全文获取类型
收费全文 | 1293篇 |
免费 | 294篇 |
国内免费 | 511篇 |
专业分类
测绘学 | 24篇 |
大气科学 | 588篇 |
地球物理 | 199篇 |
地质学 | 736篇 |
海洋学 | 120篇 |
天文学 | 9篇 |
综合类 | 73篇 |
自然地理 | 349篇 |
出版年
2024年 | 5篇 |
2023年 | 22篇 |
2022年 | 46篇 |
2021年 | 53篇 |
2020年 | 58篇 |
2019年 | 72篇 |
2018年 | 77篇 |
2017年 | 58篇 |
2016年 | 63篇 |
2015年 | 73篇 |
2014年 | 74篇 |
2013年 | 95篇 |
2012年 | 86篇 |
2011年 | 94篇 |
2010年 | 77篇 |
2009年 | 85篇 |
2008年 | 108篇 |
2007年 | 89篇 |
2006年 | 110篇 |
2005年 | 112篇 |
2004年 | 70篇 |
2003年 | 64篇 |
2002年 | 62篇 |
2001年 | 53篇 |
2000年 | 61篇 |
1999年 | 57篇 |
1998年 | 52篇 |
1997年 | 35篇 |
1996年 | 37篇 |
1995年 | 39篇 |
1994年 | 32篇 |
1993年 | 14篇 |
1992年 | 11篇 |
1991年 | 12篇 |
1990年 | 6篇 |
1988年 | 4篇 |
1987年 | 7篇 |
1986年 | 5篇 |
1985年 | 4篇 |
1984年 | 3篇 |
1983年 | 1篇 |
1982年 | 4篇 |
1981年 | 5篇 |
1980年 | 1篇 |
1954年 | 2篇 |
排序方式: 共有2098条查询结果,搜索用时 15 毫秒
271.
272.
The impact of the northward jump and westward movement of the East Asian westerly jet core from the western Pacific Ocean to the Qinghai-Tibet Plateau on precipitation distribution of eastern China is studied. It is concluded that on the one hand, the northward jump of the jet causes the precipitation belt to move northward from the middle and lower reaches of the Yangtze River valley and withdraw during the Mei-yu season; on the other hand, the westward movement of the jet core has no correspondence with withdrawal of the Mei-yu season. However, the earlier or later occurrence of the westward movement of the jet has an influence on the process of the rain belt moving northward than the northward jump of the jet: the rain belt moves northward from the middle-lower Yangtze River valley to the Huaihe River and then to an area between the Yellow River and Huaihe River during years when the time of the westward movement of the jet core is later than that of the northward jump of the jet and from the middle-lower Yangtze River valley to an area between the Yellow River and Huaihe River in other years. Further analysis shows that: (1) The northward jump of the jet and the westward movement of the East Asian westerly jet core causes significant variation of the general atmospheric circulation in middle latitudes and water vapor transport from the western Pacific, but not from the Bay of Bengal. (2) Impact of the northward jump and the westward movement of the East Asian westerly jet core on circulation are different, therefore, water vapor transport from the western Pacific and its impact on the rain belt are different. The earlier or later occurrence of the westward movement of the jet core than the northward jump of the jet causes the process of circulation and water vapor transport to be different which produces a different process of the rain belt moving northward. 相似文献
273.
利用1967-2009年的逐月海表温度(Sea Surface Temperature,SST)资料和降水资料,以及经验正交函数(Empirical Orthogonal Function,EOF)和相关分析方法,探讨了亚印太交汇区(Joining Area of Asia and Indian-Pacific Oce... 相似文献
274.
我国南方初夏汛期和东亚夏季风环流 总被引:12,自引:5,他引:12
主要根据低层夏季风热力学性质与流场演变特点深入讨论我国南方初夏汛期包括华南前汛期和长江中下游梅雨期同夏季风活动的联系,分析了东亚夏季风环流建立过程的阶段性和类型,指出汛期的开始与结束同夏季风前沿位置变动一致。我国夏季风从开始到发展鼎盛时期低纬大气环流的演变过程各年不完全相同,主要可归纳为4类,每类包括4个或3个不同阶段,从而可认识到东亚夏季风体系结构的非单一性,它可有4种结构模型,即仅是东南季风P的单气流型、强东南季风P与弱西南季风A的双气流型、强东南季风P和弱西南季风M的双气流型、强东南季风P和强(或弱)西南季风M以及弱西南季风A的3气流型。 相似文献
275.
刘惠云 《沙漠与绿洲气象(新疆气象)》2001,24(3):9-11
利用1979-1995年6-8月逐月的100hPa平均高度场资料及相对应的降水资料,对新疆夏季降水异常月的南亚高压的环流特征进行了较为系统的分析,分别总结出了南疆和北疆降水偏多月及降水偏少月时南亚高压环流特征不同的8种类型。 相似文献
276.
By analyzing the change of an index for the characteristics of South Asia High and variations of upper-air troughs in 2002–2005,we studied the impact of South Asia high on the beginning and ending of the Mei-yu(i.e.sustained rain corresponding to the ripening season of plum)in Jiangsu province.Statistic verification is conducted on the relationships between the index and the Mei-yu season in 1991–2005 to examine the impacts of the SAH characteristics index on a rain intensity index of Mei-yu and regional distribution of a characteristics index for different annual patterns of Mei-yu.Historical composite is performed of the 100-hPa circulation field for these patterns using the 100-hPa geopotential height of Northern Hemisphere from 2002 to 2005 and 45-year NCEP reanalysis to study the difference in the circulation for different patterns of Mei-yu.Diagnostic and statistic conclusions,which share much in common,have been obtained as follows.(1)The characteristics preceding to and the advancement/retreat of SAH and the movement of westerly troughs are the factors that influence the onset time of the Mei-yu season;after the Mei-yu onset,the progression/withdrawal of SAH and how farther east it extends are determining how long the Mei-yu lasts and when it ends.(2)During the Mei-yu,the general 100-hPa circulation situation and average characteristics of the SAH are well corresponding to the characteristics of the season and annual patterns of Mei-yu.In addition,the averages of the SAH ridgeline and east-extending index for June,July and the Mei-yu season have some implications to the forecast of the index of Mei-yu intensity.These conclusions can be served as powerful means in determining the starting/ending dates, duration and annual pattern of the Mei-yu season. 相似文献
277.
278.
279.
在全球变暖的背景下,近年来东亚冬季气温存在复杂的季节内变化.本文研究了2020/21年东亚冬季气温的月际转折及可预测性.结果 表明,2020/21年东亚冬季气温前冬(2020年12月-2021年1月中旬)偏冷,后冬(2021年1月中旬-2月)偏暖.西伯利亚高压强度在前冬和后冬也出现转折变化.在前冬,由于2020年9月巴... 相似文献
280.