全文获取类型
收费全文 | 7290篇 |
免费 | 1032篇 |
国内免费 | 1690篇 |
专业分类
测绘学 | 1161篇 |
大气科学 | 1530篇 |
地球物理 | 1464篇 |
地质学 | 3025篇 |
海洋学 | 970篇 |
天文学 | 393篇 |
综合类 | 566篇 |
自然地理 | 903篇 |
出版年
2024年 | 24篇 |
2023年 | 68篇 |
2022年 | 158篇 |
2021年 | 224篇 |
2020年 | 201篇 |
2019年 | 293篇 |
2018年 | 206篇 |
2017年 | 303篇 |
2016年 | 352篇 |
2015年 | 387篇 |
2014年 | 403篇 |
2013年 | 498篇 |
2012年 | 419篇 |
2011年 | 427篇 |
2010年 | 369篇 |
2009年 | 470篇 |
2008年 | 578篇 |
2007年 | 585篇 |
2006年 | 565篇 |
2005年 | 479篇 |
2004年 | 442篇 |
2003年 | 383篇 |
2002年 | 337篇 |
2001年 | 254篇 |
2000年 | 294篇 |
1999年 | 228篇 |
1998年 | 195篇 |
1997年 | 176篇 |
1996年 | 111篇 |
1995年 | 127篇 |
1994年 | 111篇 |
1993年 | 79篇 |
1992年 | 62篇 |
1991年 | 39篇 |
1990年 | 38篇 |
1989年 | 22篇 |
1988年 | 30篇 |
1987年 | 13篇 |
1986年 | 16篇 |
1985年 | 17篇 |
1984年 | 6篇 |
1983年 | 4篇 |
1981年 | 6篇 |
1980年 | 8篇 |
1979年 | 1篇 |
1976年 | 1篇 |
1974年 | 1篇 |
1954年 | 2篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
981.
利用SRTM以及DTM2006.0全球地形模型构建剩余地形模型(RTM)数据,并将其转换为RTM高程异常。通过GPS/水准点的优化选择法,选择少量GPS/水准点的实测高程异常,扣除EGM2008模型以及SRTM与DTM2006.0模型求得的剩余模型高程异常,对残余高程异常进行拟合,从而进一步提高GPS高程转换的精度。最... 相似文献
982.
983.
984.
985.
Laboratory experiments have been carried out for the flow along isobaths of simulated shelf-continental slope geometry. Cases of both homogeneous and linearly stratified fluids are considered and the background flows are sufficiently strong to have the flow near the bottom boundary range from transitional to fully turbulent. The background motions are impulsively started and flows with a coast on the right (spin-down) and on the left (spin-up) are considered. The homogeneous spin-down and spin-up processes are smooth in the sense that no vortical structures were found to be of the order of the slope width or larger. Flows reach equilibrium more quickly for spin-down cases, and this is attributed to secondary flows forced by the basin geometry. All of the stratified experiments exhibited large-scale instabilities as evidenced by the generation of slope and basin scale eddy structures and a much slower decay than their homogeneous counterparts. 相似文献
986.
The Impact of Mid- and High-Latitude Rossby Wave Activities
on the Medium-Range Evolution of the EAP Pattern During
the Pre-Rainy Period of South China
下载免费PDF全文
![点击此处可从《Acta Meteorologica Sinica》网站下载免费的PDF全文](/ch/ext_images/free.gif)
Based on the NCEP DOE AMIP II daily reanalysis data (1979{2005), the evolution of the East Asia/Pacific(EAP) teleconnection pattern during the pre-rainy period of South China is studied on the medium-range time scale. It is found that positive and negative EAP patterns share a similar generation process. In the middle and upper troposphere, Rossby wave packets emanating from the northeast Atlantic or Europe propagate toward East Asia along the Eurasian continent waveguide and finally give rise to the three anomaly centers of the EAP pattern over East Asia. Among the three anomaly centers, the western Pacific subtropical center appears the latest. Rossby wave packets propagate from the high latitude anomaly center toward the mid-latitude and the subtropical ones. The enhancement and maintenance of the subtropical anomaly center is closely associated with the subtropical jet waveguide and the incoming Rossby wave packets from the upstream. In the lower troposphere, Rossby wave packets emanate from the subtropical Asia toward East Asia.
Positive and negative EAP patterns could not be regarded as "mirrors" to each other with simply re-
versed phase. For the positive pattern, the positive height anomaly center around the Scandinavia Peninsula keeps its strength and position during the mature period, and the Rossby wave packets thus propagate persistently toward East Asia, facilitating a longer mature time of the positive pattern. As for the formation of the negative EAP pattern, however, the incoming Rossby wave energy from the upstream contributes to both the enhancement and southeastward movement of the negative anomaly belt from the Yenisei River to the Bering Strait and the positive anomaly center around Mongolia. At the peak time, the two anomlous circulations are evolved into the Northeast Asia and the mid-latitude anomaly centers of the negative pattern, respectively. The energy dispersion of Rossby wave packets is relatively fast due to the predominant zonal circulation in the extratropics, causing a shorter mature period of the negative pattern.
During the pre-rainy period of South China, the prevalence of the EAP pattern signiˉcantly affects the rainfall over the region south of the Yangtze River. The positive (negative) EAP pattern tends to causepositive (negative) precipitation anomalies in that region. This is di?erent from the earlier research findingsbased on monthly mean data. 相似文献
987.
K. P. Sooraj Daehyun Kim Jong-Seong Kug Sang-Wook Yeh Fei-Fei Jin In-Sik Kang 《Climate Dynamics》2009,33(4):495-507
Recently, there is increasing evidence on the interaction of atmospheric high-frequency (HF) variability with climatic low-frequency
(LF) variability. In this study, we examine this relationship of HF variability with large scale circulation using idealized
experiments with an aqua-planet Atmospheric GCM (with zonally uniform SST), run in different zonal momentum forcing scenarios.
The effect of large scale circulation changes to the HF variability is demonstrated here. The HF atmospheric variability is
enhanced over the westerly forced region, through easterly vertical shear. Our study also manifests that apart from the vertical
wind shear, strong low-level convergence and horizontal zonal wind shear are also important for enhancing the HF variance.
This is clearly seen in the eastern part of the forcing, where the HF activity shows relatively maximum increase, in spite
of similar vertical shear over the forced regions. The possible implications for multi-scale interaction (e.g. MJO–ENSO interaction)
are also discussed. 相似文献
988.
989.
两种初始场MM5模式预报效果对比评估 总被引:1,自引:1,他引:0
为了解本地MM5模式的预报性能,根据其预报结果,检验了基于NCEP和T213两种初始场MM5模式在河北以及京津地区2007年8月至2008年1月的降水、日极值温度和相对湿度的预报效果。结果表明,MM5晴雨(雪)预报的准确率较高,具有较好的参考价值,而对于降水的分级预报,随着预报时效的延长和降水强度的增加,其可用性逐渐降低,但整体来看基于NCEP初始场的预报均比T213初始场预报效果明显;在日极值温度预报中,最低温度效果优于最高温度,T213初始场的预报对日最高温度预报的准确率较高,NCEP初始场的预报则在日最低温度预报中略胜一筹;对08:00相对湿度的预报,两者的预报效果基本相同,绝对误差都在15%左右。 相似文献
990.