全文获取类型
收费全文 | 762篇 |
免费 | 192篇 |
国内免费 | 161篇 |
专业分类
测绘学 | 40篇 |
大气科学 | 277篇 |
地球物理 | 295篇 |
地质学 | 263篇 |
海洋学 | 107篇 |
天文学 | 41篇 |
综合类 | 27篇 |
自然地理 | 65篇 |
出版年
2024年 | 1篇 |
2023年 | 6篇 |
2022年 | 15篇 |
2021年 | 13篇 |
2020年 | 13篇 |
2019年 | 26篇 |
2018年 | 22篇 |
2017年 | 26篇 |
2016年 | 27篇 |
2015年 | 29篇 |
2014年 | 47篇 |
2013年 | 49篇 |
2012年 | 45篇 |
2011年 | 53篇 |
2010年 | 41篇 |
2009年 | 58篇 |
2008年 | 69篇 |
2007年 | 72篇 |
2006年 | 61篇 |
2005年 | 50篇 |
2004年 | 32篇 |
2003年 | 24篇 |
2002年 | 40篇 |
2001年 | 38篇 |
2000年 | 18篇 |
1999年 | 35篇 |
1998年 | 26篇 |
1997年 | 40篇 |
1996年 | 24篇 |
1995年 | 19篇 |
1994年 | 14篇 |
1993年 | 23篇 |
1992年 | 12篇 |
1991年 | 5篇 |
1990年 | 8篇 |
1989年 | 6篇 |
1988年 | 7篇 |
1987年 | 7篇 |
1986年 | 5篇 |
1985年 | 1篇 |
1984年 | 2篇 |
1982年 | 1篇 |
1980年 | 4篇 |
1978年 | 1篇 |
排序方式: 共有1115条查询结果,搜索用时 46 毫秒
91.
92.
中国传统民居建筑文化的自然地理背景 总被引:17,自引:0,他引:17
讨论了气候、地貌与水文、地质与植被等自然地理要素对中国传统民居建筑的格局、型式、风格、特色等方面的影响。在此基础上分析了以功利观、审美观和生态观为内涵的中国传统民居建筑文化的自然观。 相似文献
93.
作用于南海北部地壳岩体的外场力 总被引:1,自引:1,他引:0
用光弹等色线与地震震中密集程度对照法,得到本研究区等效外场力的主要特点为:(1)非匀布荷载;(2)方向大致为:东—中部在N13~79°之间;西北部为SN向;西部在N51~78°之间;西南部在N25~69°E之间。 相似文献
94.
CAI Qiangguo 《国际泥沙研究》1998,(2)
PHYSICALPROCESSBASEDSOILEROSIONMODELINASMALLWATERSHEDINTHEHILLYLOESSREGION1CAIQiangguo2ABSTRACTAphysicalprocesbasedperstorm... 相似文献
95.
An inverse model is applied for the analysis of hydrographic and current meter data collected on the repeat WOCE section SR4 in the Weddell Sea in 1989–1992. The section crosses the Weddell Sea cyclonic gyre from Kapp Norvegia to the northern end of the Antarctic Peninsula. The concepts of geostrophy, conservation of planetary vorticity and hydrostatics are combined with advective balances of active and passive properties to provide a dynamically consistent circulation pattern. Our variational assimilation scheme allows the calculation of three-dimensional velocities in the section plane. Current speeds are small except along the coasts where they reach up to 12 cm/s. We diagnose a gyre transport of 34 Sverdrup which is associated with a poleward heat transport of 28 × 1012 W corresponding to an average heat flux of 15 Wm–2 in the Weddell Sea south of the transect. This exceeds the estimated local flux on the transect of 2 Wm–2. As the transect is located mostly in the open ocean, we conclude that the shelf areas contribute significantly to the ocean-atmosphere exchange and are consequently key areas for the contribution of the Weddell Sea to global ocean ventilation. Conversion of water masses occuring south of the section transform 6.6 ± 1.1 Sv of the inflowing warm deep water into approximately equal amounts of Weddell Sea deep water and Weddell Sea bottom water. The volume transport of surface water equals in the in-and outflow. This means that almost all newly formed surface water is involved in the deep and bottom water formation. Comparison with the results obtained by pure velocity interpolation combined with a hydrographic data subset indicates major differences in the derived salt transports and the water mass conversion of the surface water. The differences can be explained by deviations in the structure of the upper ocean currents to which shelf areas contribute significantly. Additionally a rigorous variance analysis is performed. When only hydrographic data are used for the inversion both the gyre transport and the poleward heat transport are substantially lower. They amount to less than 40% of our best estimate while the standard deviations of both quantities are 6.5 Sv and 37 × 1012 W, respectively. With the help of long-term current meter measurements these errors can be reduced to 2 Sv and 8 × 1012 W. Our result underlines the importance of velocity data or equivalent information that helps to estimate the absolute velocities. 相似文献
96.
油气在盆地中产生和运移过程中,水动力因素起着重要的控制作用[1],如何确定这一作用的实际影响,是一个值得研究的问题。通过数学推导,得出储层中的稳态油层和非稳态油层两种情况下的水动力理论模型,并且对水动力圈闭、深度-压力系统和流体势等作出理论模拟,将其用于油气勘探中,结果与实际情况较相符。 相似文献
97.
K. S. Richards 《地球表面变化过程与地形》1978,3(4):345-354
The nature of the flow in most natural streams is gradually varied rather than uniform. This is particularly true of streams with coarse gravel bed material organized into relatively stable riffle and pool features. In spite of this, there are few applications of the gradually varied flow models (e.g. the Bernoulli equation) to such streams. This paper presents some initial results of a simulation of flow patterns in two riffle-pool reaches, using an open channel flow profile computation method based on an equation defining an energy balance between successive cross-sections separated by an incremental distance. 相似文献
98.
C. R. Haines 《Pure and Applied Geophysics》1980,119(1):46-50
A closed form solution is given for the problem of simple harmonic plane waves incident obliquely on a semi-infinite barrier. The amplitude of the Kelvin wave component is considered and it is found that increased amplitudes of the Kelvin waves can be expected for certain wave numbers, depending upon the angle of incidence. 相似文献
99.
The Institute of Atmospheric Physics Land Surface Model (IAP94) has been incorporated into the IAP two-level atmospheric general circulation model (IAP GCM). Global and regional climatology averaged over the last 25 years of 100 year integrations from the IAP GCM with and without IAP94 (“bucket” scheme) is compared. The simulated results are also compared with the reanalysis data. Major findings are:(1) The IAP GCM simulation without IAP94 has extensive regions of warmer than observed surface air tempera?tures, while the simulation with IAP94 very much improves the surface air temperature.(2) The IAP GCM simulation with IAP94 gives improvement of the simulated precipitation pattern and intensity, especially the precipitation of East Asian summer monsoon and its intraseasonal migration of the rainbelts.(3) In five selected typical regions, for most of the surface variables such as surface air temperature, precipitation, precipitation minus evaporation, net radiation, latent heat flux and sensible heat flux, the IAP GCM with IAP94 pro?vides better simulations. 相似文献
100.
Combining the Penn State/NCAR mesoscale (MM4) model, the dust transport model and an atmospheric radiative transfer model,
a super duststorm process occurred in the Gansu province on 5 May 1993 has been simulated. Based on the observations of duststorms
occurred in the northern China and the field measurements of dust particles' physical and optical properties, model simulating
dust plume transport processes and dust particle radiative forcing have been devloped. The models are described and verified
with real cases of dustorms. 相似文献