究区，探讨了遥感与GIS结合在区域滑坡调查中应用的可能性。在详细分析滑坡与环境因子关系后，将岩土类型、地貌、侵蚀、坡度等环境因子引入到影像中，与影像组成多源复合图像，可使地物的空间属性信息得到补充。同时采用适合高维复合数据的BP神经元网络对研究区天然滑坡进行识别，结果表明，区域滑坡的识别能力有较大提高。该方法的应用，将为大区域滑坡调查与监测奠定基础。  相似文献   

误差Mohr圆及协因数不变量     

寇新建 《测绘工程》1995,(2)

作者以Mohr圆表示了平面坐标系中点位协因数的各分量。本法不仅能给出任意方向上的自协因数,也可容易表示出两正交方向间的互协因数。Mohr圆不仅全面地反映了一点的误差状态,并可解决位移检验等实际问题。文中还指出,三维空间点坐标的协因数阵存在3个与坐标系无关的不变量。  相似文献   

两斜井间贯通测量方案设计     

宋丽洁  刘杨  王新建 《北京测绘》2021,35(4):516-519

本文根据贯通测量的原理,设计了主斜井及回风斜井的贯通测量方案,包括地面的平面控制测量、高程控制测量、斜井联系测量以及井下的导线测量和高程测量,最后对两巷道在水平和竖直方向上的误差进行分析,利用得出的结论判断两井巷之间是否能够准确贯通.方案设计的最终结果表明:两斜井的贯通在水平和竖直方向上均未超出规定限差,方案能够满足贯通要求.  相似文献   

新疆测震台网历史监测能力及现状   总被引：3，自引：2，他引：3  

单新建  韩京 《内陆地震》1996,10(1):61-67

文中计算了新疆从始建区域测震台网到１９９４年止主要几次变动的台网监测能力。总结出震级Ｍ＿Ｌ、震中距、周期和最大Ｓ波振辐之间的关系。最后又把新疆区域台网和新建的乌鲁木齐遥测台网组合到一起，展望了新疆测震台网未来的监测能力。  相似文献   

秩亏网平差基准条件的物理解释     

寇新建  宋计棉 《测绘工程》1996,(2)

引用能量力学理论,说明了最小势能原理与秩亏网平差中极小方差原则的一致性,并对具有普遍意义的加权秩亏网平差基准的实质作了物理解释,使这一平差方法的含意更为明确、直观。本文的结果不仅适用于普通秩亏网平差,也适用于加权与拟稳平差。从物理角度说明秩亏网平差基准的含意,可加深人们对平差结果性质的认识,因而更有利于工程技术人员选择合适的方法解决实际问题。  相似文献   

Late Pliocene–recent tectonic setting for the Tianchi volcanic zone, Changbai Mountains, northeast China     

Yu Wang  Chunfeng Li  Haiquan Wei  Xinjian Shan 《Journal of Asian Earth Sciences》2003,21(10):1159

Mafic volcanic rocks have erupted in the Tianchi volcanic zone, Changbai Mountains, northeast China, since late Pliocene time. The zone formed in an extensional environment during early-middle Cenozoic time, and in a compressional environment during late Cenozoic. Crustal thickness (about 40 km) in the Changbai Mountains is larger than the regional average of 34–36 km to the northwest and southeast. The conduit for magma upwelling was not coincident with the NE-striking regional faults, but seem to be confined to a deep-seated NW–WNW-striking fault zone. Since the late Pliocene, the Tianchi volcanic zone was subjected to crustal uplift within an intracontinental, weakly compressional environment (with minor WNW–ESE shearing) related to the westward subduction of the West Pacific plate. The nature of this volcanism is not typical of active, subduction-related continental margin volcanism. The magmatic evolutionary process evolved from trachybasalt through basaltic trachyandesite, trachyte, and pantellerite.  相似文献   

A Characteristic Analysis of the Dynamic Evolution of Preseismic- Coseismic-Postseismic Interferometric Deformation Fields Associated with the M 7.9 Earthquake of Mani, Tibet in 1997   总被引：1，自引：0，他引：1       下载免费PDF全文

SHAN Xinjian ZHANG Guohong 《《地质学报》英文版》2007,81(4):587-592

By using the D-InSAR technique,we have acquired the temporal-spatial evolution images of preseismic-cosesimci-postseismic interferometric deformation fields associated with the M 7.9 earthquake of Mani,Tibet on 8 November 1997.The analysis of these images reveals the relationships between the temporal-spatial evolution features of the interferometric deformation fields and locking, rupturing,and elastic restoring of the source rupture plane,which represent the processes of strain accumulation,strain release,and postseismic restoration.The result shows that 10 months prior to the Mani event,a left-lateral shear trend appeared in the seismic area,which was in accordance with the earthquake fault in nature.The quantity of local deformation on the north wall was slightly larger than that on the south wall,and the deformation distribution area of the north wall was relatively large.With the event impending,the deformation of the south wall varied increasingly,and the deformation center shifted eastward.Two and half monthd before the event,the west side of the fault was still locked while the east side began to slide,implying that the whole fault would rupture at any moment.These features can be regarded as short-term precursors to this earthquake.Within the period from 16 April 1996 to two and half months before the earthquake,the most remarkable deformation zones appeared in the north and south walls,which were parallel to and about 40 km apart from the fault,with accumulated local displacements of 344 mm and 251 mm on the north and south walls,respectively.The south wall was the active one with larger displacements.Five months after the earthquake,the distribution feature of interferometric fringes was just opposite to that prior to the event,expressing evident right-lateral shear.The recovered displacements are～179 mm on the north wall and～79 mm on the south wall,close to the east side of the fault.However,in the area of the south wall far from the fault there still existed a trend of sinistral motion.The deformation of the north wall was small but recovered fast in a larger area,while the active south wall began to recover from the east section of the fault toward the WSW.  相似文献   

市（地）级人工增雨决策指挥系统          下载免费PDF全文

魏慧娟  崔新建  杨国锋  王静  张俊波  袁春风 《气象》2007,33(12):110-115

介绍了驻马店市人工增雨作业指挥系统的结构、技术要点、功能和应用情况。系统将作业需求分析、作业潜势预报、作业条件判别、作业现场指挥与反馈、作业效果分析评估、作业信息共享等功能有机地融合,为市、县增雨作业提供了可视化、可操作性强、自动化程度高的业务技术平台和决策指挥平台。  相似文献   

人工增雨火箭发射仰角及用弹量的估算     

王志强  易亮  袁文良  祝新建  王志刚 《河南气象》2007,(Z1)

根据南阳气象观测站探空资料及AgI在云中成核率与温度的关系,确定了豫南BL-1型火箭人工增雨可播云体的判别标准、火箭发射仰角及火箭用弹量。  相似文献