全文获取类型
收费全文 | 893篇 |
免费 | 150篇 |
国内免费 | 196篇 |
专业分类
测绘学 | 94篇 |
大气科学 | 193篇 |
地球物理 | 270篇 |
地质学 | 217篇 |
海洋学 | 228篇 |
天文学 | 8篇 |
综合类 | 45篇 |
自然地理 | 184篇 |
出版年
2024年 | 8篇 |
2023年 | 23篇 |
2022年 | 27篇 |
2021年 | 32篇 |
2020年 | 46篇 |
2019年 | 38篇 |
2018年 | 33篇 |
2017年 | 31篇 |
2016年 | 38篇 |
2015年 | 45篇 |
2014年 | 44篇 |
2013年 | 90篇 |
2012年 | 55篇 |
2011年 | 46篇 |
2010年 | 38篇 |
2009年 | 43篇 |
2008年 | 55篇 |
2007年 | 61篇 |
2006年 | 59篇 |
2005年 | 51篇 |
2004年 | 48篇 |
2003年 | 39篇 |
2002年 | 29篇 |
2001年 | 30篇 |
2000年 | 27篇 |
1999年 | 28篇 |
1998年 | 26篇 |
1997年 | 20篇 |
1996年 | 29篇 |
1995年 | 9篇 |
1994年 | 22篇 |
1993年 | 15篇 |
1992年 | 12篇 |
1991年 | 7篇 |
1990年 | 6篇 |
1989年 | 9篇 |
1988年 | 9篇 |
1987年 | 5篇 |
1986年 | 1篇 |
1984年 | 1篇 |
1979年 | 1篇 |
1978年 | 2篇 |
1977年 | 1篇 |
排序方式: 共有1239条查询结果,搜索用时 15 毫秒
991.
992.
黄金水 《武汉大学学报(信息科学版)》2005,30(6):478-482
根据建立的垂直于大洋中脊的二维热对流有限元数值模型,采用常粘性以及与温度相关的粘性两种粘性结构对小尺度地幔对流对海底地形的影响进行了重新研究。该模型的主要特点是采用开放边界条件,从而可以避免原有封闭模型因回流问题而产生的复杂效应。数据结果显示,在常粘性模型中,小尺度地幔对流可造成海底地形抬升;但对与温度相关的粘性模型,小尺度对流对地形几乎不产生影响。 相似文献
993.
为更好地理解和认识小尺度地形对降水特性的影响,利用位于云贵高原地区相近的两个国家基准站太华山和昆明站2006—2018年雨季(5—10月)小时降水资料,统计分析了两站降水精细化的时空特征。结果表明,两站的海拔高度差约500 m、站距约5 km,暖季降水量差异不大,但降水的精细特征却存在明显差异,主要表现为:(1)两站的降水量和平均降水强度年际差异不明显,但太华山站多数年份的降水频次远多于昆明站;(2)降水日变化上,太华山站在11—20时的累积降水量要高于昆明站;两站降水频次均具有双峰型特征,但在03—09时和11—17时太华山站的降水频次要明显高于昆明站,00—13时和21—23时昆明站的平均降水强度高于太华山站。(3)两站的降水事件特征不同,太华山站的降水事件次数和累积降水量都明显多于昆明站,主要由持续时间在6 h以上的降水事件贡献。(4)两站降水事件主要为共有降水事件,降水特性差异也主要由共有降水事件造成。太华山站先开始(结束)降水的共有降水事件次数比昆明站多(少),持续时间(降水频次)比昆明站长(多),短、长时降水事件的降水量(降水频次)比昆明站大(多),平均降水持续时间比昆明站多0.36 h。(5)两站单独降水事件占总降水事件的39.9%,太华山站的单独降水事件数是昆明站的1.83倍,而且平均持续时间长于昆明站。
相似文献994.
The Plio-Quaternary conglomeratic sets within the marine environment of the Viranşehir coast (W Mersin, S Turkey) are responsible
for the evolution of sandy and gravely beaches due to their control on various factors such as sea floor irregularity, wave
energy, and organic activity. The conglomeratic sets close to the shoreline (50–150 cm) act as wave breakers, creating hard
substratum and high energy, well-oxygenated environment for organisms like Patella sp., Phoronida worms and Brachidontes pharaonis (Fischer P. 1870). The boring activities of these organisms have disintegrated the sandy matrix of these sets. Finer-grained
matrix sediments have been transported to the interset and open sea, while cobble–pebbles have been carried landwards and
have created imbricated gravely beach deposits without matrix. Sandy beach is evolving where the conglomeratic sets away from
the shoreline (5.0–10.0 m). In this example, sets form a bar; causing fivefold division as backshore, berm, surf zone, bar
and offshore from land to sea. Poorly sorted, cobbles-pebbles cobbles and pebbles are found associated with the high-energy
environments of bars, whilst well-sorted sands are observed in low energetic environments on shore. The sets and recent shell
fragments are the main sources of coastal sediments in Viranşehir. However, the amount of shell fragments decrease towards
the active river mouth. This is due to sediment and fresh water influx from the river causing deteriorated temperature, salinity
and light penetration of the marine environment resulting in less organic diversity.
Electronic supplementary material The online version of this article (doi:) contains supplementary material, which is available to authorized users. 相似文献
995.
An inhomogeneous KdV equation including topographic forcing is derived by usingperturbation expansions and stretching transforms of time and space.The generation of forcedsolitary Rossby waves by topography in a near-resonant flow and their interactions with freesolitary waves are discussed,and some interesting results are obtained.The numerical resultsshow that the topography has obvious effect on enhancing the amplitude of disturbances,and itmay explain to some degree the formation of blocking by localized topography. 相似文献
996.
Prior to hydrologic modelling, topographic features of a surface are derived, and the surface is divided into sub‐basins. Surface delineation can be described as a procedure, which leads to the quantitative rendition of surface topography. Different approaches have been developed for surface delineation, but most of them may not be applicable to depression‐dominated surfaces. The main objective of this study is to introduce a new depression‐dominated delineation (D‐cubed) method and highlight its unique features by applying it to different topographic surfaces. The D‐cubed method accounts for the hierarchical relationships of depressions and channels by introducing the concept of channel‐based unit (CBU) and its connection with the concept of puddle‐based unit (PBU). This new delineation method implements a set of new algorithms to determine flow directions and accumulations for puddle‐related flats. The D‐cubed method creates a unique cascaded channel‐puddle drainage system based on the channel segmentation algorithm. To demonstrate the capabilities of the D‐cubed method, a small laboratory‐scale surface and 2 natural surfaces in North Dakota were delineated. The results indicated that the new method delineated different surfaces with and without the presence of depressional areas. Stepwise changes in depression storage and ponding area were observed for the 3 selected surfaces. These stepwise changes highlighted the dynamic filling, spilling, and merging processes of depressions, which need to be considered in hydrologic modelling for depression‐dominated areas. Comparisons between the D‐cubed method and other methods emphasized the potential consequences of use of artificial channels through the flats created by the depression‐filling process in the traditional approaches. In contrast, in the D‐cubed method, sub‐basins were further divided into a number of smaller CBUs and PBUs, creating a channel‐puddle drainage network. The testing of the D‐cubed method also demonstrated its applicability to a wide range of digital elevation model resolutions. Consideration of CBUs, PBUs, and their connection provides the opportunity to incorporate the D‐cubed method into different hydrologic models and improve their simulation of topography‐controlled runoff processes, especially for depression‐dominated areas. 相似文献
997.
Glacial features in the geological record provide essential clues about past behavior of climate. Of the numerous physical systems on earth, glaciers are one of most responsive to climate change, especially small glaciers, their direct marginal response taking only a few years or decades to be expressed. Accelerating recession of modern glaciers raises the issue of the climate’s impact on water runoff. Data based on topographic maps and Advanced Spaceborne Thermal Emission and Radiometer (ASTER) imagery sho... 相似文献
998.
A shallow flow generally features complex hydrodynamics induced by complicated domain topography and geometry. A numerical scheme with well-balanced flux and source term gradients is therefore essential before a shallow flow model can be applied to simulate real-world problems. The issue of source term balancing has been exhaustively investigated in grid-based numerical approaches, e.g. discontinuous Galerkin finite element methods and finite volume Godunov-type methods. In recent years, a relatively new computational method, smooth particle hydrodynamics (SPH), has started to gain popularity in solving the shallow water equations (SWEs). However, the well-balanced problem has not been fully investigated and resolved in the context of SPH. This work aims to discuss the well-balanced problem caused by a standard SPH discretization to the SWEs with slope source terms and derive a corrected SPH algorithm that is able to preserve the solution of lake at rest. In order to enhance the shock capturing capability of the resulting SPH model, the Monotone Upwind-centered Scheme for Conservation Laws (MUSCL) is also explored and applied to enable Riemann solver based artificial viscosity. The new SPH model is validated against several idealized benchmark tests and a real-world dam-break case and promising results are obtained. 相似文献
999.
James A. Henry 《自然地理学》2013,34(2):146-159
Location, timing, and intensities of urban atmospheric moisture anomalies in the relatively small city of Lawrence, Kansas are mapped, explained, and compared with previously studied cities. Forty-five urban-rural dew point distributions were obtained during mornings, afternoons, and evenings in August, September, and October. A meteorologically-equipped auto was used to traverse an 88.5-km route through the major land uses in the city and surrounding countryside. Rural dew points exceeded urban values much more frequently than the reverse. On several dates, a reversal of the urban-rural dew point relationship occurred; in the afternoon, rural dew points were greater than urban values, but at night urban values exceeded those in rural areas. Lowest values often corresponded with the most developed sections of the city, and the central business district exerted the most consistent influence on dew points. Greatest gradients developed on the periphery of the developed area. Pattern complexity was generally at a maximum in the afternoon and was least complex during morning hours. Results compare and contrast with previous urban-rural humidity studies. 相似文献
1000.