全文获取类型
收费全文 | 80篇 |
免费 | 14篇 |
国内免费 | 11篇 |
专业分类
测绘学 | 14篇 |
大气科学 | 6篇 |
地球物理 | 15篇 |
地质学 | 40篇 |
海洋学 | 17篇 |
天文学 | 5篇 |
综合类 | 4篇 |
自然地理 | 4篇 |
出版年
2023年 | 2篇 |
2022年 | 4篇 |
2021年 | 5篇 |
2020年 | 3篇 |
2019年 | 2篇 |
2018年 | 4篇 |
2017年 | 3篇 |
2016年 | 5篇 |
2015年 | 3篇 |
2014年 | 7篇 |
2013年 | 4篇 |
2012年 | 10篇 |
2011年 | 7篇 |
2010年 | 5篇 |
2009年 | 4篇 |
2008年 | 5篇 |
2007年 | 4篇 |
2005年 | 1篇 |
2004年 | 4篇 |
2003年 | 5篇 |
2002年 | 6篇 |
2001年 | 4篇 |
2000年 | 3篇 |
1999年 | 5篇 |
排序方式: 共有105条查询结果,搜索用时 15 毫秒
1.
2030年前实现碳达峰、2060年前实现碳中和(简称“双碳”)是我国对国际社会的庄严承诺,已被纳入生态文明建设的总体布局。生态系统碳汇是实现“双碳”目标的重要手段,也是林业和草原实现高质量发展的必然要求。国际有关机构对全球森林、草地和湿地生态系统的碳储量和碳循环进行了评估。自1990年以来,附件一国家(指《联合国气候变化框架公约》附件一列出的经济合作发展组织中所有发达国家和经济转型国家)对本国的碳排放和碳汇进行估算,编制了年度温室气体清单; 我国也编制了5次国家温室气体清单。这些工作对我国开展应对气候变化的研究提供了基础。提出了如下建议: 在编制“双碳” 路线图和时间表时,既要考虑我国生态系统碳汇与能源和工业领域碳排放在区域空间分布和时间维度上的差异性,也要考虑生态系统同时所具有的碳汇和碳排放的特殊性; 生态系统碳汇是碳达峰的非选项,是碳中和的必选项; 生态系统碳汇要遵循国家实现“双碳”目标的基本原则,要将生态系统碳汇作为国家生态建设和保护工程的主要目标,提高碳汇计量和监测能力,完善市场和融资机制。 相似文献
2.
Björn Heincke Thomas Günther Einar Dalsegg Jan Steinar Rønning Guri Venvik Ganerød Harald Elvebakk 《Journal of Applied Geophysics》2010,70(4):292-306
We present a combined 3-D geoelectric and seismic tomography study conducted on the large Åknes rockslide in western Norway. Movements on the slope are strongly influenced by water infiltration, such that the hydrogeological regime is considered as a critical factor affecting the slope stability. The aim of our combined geophysical study was to identify and visualize the main shallow tension fractures and to determine their effect on hydraulic processes by comparing the geophysical results with information from borehole logging and tracer tests. To resolve the complex subsurface conditions of the highly fractured rock mass, a three-dimensional set-up was chosen for our seismic survey. To map the water distribution within the rock mass, a pattern of nine intersecting 2-D geoelectric profiles covered the complete unstable slope. Six of them that crossed the seismic survey area were considered as a single data set in a 3-D inversion. For both methods, smoothing-constraint inversion algorithms were used, and the forward calculations and parameterizations were based on unstructured triangular meshes. A pair of parallel shallow low-velocity anomalies (< 1400 m/s) observed in the final seismic tomogram was immediately underlain by two anomalies with resistivities <13 kΩm in the resistivity tomogram. In combination with borehole logging results, the low-velocity and resistivity anomalies could be associated with the drained and water-filled part of the tension fractures, respectively. There were indications from impeller flowmeter measurements and tracer tests that such tension fractures intersected several other water-filled fractures and were responsible for distinct changes of the main groundwater flow paths. 相似文献
3.
Bathymetry enhancement by altimetry-derived gravity anomalies in the East Sea (Sea of Japan) 总被引:1,自引:0,他引:1
Kwang Bae Kim Yu-Shen Hsiao Jeong Woo Kim Bang Yong Lee Yi Kyun Kwon Chang Hwan Kim 《Marine Geophysical Researches》2010,31(4):285-298
The gravity-geologic method (GGM) was used to enhance the bathymetry of the East Sea (Sea of Japan) with satellite altimetry-derived
free-air gravity anomalies and shipborne depth measurements. By comparison with the bathymetry model of Smith and Sandwell’s
(SAS) approach (1994), GGM was found to have an advantage with short wavelength (≤12 km) components, while SAS better predicts
longer wavelength (≥25 km) components, despite its dependency on density contrast. To mitigate this limitation, a tuning density
contrast of 10.25 g/cm3 between seawater and the seafloor was primarily estimated by the downward continuation method and then validated by the check
points method with GGM. Similarly, SAS is limited by the “A” value in low-pass part of the Wiener filter, which defines the effective range of the wavelength components on bathymetry.
As a final result, we present an enhanced GGM bathymetry model by integrating all available data. 相似文献
4.
断裂趋势带是指盆地基底断裂继承性活动或盖层受到剪切作用影响而产生在盖层中的弱变形构造带,是主断裂面形成前的变形程度较弱的构造带。研究发现,东营凹陷南斜坡王家岗和八面河断裂趋势带是由一系列雁列式排列小断层带组成的,具有上宽下窄,下部收敛于主走滑断裂的特点。由于浅层没有主断层显现,故也称这种构造带为隐性断裂带,其形成机制和变形程度不同,发育的圈闭数量、圈闭性质等特征不同,富集油气的能力也有差异。构造物理模拟实验表明,王家岗和八面河断裂趋势带都形成于基底断裂走滑—伸展双重作用,前者走滑—伸展运动方向夹角为40°~50°,后者夹角为20°左右。前者处于断裂带发育的幼年期,变形程度较弱,趋势带宽度小,断裂密度小;后者处于断裂带发育的青年期,变形程度强,趋势带宽度大,断裂密度大,形成与断裂相关的圈闭数量多,油气聚集能力高于前者。根据断裂趋势带演化阶段、发育特征和源藏匹配关系,认为断裂趋势带变形强度是控制油气富集程度的关键因素。王家岗断裂趋势带成藏模式为“幼年期弱变形—单洼供烃成藏模式”,八面河断裂趋势带成藏模式为“青年期强变形—双洼供烃成藏模式”。 相似文献
5.
Ayman F. Habib Ana Paula Kersting Ki-In Bang Ruifang Zhai Mohannad Al-Durgham 《The Photogrammetric Record》2009,24(126):171-195
Lidar (laser scanning) technology has been proven as a prominent technique for the acquisition of high-density and accurate topographic information. Because of systematic errors in the lidar measurements (drifts in the position and orientation information and biases in the mirror angles and ranges) and/or in the parameters relating the system components (mounting parameters), adjacent lidar strips may exhibit discrepancies. Although position and orientation drifts can have a more significant impact, these errors and their impact do not come as a surprise if the quality of the GPS/INS integration process is carefully examined. Therefore, the mounting errors are singled out in this work. The ideal solution for improving the compatibility of neighbouring strips in the presence of errors in the mounting parameters is the implementation of a rigorous calibration procedure. However, such a calibration requires the original observations, which may not be usually available. In this paper, a strip adjustment procedure to improve the compatibility between parallel lidar strips with moderate flight dynamics (for example, acquired by a fixed-wing aircraft) over an area with moderately varying elevation is proposed. The proposed method is similar to the photogrammetric block adjustment of independent models. Instead of point features, planar patches and linear features, which are represented by sets of non-conjugate points, are used for the strip adjustment. The feasibility and the performance of the proposed procedure together with its impact on subsequent activities are illustrated using experimental results from real data. 相似文献
6.
7.
利用中国科学院大气物理研究所9层大气环流模式(IAP9L AGCM)对夏季气候进行了30年( 1970~1999年)集合回报试验,并采用统计学分析方法对跨季度夏季短期气候的可预测性问 题进行了初步探讨. 结果表明,该模式对对流层中、高层大气环流的预测能力强于低层,位 势高度场和表面气温的可预测性最大,而降水的可预测性则相对较小. 对流层中、高层位势 高度场的可预测性基本呈带状分布,越靠近赤道可预测性越高;而降水的可预测性基本局限 于赤道东太平洋及热带个别区域. 由此可见,降水的预测极为困难和复杂,订正系 统的研究和寻找新的预报物理因子非常重要. 相似文献
8.
Decoupling of the East Asian summer monsoon and Indian summer monsoon between 20 and 17 ka 总被引:2,自引:0,他引:2
Xiuyang Jiang Yaoqi He Chuan-Chou Shen Shi-Yu Lee Bang Yang Ke Lin Zhizhong Li 《Quaternary Research》2014
Marine Oxygen Isotope Stage (MIS) 2, with its profound environmental and climatic changes from before the last glacial maximum (LGM) to the last deglaciation, is an ideal period for understanding the evolution of the East Asian summer monsoon (EASM) and Indian summer monsoon (ISM), two Asian monsoon sub-systems. With 875 stable oxygen isotope ratios and 43 230Th dates from stalagmites in Sanxing Cave, southwestern China, we construct and interpret a new, replicated, Asian summer monsoon (ASM) record covering 30.9–9.7 ka with decadal resolution. δ18O records from this site and other reported Chinese caves display similar long-term orbitally dominated trends and synchronous millennial-scale strong and weak monsoonal events associated with climate changes in high northern latitudes. Interestingly, Sanxing δ18O and Arabian Sea records show a weakening ISM from 22 to 17 ka, while the Hulu and Qingtian records from East and Central China express a 3-ka intensifying EASM from 20 to 17 ka. This decoupling between EASM and ISM may be due to different sensitivities of the two ASM sub-systems in response to internal feedback mechanisms associated with the complex geographical or land-ocean configurations. 相似文献
9.
BTOPMC模型与新安江模型在史河上游的应用比较研究 总被引:1,自引:0,他引:1
介绍了一个由TOPMODEL发展而来的基于栅格的分布式水文模型--BTOPMC模型.选取史河流域黄泥庄水文站以上集水面积为研究区域,在空间分辨率为30秒的数字高程模型数据基础上构建数字流域水系,基于IGBP全球陆面土地覆被数据以及FAO全球数字土壤数据运用BTOPMC模型和新安江模型分别对黄泥庄站1982年到1987年的日径流过程进行模拟.采用模拟与实测洪量比和确定性系数对两个模型的模拟结果进行比较分析.结果表明两个模型都能很好地模拟日径流过程,新安江模型有更好的模拟效果. 相似文献
10.