首页 | 本学科首页   官方微博 | 高级检索  
文章检索
  按 检索   检索词:      
出版年份:   被引次数:   他引次数: 提示:输入*表示无穷大
  收费全文   469篇
  免费   107篇
  国内免费   54篇
测绘学   70篇
大气科学   46篇
地球物理   160篇
地质学   86篇
海洋学   230篇
天文学   11篇
综合类   18篇
自然地理   9篇
  2024年   1篇
  2023年   3篇
  2022年   24篇
  2021年   25篇
  2020年   30篇
  2019年   35篇
  2018年   22篇
  2017年   34篇
  2016年   24篇
  2015年   26篇
  2014年   31篇
  2013年   49篇
  2012年   40篇
  2011年   39篇
  2010年   31篇
  2009年   38篇
  2008年   29篇
  2007年   36篇
  2006年   26篇
  2005年   18篇
  2004年   13篇
  2003年   13篇
  2002年   8篇
  2000年   5篇
  1999年   10篇
  1998年   5篇
  1997年   3篇
  1995年   1篇
  1994年   4篇
  1993年   3篇
  1992年   1篇
  1957年   1篇
  1954年   2篇
排序方式: 共有630条查询结果,搜索用时 15 毫秒
51.
52.
IP地址绑定和IP用户管理是校园网管理员的主要工作,作者介绍哈尔滨工业大学校园网IP地址绑定和IP用户管理系统的设计思路及实现技术,该系统是采用J2EE技术和Struts+Hibernate框架实现的B/S结构WEB应用系统,用于校园网用户的IP地址分配I、P地址绑定及IP用户管理等方面。该系统的实现与应用大大提高了网络管理员的工作效率、避免了操作失误、改善了对用户的服务质量。  相似文献   
53.
利用黑龙江省1981-2010年的土壤湿度数据,以富锦县、龙江县、双城县、黑河市、海伦县为代表点,分析了黑龙江省东、西、南、北、中各区域封冻前(11月8日)0~30 cm土层土壤湿度的趋势变化和干湿变化,采用线性趋势、5年滑动平均和Mann-Kendall法检验变化趋势,利用Mann-Kendall和Yamamoto法对土壤湿度变化趋势进行突变点检验.结果表明:封冻前0~30 cm土层各地土壤湿度在30年间均有不同程度下降,西部龙江县下降剧烈,中部海伦县较剧烈,北部黑河市和南部双城县次之,上述代表点20 cm土层土壤湿度下降均达到了P<0.05以内的显著水平,东部富锦县下降趋势最弱;经Mann-Kendall法检验,0~30 cm土层龙江县、海伦县土壤湿度出现了下降的突变区域,其余代表点的土壤湿度变化趋势在近几年中逐渐接近或已经超越了显著线;1994年是龙江县10 cm、20 cm土壤湿度下降的突变时期;黑龙江省各地土壤湿度的下降与封冻前一段时期内气温和降水变化密切相关,还与土壤物理性质的恶化等因素有关.  相似文献   
54.
The development of robust and accurate methods for automatic registration of optical imagery and 3D LiDAR data continues to be a challenge for a variety of applications in photogrammetry, computer vision and remote sensing. This paper proposes a new approach for the registration of optical imagery with LiDAR data based on the theory of Mutual Information (MI), which exploits the statistical dependency between same- and multi-modal datasets to achieve accurate registration. The MI-based similarity measures quantify dependencies between aerial imagery, and both LiDAR intensity data and 3D point cloud data. The needs for specific physical feature correspondences, which are not always attainable in the registration of imagery with 3D point clouds, are avoided. Current methods for registering 2D imagery to 3D point clouds are first reviewed, after which the mutual MI approach is presented. Particular attention is given to adoption of the Normalised Combined Mutual Information (NCMI) approach as a means to produce a similarity measure that exploits the inherently registered LiDAR intensity and point cloud data so as to improve the robustness of registration between optical imagery and LiDAR data. The effectiveness of local versus global similarity measures is also investigated, as are the transformation models involved in the registration process. An experimental program conducted to evaluate MI-based methods for registering aerial imagery to LiDAR data is reported and the results obtained in two areas with differing terrain and land cover, and with aerial imagery of different resolution and LiDAR data with different point density are discussed. These results demonstrate the potential of the MI and especially the CMI methods for registration of imagery and 3D point clouds, and they highlight the feasibility and robustness of the presented MI-based approach to automated registration of multi-sensor, multi-temporal and multi-resolution remote sensing data for a wide range of applications.  相似文献   
55.
欧亚大陆春季融雪与长江流域夏季降水的可能联系   总被引:1,自引:1,他引:0       下载免费PDF全文
韩冬  陈海山  许蓓  齐铎  吴波 《气象科学》2014,34(3):237-242
利用1979—2007年全球月平均的积雪水当量资料,定义了春季积雪水当量增量指数,该指数可以较为直观地反映春季融雪的情况。通过这一纽带,分析了欧亚大陆春季融雪与长江流域夏季降水之间的联系。研究表明:欧亚大陆春季融雪与中国长江流域夏季降水是负相关关系,这与高原积雪的影响是不一致的。春季融雪量的减少,使得欧亚大陆北部夏季剩余积雪偏多,夏季融雪增多。融雪的局地效应使得土壤湿度增加,加大了欧亚大陆南北热力差异。从而,夏季中纬度的纬向风切变增大,对流层上层的副热带西风急流增强,副热带高压增强西伸,但是北抬受到抑制。长江流域位于异常西南暖湿气流与冷空气的辐合带上,上升运动活跃,有利于降水偏多。  相似文献   
56.
Recently derived (Webster et al., 2011), simplified higher-level Green–Naghdi equations (GN-3, GN-5 and GN-7) are used in this work to simulate the transformation of two-dimensional, shallow-water wave problems. The spatial derivatives are discretized through a five-point difference scheme. A new algorithm is developed to solve the resulting block-pentadiagonal matrix. These high-level GN equations are then utilized to develop a numerical wave tank. A wave-maker is placed at the forcing boundary of the tank that uses the stream-function theory to generate nonlinear incident waves. The numerical wave tank is used to analyze the effects of large-amplitude waves passing over a submerged bar. A damping zone is placed near the wave-maker (up-wave side) to absorb the reflected waves from the front side of the submerged bar. Another damping zone is placed at the down-wave side of the computational domain to absorb the radiated waves. In the first test case, the front and back slopes of the bar are both mild (Luth et al., 1994). The waves that evolved over the bar are simulated by using the GN-3, GN-5 and GN-7 equations. The GN-3 equations provide time histories that compare well with the experimental data at different wave gauges, except at the ones behind the bar. The results of the GN-5 and GN-7 equations compare very well with all the experimental data considered here. In the second test case, the front and back slopes of the bar are both steep (Ohyama et al., 1995). The GN-5 equations predict the wave elevation well. In the third test case, the front and back slopes of the bar alternate, one of them being mild and the other one being steep (Zou et al., 2010). Again, the predictions of the GN-5 equations agree with the experimental data well. In all the test cases considered in this work, there are some differences between the GN-3 and GN-5 results after the crest of the bar. Numerical results obtained by the GN-5 and GN-7 equations are almost the same along the wave flume, but the GN-7 equations require more computational time. Therefore, the GN-5 results are accepted here as the converged GN theory results. The numerical validations show that the GN-5 equations can simulate the strongly nonlinear and dispersive waves observed behind the submerged bar crest satisfactorily.  相似文献   
57.
In order to study hydrodynamic performance of a propeller in the free surface, the numerical simulation and open-water experiments are carried out with varying shaft depths of propeller. The influences of shaft depths of a propeller on thrust and torque coefficient in calm water are mainly studied. Meanwhile, this paper also studies the propeller air-ingestion under special working conditions by experiment and theoretical calculation method, and compares the calculation results and experimental results. The results prove that the theoretical calculation model used in this paper can imitate the propeller air-ingestion successfully. The successful phenomenon simulation provides an essential theoretical basis to understand the physical essence of the propeller air-ingestion.  相似文献   
58.
Owing to the existence of the flow field boundary, the shock wave load near the boundary is different from the freefield shock wave load. In the present paper, the hull plate load subjected to underwater shock wave is investigated based onwave motion theories; in addition, the experimental study of the hull plate load is carried out. According to the theoreticalanalysis of the hull plate pressure, we find that the hull plate pressure oscillates repeatedly and decays rapidly with timepassing, the maximum hull plate pressure is 2/(1+n) times the maximum free field pressure, where n is the ratio ofimpedance, and the impulse is much smaller than the free field impulse. Compared with the experimental study, thetheoretical results agree well with the experimental data.  相似文献   
59.
在时域内分析深水钢悬链立管在平台运动和波流载荷共同作用下的非线性动力响应;采用雨流计数法处理立管节点应力的时间历程,选用DoE.E型S-N曲线分析立管在单一海况和平台运动联合作用下的疲劳损伤;将各方向含概率分布的疲劳损伤进行叠加,得到立管整体的全方向疲劳损伤及疲劳寿命。平台的运动为六自由度的运动预报数据,波流载荷由某海域实际的波浪统计数据采用Morison公式计算所得。计算结果表明钢悬链立管疲劳寿命的极值点分别位于悬挂点附近和触地点附近,对立管疲劳寿命极值点各方向疲劳损伤分布情况进行了分析。所提方法为钢悬链立管疲劳分析提供了新思路,给出的结论对钢悬链立管设计分析有一定借鉴意义。  相似文献   
60.
This paper describes the geometric in-flight calibration of the Modular Optoelectronic Multispectral Scanner MOMS-2P, which has collected digital multispectral and threefold along-track stereoscopic imagery of the earth's surface from the PRIRODA module of the Russian space station MIR from October 1996 to August 1999. The goal is the verification and, if necessary, the update of the calibration data, which were estimated from the geometric laboratory calibration. The paper is subdivided into two parts, describing two different procedures of geometric in-flight calibration. The first method is based on DLR matching software and is restricted to nadir looking channels, which are read out simultaneously. From a high number of individual point matches between the images of the same area taken by the different CCD arrays, the most reliable ones are selected and used to calculate shifts with components in and across flight direction between the CCD arrays. These actual shifts are compared to the nominal shifts, derived from the results of the laboratory calibration, and parameters of the valid camera model are estimated from both data sets by least squares adjustment. A special case of band-to-band registration are the two optically combined CCD-arrays of the nadir high-resolution channel. They are read out simultaneously with a nominal 10 pixel overlap in stereoscopic imaging mode A. The DLR matching software is applied to calculate the displacement vector between the two CCD-arrays. The second method is based on combined photogrammetric bundle adjustment using an adapted functional model for the reconstruction of the interior orientation. It requires precise and reliable ground control information as well as navigation data of the navigation-package MOMS-NAV. Nine contiguous image scenes of MOMS-2P data-take T083C building an about 550-km-long strip over southern Germany and Austria taken in March 1997 were evaluated. From both procedures calibration data are estimated, which are presented and compared to the lab-calibration results.  相似文献   
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号