全文获取类型
收费全文 | 63篇 |
免费 | 63篇 |
国内免费 | 107篇 |
专业分类
大气科学 | 203篇 |
地球物理 | 25篇 |
地质学 | 1篇 |
自然地理 | 4篇 |
出版年
2023年 | 3篇 |
2022年 | 4篇 |
2021年 | 1篇 |
2020年 | 1篇 |
2019年 | 2篇 |
2018年 | 5篇 |
2016年 | 3篇 |
2015年 | 1篇 |
2014年 | 8篇 |
2013年 | 5篇 |
2012年 | 5篇 |
2011年 | 9篇 |
2010年 | 6篇 |
2009年 | 4篇 |
2008年 | 4篇 |
2007年 | 7篇 |
2006年 | 7篇 |
2005年 | 20篇 |
2004年 | 11篇 |
2003年 | 14篇 |
2002年 | 23篇 |
2001年 | 7篇 |
2000年 | 15篇 |
1999年 | 6篇 |
1998年 | 5篇 |
1997年 | 3篇 |
1996年 | 5篇 |
1995年 | 1篇 |
1994年 | 5篇 |
1993年 | 10篇 |
1992年 | 9篇 |
1991年 | 11篇 |
1990年 | 4篇 |
1989年 | 2篇 |
1987年 | 2篇 |
1986年 | 2篇 |
1985年 | 1篇 |
1983年 | 1篇 |
1979年 | 1篇 |
排序方式: 共有233条查询结果,搜索用时 15 毫秒
231.
长江流域水汽收支与高原水汽输送分量“转换”特征 总被引:33,自引:3,他引:30
文中采用"箱体"模型边界的整层水汽输送特征描述长江流域梅雨带水汽收支总体效应,发现长江流域夏季降水与"箱体"模型整层水汽输送收支总量呈显著相关;青藏高原动力、热力强迫构成周边水汽输送特殊流型结构,大地形动力强迫导致高原周边水汽输送在高原南侧与东侧存在经向或纬向不同分量的水汽流型,且它们分别对长江流域梅雨带"箱体"模型水汽收支具有重要的影响.研究还发现高原南侧经向水汽输送与高原东侧纬向水汽输送分量之间呈显著相关特征,此研究揭示了长江流域洪涝过程上游高原周边关键区水汽输送不同分量间的"转换"特征,且此类水汽输送流型对夏季长江全流域各区域降水具有不同程度影响.上述高原周边水汽输送经向-纬向分量间的相互"转换"效应,是认识长江流域异常洪涝过程形成的关键环节之一.高原周边水汽输送分量相关结构及区域边界水汽收支问题将为长江流域洪涝预报提供科学依据. 相似文献
232.
233.
The Response of Anomalous Vertically Integrated Moisture Flux Patterns Related to Drought and Flood in Southern China to Sea Surface Temperature Anomaly 下载免费PDF全文
With the extreme drought (flood) event in southern China from July to August in 2022 (1999) as the research object, based on the comprehensive diagnosis and composite analysis on the anomalous drought and flood years from July to August in 1961-2022, it is found that there are significant differences in the characteristics of the vertically integrated moisture flux (VIMF) anomaly circulation pattern and the VIMF convergence (VIMFC) anomaly in southern China in drought and flood years, and the VIMFC, a physical quantity, can be regarded as an indicative physical factor for the "strong signal" of drought and flood in southern China. Specifically, in drought years, the VIMF anomaly in southern China is an anticyclonic circulation pattern and the divergence characteristics of the VIMFC are prominent, while those are opposite in flood years. Based on the SST anomaly in the typical draught year of 2022 in southern China and the SST deviation distribution characteristics of abnormal draught and flood years from 1961 to 2022, five SST high impact areas (i.e., the North Pacific Ocean, Northwest Pacific Ocean, Southwest Pacific Ocean, Indian Ocean, and East Pacific Ocean) are selected via the correlation analysis of VIMFC and the global SST in the preceding months (May and June) and in the study period (July and August) in 1961-2022, and their contributions to drought and flood in southern China are quantified. Our study reveals not only the persistent anomalous variation of SST in the Pacific and the Indian Ocean but also its impact on the pattern of moisture transport. Furthermore, it can be discovered from the positive and negative phase fitting of SST that the SST composite flow field in high impact areas can exhibit two types of anomalous moisture transport structures that are opposite to each other, namely an anticyclonic (cyclonic) circulation pattern anomaly in southern China and the coastal areas of east China. These two types of opposite anomalous moisture transport structures can not only drive the formation of drought (flood) in southern China but also exert its influence on the persistent development of the extreme weather. 相似文献