全文获取类型
收费全文 | 414篇 |
免费 | 59篇 |
国内免费 | 62篇 |
专业分类
测绘学 | 27篇 |
大气科学 | 77篇 |
地球物理 | 96篇 |
地质学 | 194篇 |
海洋学 | 51篇 |
天文学 | 48篇 |
综合类 | 12篇 |
自然地理 | 30篇 |
出版年
2023年 | 3篇 |
2022年 | 18篇 |
2021年 | 15篇 |
2020年 | 23篇 |
2019年 | 14篇 |
2018年 | 25篇 |
2017年 | 13篇 |
2016年 | 17篇 |
2015年 | 15篇 |
2014年 | 22篇 |
2013年 | 26篇 |
2012年 | 12篇 |
2011年 | 28篇 |
2010年 | 16篇 |
2009年 | 17篇 |
2008年 | 21篇 |
2007年 | 20篇 |
2006年 | 14篇 |
2005年 | 12篇 |
2004年 | 10篇 |
2003年 | 13篇 |
2002年 | 9篇 |
2001年 | 15篇 |
2000年 | 9篇 |
1999年 | 14篇 |
1998年 | 11篇 |
1997年 | 8篇 |
1996年 | 4篇 |
1995年 | 6篇 |
1994年 | 6篇 |
1993年 | 3篇 |
1992年 | 8篇 |
1991年 | 4篇 |
1990年 | 7篇 |
1989年 | 3篇 |
1987年 | 3篇 |
1986年 | 5篇 |
1984年 | 3篇 |
1983年 | 9篇 |
1982年 | 3篇 |
1981年 | 4篇 |
1977年 | 5篇 |
1973年 | 3篇 |
1971年 | 3篇 |
1966年 | 2篇 |
1962年 | 2篇 |
1923年 | 2篇 |
1919年 | 2篇 |
1917年 | 2篇 |
1915年 | 2篇 |
排序方式: 共有535条查询结果,搜索用时 250 毫秒
531.
Wei-Kuo Tao Jainn Jong Shi Shuyi S. Chen Stephen Lang Pay-Liam Lin Song-You Hong Christa Peters-Lidard Arthur Hou 《Asia-Pacific Journal of Atmospheric Sciences》2011,47(1):1-16
During the past decade, both research and operational numerical weather prediction models [e.g. the Weather Research and Forecasting Model (WRF)] have started using more complex microphysical schemes originally developed for high-resolution cloud resolving models (CRMs) with 1–2 km or less horizontal resolutions. WRF is a next-generation meso-scale forecast model and assimilation system. It incorporates a modern software framework, advanced dynamics, numerics and data assimilation techniques, a multiple moveable nesting capability, and improved physical packages. WRF can be used for a wide range of applications, from idealized research to operational forecasting, with an emphasis on horizontal grid sizes in the range of 1–10 km. The current WRF includes several different microphysics options. At NASA Goddard, four different cloud microphysics options have been implemented into WRF. The performance of these schemes is compared to those of the other microphysics schemes available in WRF for an Atlantic hurricane case (Katrina). In addition, a brief review of previous modeling studies on the impact of microphysics schemes and processes on the intensity and track of hurricanes is presented and compared against the current Katrina study. In general, all of the studies show that microphysics schemes do not have a major impact on track forecasts but do have more of an effect on the simulated intensity. Also, nearly all of the previous studies found that simulated hurricanes had the strongest deepening or intensification when using only warm rain physics. This is because all of the simulated precipitating hydrometeors are large raindrops that quickly fall out near the eye-wall region, which would hydrostatically produce the lowest pressure. In addition, these studies suggested that intensities become unrealistically strong when evaporative cooling from cloud droplets and melting from ice particles are removed as this results in much weaker downdrafts in the simulated storms. However, there are many differences between the different modeling studies, which are identified and discussed. 相似文献
532.
改造现有LIS支持时空数据管理和土地变更的实现 总被引:1,自引:0,他引:1
尝试为现有的GIS和LIS的数据管理系统增加时空数据管理功能,并扩展现有的数据管理功能,以便最大可能地应用数据库中的数据,最后以一个具体的LIS为例,描述如何对其改造以实现对时空数据的管理并完成土地变更的过程。 相似文献
533.
534.
Xenolith evidence for lithospheric melting above anomalously hot mantle under the northern Canadian Cordillera 总被引:2,自引:0,他引:2
Lang Shi Don Francis John Ludden Andrew Frederiksen Michael Bostock 《Contributions to Mineralogy and Petrology》1998,131(1):39-53
A comparison of mantle xenolith suites along the northern Canadian Cordillera reveals that the xenoliths from three suites
exhibit bimodal populations whereas the xenoliths from the other four suites display unimodal populations. The bimodal suites
contain both fertile lherzolite and refractory harzburgite, while the unimodal suites are dominated by fertile lherzolite
xenoliths. The location of the three bimodal xenolith suites correlates with a newly discovered P-wave slowness anomaly in
the upper mantle that is 200 km in width and extends to depths of 400–500 km (Frederiksen AW, Bostock MG, Van Decar JC, Cassidy
J, submitted to Tectonophysics). This correlation suggests that the bimodal xenolith suites may either contain fragments of
the anomalously hot asthenospheric mantle or that the lithospheric upper mantle has been affected by the anomalously hot mantle.
The lherzolite xenoliths in the bimodal suites display similar major element compositions and trace element patterns to the
lherzolite xenoliths in the unimodal suites, suggesting that the lherzolites represent the regional lithospheric upper mantle.
In contrast, the harzburgite xenoliths are highly depleted in terms of major element composition, but their clinopyroxenes
[Cpx] have much higher incompatible trace element contents than those in the lherzolite xenoliths. The major element and mildly
incompatible trace element systematics of the harzburgite and lherzolite xenoliths indicate that they could be related by
a partial melting process. The lack of textural and geochemical evidence for the former existence of garnet argues against
the harzburgite xenoliths representing actual fragments of the deeper anomalous asthenospheric mantle. Furthermore, the calculated
P-wave velocity difference between harzburgite and lherzolite end-members is only 0.8%, with the harzburgites having higher
P-wave velocities. Therefore the 3% P-wave velocity difference detected teleseismically cannot be produced by the compositional
difference between the lherzolite and harzburgite xenoliths. If temperature is responsible for the observed 3% P-wave velocity
perturbation, the anomalous mantle is likely to be at least 200 °C higher than the surrounding mantle. Taken together these
data indicate that the refractory harzburgite xenoliths represent the residue of 20–25% partial melting of a lherzolite lithospheric
mantle. The incompatible trace element enrichment of the harzburgites suggests that this melting was accompanied by the ingress
of fluids. The association of the bimodal xenolith suites with the mantle anomaly detected teleseismically suggests that anomalously
hot asthenospheric mantle provided both the heat and volatiles responsible for the localized melting and enrichment of the
lithospheric mantle.
Received: 16 May 1997 / Accepted: 25 October 1997 相似文献
535.
苏北黄泛平原地势平坦,浅部地层结构松散,可储水“海绵体”特征明显。为评价该区域“海绵体”雨水渗储潜力,以南部的江苏宿迁市区为例,在系统分析天然“海绵体”渗储能力主要影响因素的基础上,构建了天然“海绵体”雨水渗储潜力两级评价指标体系,借助层次分析法计算各指标权重,运用MapGIS进行综合评价。结果表明,废黄河漫滩区天然“海绵体”雨水渗储潜力较好,漫滩区以外区域渗储潜力一般或较差。 相似文献