全文获取类型
收费全文 | 1645篇 |
免费 | 252篇 |
国内免费 | 280篇 |
专业分类
测绘学 | 395篇 |
大气科学 | 186篇 |
地球物理 | 396篇 |
地质学 | 591篇 |
海洋学 | 181篇 |
天文学 | 21篇 |
综合类 | 161篇 |
自然地理 | 246篇 |
出版年
2024年 | 2篇 |
2023年 | 14篇 |
2022年 | 44篇 |
2021年 | 60篇 |
2020年 | 69篇 |
2019年 | 72篇 |
2018年 | 60篇 |
2017年 | 78篇 |
2016年 | 86篇 |
2015年 | 85篇 |
2014年 | 90篇 |
2013年 | 99篇 |
2012年 | 101篇 |
2011年 | 95篇 |
2010年 | 93篇 |
2009年 | 123篇 |
2008年 | 101篇 |
2007年 | 108篇 |
2006年 | 83篇 |
2005年 | 90篇 |
2004年 | 85篇 |
2003年 | 69篇 |
2002年 | 59篇 |
2001年 | 57篇 |
2000年 | 46篇 |
1999年 | 37篇 |
1998年 | 41篇 |
1997年 | 43篇 |
1996年 | 26篇 |
1995年 | 32篇 |
1994年 | 21篇 |
1993年 | 23篇 |
1992年 | 24篇 |
1991年 | 23篇 |
1990年 | 7篇 |
1989年 | 4篇 |
1988年 | 10篇 |
1987年 | 5篇 |
1986年 | 5篇 |
1984年 | 1篇 |
1982年 | 1篇 |
1980年 | 1篇 |
1978年 | 1篇 |
1976年 | 1篇 |
1954年 | 2篇 |
排序方式: 共有2177条查询结果,搜索用时 209 毫秒
991.
新疆阿勒泰地区地气温差变化特征分析 总被引:1,自引:0,他引:1
利用阿勒泰地区7个气象站1963-2004年0 cm地温和气温月平均资料,采用统计法、趋势和突变检验方法,分析了该地区地气温差的时空演变特征及突变.研究表明:该地区地气温差6月最大,12月最小;暖季最大,冬季最小,常年存在随季节变化的高低值区域与海拔和地形有关.地气温差受大尺度气候异常的影响,第一载荷向量场反映全区一致的性质,第二、三载荷向量场具有南北差异和东西差异.线性趋势分析表明,地气温差12月-次年2月呈显著下降趋势,4-9月和年均呈显著上升趋势,过渡季节3月和10-11月趋势变化不显著.突变检验表明,10-11月、12月-次年2月该地区地气温差在20世纪60年代末到70年代初发生了显著的突变,与其他文献的结论不同;3月、4-9月和年均在20世纪70年代末到80年代初发生了显著的突变,与其他文献的结论及新疆气候的突变较为一致. 相似文献
992.
993.
994.
湖南省区域经济综合发展水平动态变化研究 总被引:2,自引:0,他引:2
文章运用创新的主成分分析方法构建测度模型,对湖南省的14个地区进行了区域经济发展水平的动态测算。在研究的时间段中,湖南省的区域经济发展水平都有不同程度的增长,但是增长的幅度有较大的差异。导致区域经济的地区绝对差异拉大,而相对差异有所缩小。经济发展水平的增长能力差异是影响地区经济发展水平动态变化的主要因素。 相似文献
995.
Estimation of areal precipitation in the Qilian Mountains based on a gridded dataset since 1961 总被引:1,自引:1,他引:0
Fang Qiang Mingjun Zhang Shengjie Wang Yangmin Liu Zhengguo Ren Xiaofan Zhu 《地理学报(英文版)》2016,26(1):59-69
Based on a 0.5°×0.5° daily gridded precipitation dataset and observations in meteorological stations released by the National Meteorological Information Center, the interannual variation of areal precipitation in the Qilian Mountains during 1961-2012 is investigated using principal component analysis (PCA) and regression analysis, and the relationship between areal precipitation and drought accumulation intensity is also analyzed. The results indicate that the spatial distribution of precipitation in the Qilian Mountains can be well reflected by the gridded dataset. The gridded data-based precipitation in mountainous region is generally larger than that in plain region, and the eastern section of the mountain range usually has more precipitation than the western section. The annual mean areal precipitation in the Qilian Mountains is 724.9×108 m3, and the seasonal means in spring, summer, autumn and winter are 118.9×108 m3, 469.4×108 m3, 122.5×108 m3 and 14.1×108 m3, respectively. Summer is a season with the largest areal precipitation among the four seasons, and the proportion in summer is approximately 64.76%. The areal precipitation in summer, autumn and winter shows increasing trends, but a decreasing trend is seen in spring. Among the four seasons, summer have the largest trend magnitude of 1.7×108 m3×a-1. The correlation between areal precipitation in the mountainous region and dry-wet conditions in the mountains and the surroundings can be well exhibited. There is a negative correlation between drought accumulation intensity and the larger areal precipitation is consistent with the weaker drought intensity for this region. 相似文献
996.
997.
《Geoforum》2017
Understanding the complexity of vulnerability to disasters, including those triggered by floods, droughts and epidemics is at the heart of disaster risk reduction. Despite its importance in disaster risk reduction, there remains a paucity of approaches that contribute to our understanding of social vulnerability that is hidden in dynamic contextual conditions. The study demonstrates an accessible means to assessing the spatial variation of social vulnerability to flood hazards and related for the context of Muzarabani district in northeast Zimbabwe. The study facilitated local identification with residents of variables contributing to social vulnerability and used the principal component analysis (PCA) technique to develop a social vulnerability index (SoVI). Using ArcMap10.2 geographic information systems (GIS) tool, the study mapped composite SoVI at the ward level. The results showed that Muzarabani district is socially vulnerable to hazards. The social vulnerability is influenced by a variety of economic, social and institutional factors that vary across the wards. Quantifying and visualising social vulnerability in Muzarabani provides useful information for decision makers to support disaster preparedness and mitigation programmes. The approach shows how spatially distributed multivariate vulnerability, as grounded in interpretations at local level, can be quantitatively derived for contexts such as those of Muzarabani. The study findings can inform disaster risk reduction communities and cognate disciplines on quantitative assessments for managing hazard vulnerability where these have hitherto not been developed. 相似文献
998.
999.
1000.
James K. H. Fang Christine H. L. Schönberg David I. Kline Ove Hoegh‐Guldberg Sophie Dove 《Marine Ecology》2013,34(2):193-206
This study applied the loss after combustion (LAC) method and the acid decalcification (ADC) method to quantify different components of an excavating sponge. Samples of dried coral skeleton of Favia sp. invaded by the Indo‐Pacific excavating sponge Cliona orientalis Thiele, 1900 were used. The sponge tissue penetrated the 12‐mm‐thick samples to approximately 10 mm. The average proportional weight of organic matter, siliceous spicules, calcareous substrate and salts in the entire samples was found to be respectively 2.5%, 4.4%, 90.5% and 2.5% of dry weight applying the LAC method, and 2.9%, 5.9%, 89.0% and 2.3% of dry weight applying the ADC method. Respective volumetric proportions of the organic matter, spicules, substrate and salts were then calculated to be 6.4%, 5.5%, 85.2% and 3.0% of volume with the LAC method, and 7.4%, 7.2%, 82.7% and 2.7% of volume with the ADC method. The LAC method showed low variability of data and is simple and fast and therefore is recommended. The ADC method generated very similar results to the LAC method. However, due to the handling involved in the ADC method, more than half of the spicules may be lost and the method is therefore not recommended unless careful data corrections are considered. In addition, the buoyant weight method was used to quantify actual substrate weight in the fresh sponge‐substrate samples. This method was found to be at least 97% effective, revealing that buoyant weights can potentially be used to quantify bioerosion rates of excavating sponges. To our knowledge, this is the first study to systemically quantify organic and inorganic components of an excavating sponge and its calcareous substrate, providing improved standard methods for future studies. 相似文献