全文获取类型
收费全文 | 4728篇 |
免费 | 1214篇 |
国内免费 | 2370篇 |
专业分类
测绘学 | 121篇 |
大气科学 | 1022篇 |
地球物理 | 709篇 |
地质学 | 5369篇 |
海洋学 | 360篇 |
天文学 | 39篇 |
综合类 | 258篇 |
自然地理 | 434篇 |
出版年
2024年 | 43篇 |
2023年 | 139篇 |
2022年 | 235篇 |
2021年 | 242篇 |
2020年 | 308篇 |
2019年 | 328篇 |
2018年 | 274篇 |
2017年 | 327篇 |
2016年 | 363篇 |
2015年 | 396篇 |
2014年 | 480篇 |
2013年 | 390篇 |
2012年 | 449篇 |
2011年 | 396篇 |
2010年 | 343篇 |
2009年 | 312篇 |
2008年 | 323篇 |
2007年 | 347篇 |
2006年 | 319篇 |
2005年 | 264篇 |
2004年 | 285篇 |
2003年 | 218篇 |
2002年 | 191篇 |
2001年 | 170篇 |
2000年 | 195篇 |
1999年 | 214篇 |
1998年 | 157篇 |
1997年 | 128篇 |
1996年 | 112篇 |
1995年 | 89篇 |
1994年 | 66篇 |
1993年 | 64篇 |
1992年 | 44篇 |
1991年 | 22篇 |
1990年 | 21篇 |
1989年 | 15篇 |
1988年 | 10篇 |
1987年 | 10篇 |
1986年 | 6篇 |
1985年 | 3篇 |
1984年 | 4篇 |
1983年 | 3篇 |
1980年 | 2篇 |
1978年 | 2篇 |
1954年 | 3篇 |
排序方式: 共有8312条查询结果,搜索用时 93 毫秒
911.
BAO Qing 《大气和海洋科学快报》2012,5(1):43-48
Responses of the Asian Summer Monsoon(ASM) in future projections have been studied based on two core future projections of phase five of the Coupled Model Intercomparison Project(CMIP5) coordinated experiments with the IAP-coupled model FGOALS_s2(the Flexible Global Ocean-Atmosphere-Land System Model).The projected changes of the ASM in climatological mean and interannual variability were respectively reported.Both the South Asian Summer Monsoon(SASM) and the East Asian Summer Monsoon(EASM) were intensified in their climatology,featuring increased monsoon precipitation and an enhanced monsoon lower-level westerly jet flow.Accordingly,the amplitude of the annual cycle of rainfall over East Asia(EA) is enhanced,thereby indicating a more abrupt monsoon onset.After the EA monsoon onset,the EASM marched farther northward in the future scenarios than in the historical runs.In the interannual variability,the leading pattern of the EASM,defined by the first multi-variable EOF analysis over EA,explains more of the total variances in the warmest future scenario,specifically,Representative Concentration Pathway(RCP8.5).Also,the correlation coefficients analysis suggests that the relationship between the EASM interannual variations and ENSO was significantly strengthened in the future projections,which may indicate improved predictability of the EASM interannual variations. 相似文献
912.
卫星搭载的有效载荷在进行在轨对地观测过程中,受仪器本身特性和地球固有特性因素的影响,在图像上会产生多种观测失准和干扰现象。如图像旋转现象,蝴蝶结效应以及探元非均匀性条纹现象等。针对这类可以预见到的冗余和条纹,对仪器设计优化以及借助卫星星历轨道等辅助数据和成熟的图像处理算法可以对其实现有效地恢复。仪器在轨运行期间新引入的周期性或非周期性干扰,则需综合运用多种数据来源和关于干扰产生原理的先验知识,并结合图像处理手段实现图像恢复,同时保存原有辐射信息的真实性,为定量研究提供高质量可靠的数据准备。本研究针对某卫星中波红外图像干扰条纹,利用星上定标数据,并通过条纹现象分析和产生机理分析,探索了一种新的基于空域信号补偿原理的图像干扰条纹处理算法,通过大量图像数据处理实践证明,该算法对图像质量改善明显,且在动态范围和辐射信息保存方面优于传统频域滤波算法。 相似文献
913.
914.
915.
This study examines cloud radiative forcing (CRF) in the Asian monsoon region
(0o--50oN,60o--150oE) simulated by Intergovernmental Panel on
Climate Change (IPCC) Fourth Assessment Report (AR4) AMIP models. During boreal winter,
no model realistically reproduces the larger long-wave cloud radiative forcing (LWCF) over
the Tibet Plateau (TP) and only a couple of models reasonably capture the larger short-wave
CRF (SWCF) to the east of the TP. During boreal summer, there are larger biases for central
location and intensity of simulated CRF in active convective regions. The CRF biases are closely
related to the rainfall biases in the models. Quantitative analysis further indicates that the
correlation between simulated CRF and observations are not high, and that the biases and diversity
in SWCF are larger than that in LWCF. The annual cycle of simulated CRF over East Asia (0o--50oN,
100o--145oE) is also examined. Though many models capture the basic annual cycle in
tropics, strong LWCF and SWCF to the east of the TP beginning in early spring are underestimated
by most models. As a whole, GFDL-CM2.1, MPI-ECHAM5, UKMO-HadGAM1, and MIROC3.2 (medres) perform
well for CRF simulation in the Asian monsoon region, and the multi-model ensemble (MME) has improved
results over the individual simulations. It is suggested that strengthening the physical
parameterizations involved over the TP, and improving cumulus convection processes and model
experiment design are crucial to CRF simulation in the Asian monsoon region. 相似文献
916.
The observed South Asia High (SAH) center is characterized by two distinctive equilibrium modes
during boreal midsummer, namely the center of SAH is located between 82.5o--92.5oE for the
Tibetan Plateau mode and between 55o--65oE for the Iranian Plateau mode, respectively. The
present study describes the ability of 15 coupled general circulation models (CGCM) used in the Intergovernmental
Panel on Climate Changes (IPCC) 4th Assessment Report to reproduce the observed bimodality of the SAH. These models
reveal a wide range of skill in simulating this bimodality. Nearly half of the models reproduced the bimodality,
while the other half of the models did not simulate well these two modes whereas usually preferring one
mode. The models that reproduced the bimodality of the SAH present similar horizontal and vertical
circulations as those features from the NCEP reanalysis data. The results from these models identify
the warm characteristics of the SAH and indicate that these two modes have different dynamic and
thermodynamic properties.
Different characteristics of the simulated sensible heat and latent heat related to precipitation
partly contribute to the difference in the simulations of the SAH bimodality. The majority of these
models that prefer to simulate the Tibetan Plateau mode produce a small sensible heat flux difference
between the Iranian Plateau and the Tibetan Plateau, and also generally simulate a very strong false
precipitation center over the east of the Tibetan Plateau, which indicates strong latent release and
thereby contributes to the preference of the SAH center on the Tibetan Plateau. Whereas, the models
that reproduce the bimodality of the SAH tend to simulate large precipitation over the southern Himalayas
and no obviously false precipitation is produced over the east of the Tibetan Plateau. In addition,
the models resolution may also have important impacts on the simulations of precipitation. 相似文献
917.
918.
将有限区域流函数、速度势求解中常用的两种张驰法(即理查逊法和加速利布曼法)与调和—余弦谱展开法(H-C法)进行了比较,理论研究表明:H-C法单独考虑边界影响分量,物理意义明确,且不会丢失边界上的天气系统;从计算上看,H-C法重建的风场能精确还原原始风场,且计算效率明显高于两种张驰法,即收敛更快。通过在台风Bilis(0604)暴雨增幅过程诊断中的应用发现,常用的两种张驰迭代方法在求解有限区域流函数和速度势的问题上效果都不是很好,即:用理查逊法和加速利布曼法计算的流函数和速度势重建的风场与原始风场差别较大,不能准确还原原始风场;用H-C法不仅计算效率高,还原的风场与原始风场差异极小,且不受南边界较强的西南季风涌影响,在暴雨增幅前期能较好地反映与暴雨增幅相关的强辐合信号。因此,可用H-C法计算得到的无辐散风和无旋风对有限区域的天气系统进行更深入的动力结构分析。 相似文献
919.
Simulated Change in the Interannual Variability of South Asian Summer Monsoon in the 21st Century 总被引:1,自引:0,他引:1
This study investigates the projected changes in interannual variability of South Asian summer monsoon and changes of ENSO-monsoon relationships in the 21st century under the Intergovernmental Panel on Climate Change (IPCC) scenarios A1B and A2, respectively, by analyzing the simulated results of twelve Coupled Model Intercomparison Project Phase 3 (CMIP3) coupled models. The dynamical monsoon index (DMI) was adopted to describe the interannual variability of South Asian summer monsoon, and the standard dev... 相似文献
920.
Interdecadal Variability of East Asian Summer Monsoon Precipitation over 220 Years (1777-1997) 总被引:1,自引:1,他引:0
In this study, long-term (1777–1997) precipitation data for Seoul, Korea, wetness indices from eastern China, and modern observations are used to identify the interdecadal variability in East Asian summer monsoon precipitation over the last 220 years. In the East Asian monsoon region, two long-term timescales of dry–wet transitions for the interdecadal variability and quasi-40-and quasi-60-year timescales are dominant in the 220-year precipitation data of Seoul, as well as in the wetness indices over China.... 相似文献