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961.
云闪放电过程中雨滴增长的数值试验研究 总被引:1,自引:1,他引:0
利用二维数值模式,对雨滴在云闪放电条件下的增长进行了试验研究。分别讨论了在不同的电场、荷电量和电场角度时雨滴的增长演变及其运动状况。结果表明:二维模式中闪电放电对雨滴增长的影响与一维有明显不同。电场和荷电量作单因子变化时,雨滴在二维中随参量取值的增加变化较大。两者同时变化时,其乘积愈大雨滴增长幅度愈大。雨滴对电场角度绝对值变化的反应较为缓慢。其运动轨迹在不同的条件下均为准周期的。 相似文献
962.
以国家气象中心T42产品资料作为环境的初始场,采用P-σ混合坐标的有限区域细网格模式,对9406号台风暴雨过程进行24、48小时数值预报模拟试验并取得较好效果。 相似文献
963.
数字地球对二十一世纪人类星球的理解 总被引:5,自引:1,他引:4
戈尔 《地球信息科学学报》1998,(2):8-11
一场新的技术革命正在使我们获取、存储、处理和显示信息的方法发生天翻地覆的变化,它使得我们对有关我们所处的星球以及周围环境、文化现象等史无前例的海量数据的处理成为可能,而它们中的大部分信息是有关地球的--即与地表位置有关的信息。 相似文献
964.
SUN Weidong PENG Zicheng CHEN Daogong ZHI Xiachen WANG Zhaorong GE NingjieDepartment of Earth & Space Sciences University of Science & Technology of Chin and Advanced Centre for Earth Sciences & Astronomy The Third World Academyof Sciences Hefei Anhui Province Zhu Xiling 《《地质学报》英文版》1998,72(2):180-190
This paper presents a study of the major and trace element compositions of fresh mantle-derived spinel lherzolite and harzburgite inclusions from Cenozoic alkaline basalt in Mount Lianshan and Mount Panshi, Liuhe County, Jiangsu Province. An estimation is made of the contents of the major elements and some of the trace elements in the primitive mantle source region of the area, from which the authors have obtained MgO/Al2O3= 7.86. The contents of MgO and Al2O3 are also obtained as 37.58% and 4.78% respectively based on the correlation of MgO-Al2O3. Then, the contents of various elements in the primitive mantle are calculated using their regression equations with MgO, and the compositor) of the primitive mantle, a basic issue in geochemistry study, is discussed on that basis. 相似文献
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966.
The seasonal movement and jumping of subtropical high ridge line were simulated in the previous paper by using the two-dimensional zonal average model to consider the solar radiation heating. In this paper, the simulation is made by means of the same model considering water vapor condensation heating released from the rainfall belt north of subtropical high in addition to the solar radiation heating.The basic characteristics such as the northward seasonal jumping can still be simulated, and the condensation heating in the model can make the subtropical high ridge line move to the position a little further south than that without the condensation heating. Therefore, it may be realized that the basic characteristics of seasonal movement of subtropical high depend mainly on the solar radiation heating, but the meridional departure of ridge line from its normal latitude position is due to the feedback of drought-waterlogging in the precipitation area to the north of subtropical high. 相似文献
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This paper presents new high-resolution proxies and paleoclimatic reconstructions for studying climate changes in China for the past 2000 years. Multi-proxy synthesized reconstructions show that temperature variation in China has exhibited significant 50–70-yr, 100–120-yr, and 200–250-yr cycles. Results also show that the amplitudes of decadal and centennial temperature variation were 1.3℃ and 0.7℃, respectively, with the latter significantly correlated with long-term changes in solar radiation, especially cold periods, which correspond approximately to sunspot minima. The most rapid warming in China occurred over AD 1870–2000, at a rate of 0.56°± 0.42℃(100 yr)~(-1); however, temperatures recorded in the 20 th century may not be unprecedented for the last 2000 years, as data show records for the periods AD 981–1100 and AD1201–70 are comparable to the present. The ensemble means of dryness/wetness spatial patterns in eastern China across all centennial warm periods illustrate a tripole pattern: dry south of 25°N, wet from 25°–30°N, and dry to the north of 30°N. However, for all centennial cold periods, this spatial pattern also exhibits a meridional distribution. The increase in precipitation over the monsoonal regions of China associated with the 20 th century warming can primarily be attributed to a mega El Nino–Southern Oscillation and the Atlantic Multidecadal Oscillation. In addition, a significant association between increasing numbers of locusts and dry/cold conditions is found in eastern China. Plague intensity also generally increases in concert with wetness in northern China, while more precipitation is likely to have a negative effect in southern China. 相似文献