全文获取类型
收费全文 | 220篇 |
免费 | 23篇 |
国内免费 | 38篇 |
专业分类
测绘学 | 18篇 |
大气科学 | 35篇 |
地球物理 | 45篇 |
地质学 | 99篇 |
海洋学 | 29篇 |
天文学 | 17篇 |
综合类 | 24篇 |
自然地理 | 14篇 |
出版年
2024年 | 1篇 |
2023年 | 4篇 |
2022年 | 2篇 |
2021年 | 11篇 |
2020年 | 1篇 |
2019年 | 6篇 |
2018年 | 5篇 |
2017年 | 9篇 |
2016年 | 8篇 |
2015年 | 4篇 |
2014年 | 10篇 |
2013年 | 8篇 |
2012年 | 14篇 |
2011年 | 11篇 |
2010年 | 11篇 |
2009年 | 14篇 |
2008年 | 6篇 |
2007年 | 12篇 |
2006年 | 8篇 |
2005年 | 9篇 |
2004年 | 4篇 |
2003年 | 5篇 |
2002年 | 9篇 |
2001年 | 2篇 |
2000年 | 9篇 |
1999年 | 7篇 |
1998年 | 9篇 |
1997年 | 9篇 |
1996年 | 6篇 |
1995年 | 7篇 |
1994年 | 6篇 |
1993年 | 4篇 |
1992年 | 7篇 |
1991年 | 3篇 |
1990年 | 6篇 |
1989年 | 6篇 |
1988年 | 2篇 |
1987年 | 3篇 |
1986年 | 2篇 |
1985年 | 2篇 |
1984年 | 1篇 |
1983年 | 3篇 |
1982年 | 5篇 |
1981年 | 1篇 |
1980年 | 2篇 |
1979年 | 2篇 |
1978年 | 1篇 |
1977年 | 2篇 |
1975年 | 1篇 |
1974年 | 1篇 |
排序方式: 共有281条查询结果,搜索用时 15 毫秒
31.
Wan-Li Cheng Li-Wei Lai Walter Den Shu-Ying Wang Pay-Liam Lin Chueh-Ying Pai 《Meteorology and Atmospheric Physics》2012,117(3-4):153-166
This study investigated the potential factors contributing to a series of ozone (O3) episodes in the Taichung metropolis, which occurred during the first half of May 2007. Surface data of the meteorological parameters and air pollutant concentrations, supported by Taiwan Environmental Protection Administration, and vertical data monitored via tethersonde sampling were analysed. The analyses showed that local anthropogenic activities and physical factors such as the sea–air interaction were not the main factors contributing to the O3 events. Excluding these potential causes, the results suggest that, during the aforementioned period, the stronger Mainland High and Pacific Low may have been responsible for the long-range transport of large quantities of O3 from Mainland China to Taiwan. Furthermore, O3 photochemical activity also played an important role in the O3 episodes. The faster consumption of NO lead to a more rapid increase in the O3 concentration. 相似文献
32.
Continuous Measurement of Number Concentrations and
Elemental Composition of Aerosol Particles
for a Dust Storm Event in Beijing 总被引:1,自引:0,他引:1
A continuous measurement of number size distributions and chemical composition of aerosol particles was conducted in Beijing in a dust storm event during 21-26 March 2001. The number concentration of coarse particles ( 〉2μm) increased more significantly than fine particles ( 〈2μm) during the dust storm due to dust weather, while the anthropogenic aerosols collected during the non-dust-storm period tended to be associated with fine particles. Elemental compositions were analyzed by using proton-induced X-ray emission (PIXE). The results show that 20 elements in the dust storm were much higher than in the non-dust-storm period. The calculated soil dust concentration during the dust storm was, on average, 251.8μg m^-3, while it was only 52.1μg m^-3 on non-dust-storm days. The enrichment factors for Mg, A1, P, K, Ca, Ti, Mn, Fe, C1, Cu, Pb, and Zn show small variations between the dust storm and the non-dust-storm period, while those for Ca, Ni and Cr in the dust storm were much lower than those in the non-dust-storm period due to significant local emission sources. A high concentration and enrichment factor for S were observed during the dust storm, which implies that the dust particles were contaminated by aerosol particles from anthropogenic emissions during the long-range transport. A statistical analysis shows that the elemental composition of particles collected during the dust storm in Beijing were better correlated with those of desert soil colleted from desert regions in Inner Mongolia. Air mass back-trajectory analysis further confirmed that this dust storm event could be identified as streaks of dust plumes originating from Inner Mongolia. 相似文献
33.
一次全省性强雷暴天气的地闪特征 总被引:4,自引:2,他引:2
2009年6月26日浙江出现全省范围的雷暴天气,此次过程中出现的地闪频数是自2006年闪电定位系统建立以来出现最多的一次。利用闪电定位实测资料、加密雨量站雨量实况以及多普勒天气雷达产品,对这一过程的地闪特征进行了分析。结果表明:此次地闪以负地闪为主,负地闪广泛分布于25~55dBz雷电回波区域内,而正闪多出现在25~35dBz回波中;地闪多出现在回波发展和前进的一侧,且密集分布在回波的梯度最大处,强回波中心处地闪较少出现;在回波开始减弱到中心强度为35dBz左右的区域没有地闪发生。地闪频数与全省过程累积降水量有很好的相关性,地闪的出现及其频数的增加意味着影响某地的强对流风暴正在发展或正向本地移来,对于单站来说雨强峰值滞后于地闪频数峰值半个小时以上,对于全省累积降水量则提前1~2h。因此地闪资料可以作为强对流天气的短时强降水预报的预警依据。 相似文献
34.
目的:探讨容积穿梭CT灌注时间-密度曲线特征结合形态学参数对腮腺良性肿瘤鉴别诊断的价值。方法:收集我院拟诊腮腺肿瘤患者100例,术前均行容积穿梭CT灌注成像检查,术后经手术病理证实。将所得影像数据传送至工作站及pacs系统,观察分析不同病理类型腮腺肿瘤的形态学参数(位置、大小、密度、边界、颈部淋巴结、增强扫描强化幅值)及时间-密度曲线(TDC)类型,计数资料比较采用χ2检验,计量资料符合正态分布采用两独立样本t检验,不符合正态分布的采用秩和检验,检验水准α=0.05。结果:腮腺良性肿瘤(多行性腺瘤、腺淋巴瘤、基底细胞瘤及肌上皮瘤)间的形态学参数无统计学差异;时间-密度曲线类型差异有统计学差异。结论:CT灌注时间-密度曲线特征结合形态学参数对腮腺良性肿瘤的鉴别诊断有重要价值,为患者术式的选择有重要指导意义。 相似文献
35.
探讨了位置数据异常分析的一种新思路,给出了面向异常的时空表达模型,建立了基于区域位置点统计的异常检测和分析框架,探寻异常在事件影响下的时空发展趋势和分布特征。通过纽约两个月的出租车出行数据的实验分析验证了框架的有效性,并发现一些有趣的规律,为公共安全、交通管控应急、城市功能区分析等提供指导信息。 相似文献
36.
E. Den Tex 《Engineering Geology》1974,8(4):403-405
37.
Fred C. Bosveld A.A. M. Holtslag B.J. J.M. Van Den Hurk 《Boundary-Layer Meteorology》1999,93(2):171-195
Infrared radiative surface temperatures as observed over a dense Douglas fir forest during stable atmospheric conditions are analyzed. It is shown that the concept of a single surface temperature to describe both the thermal coupling and the radiative coupling between atmosphere and forest fails when longwave cooling is large and wind speeds are low. In such cases a decoupling of the radiative surface temperature from the air temperature aloft is observed. Conditions for decoupling are formulated in terms of an appropriate Richardson number. It is shown that a convective surface temperature comes into play that is coupled to the forest interior air temperature. Observed radiative surface temperature is then composed of this convective surface temperature and the aerodynamic surface temperature. Forest interior air temperature during nighttime is, in general, lower than air temperature above the canopy. A simple two-layer canopy model is used to explain this phenomenon in terms of the distribution of atmospheric sensible heat flux and storage heat flux over the two canopy layers. 相似文献
38.
Rupture process of the 2015 Pishan earthquake from joint inversion of InSAR,teleseismic data and GPS
An earthquake of Mw6.4 occurred in Pishan County in Xinjiang Province, northwestern Tibetan Plateau, on July 3,2015. The epicenter was located on an active blind thrust system located at the northern margin of the Western Kunlun Mountain Orogenic Belt southwest of the Tarim Basin. We constructed a shovel-shaped fault model based on the layered-crust model with reference to the seismic reflection profile, and obtained the rupture process of the earthquake from the joint inversion of Interferometric Synthetic Aperture Radar(InSAR) measurements, far-field waveform data, and Global Positioning System(GPS) data. The results show that the seismic fault dips southward with a strike of 109°, and the rupture direction was essentially northward. The fault plane rupture distribution is concentrated, with a maximum recorded slip of 73 cm. The main features of the fault are as follows: low inclination angle(25°–10°), thrust slip at a depth of 9–13 km, rupture propagation time of about 12 s, no significant slip in soft or hard sedimentary layers at 0–4 km depth and propagation from the initial rupture point to the surrounding area with no obvious directionality. The InSAR time-series analysis method is used to determine the deformation rate in the source region within 2 years after the earthquake, and the maximum value is ~17 mm yr-1 in the radar line-of-sight direction. Obvious post-earthquake deformation is evident in the hanging wall, with a similar trend to the coseismic displacement field. These results suggest that the Pishan earthquake has not completely released the accumulated energy of the region, given that the multilayer fold structure above the blind fault is still in a process of slow uplift since the earthquake. Post-earthquake adjustment models and aftershock risk analysis require further study using more independent data. 相似文献
39.
40.