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 31 毫秒
171.
海河平原东部地区地面沉降机理与趋势 总被引:8,自引:0,他引:8
海河平原东部地区是中国水资源最紧缺的地区之一。地下水开采量占该地区供水总水量的60%以上。深、浅层地下水超采量均超过500亿m^3。该区也是山前拦蓄地表径流最高的地区,大小水库达1820多座,拦蓄能力320亿m^3,控制山区流域面积近90%。在地下水补给源减少与大规模超采地下水的综合作用下,造成平原区河流干涸、地下水水位持续下降、含水层疏干及地面沉降等环境地质问题。同时诱发了含水层之间强越流渗透以求动力场平衡问题,第四系松散地层出现垂向压密而导致地层塑性变形。在滨海平原区,区域性地层垂向压密变形存在缓慢发展趋势。研究表明,地面沉降致灾过程至少存在3个阶段,即自然沉降机制阶段、缓变劣变质变阶段以及快速衰变破坏阶段。缓变劣变质变阶段是采取措施减灾最佳时期。 相似文献
172.
Heating status of the Tibetan Plateau from April to June and rainfall and atmospheric circulation anomaly over East Asia in midsummer 总被引:20,自引:0,他引:20
DUAN Anmin LIU Yimin & WU Guoxiong State Key Laboratory of Numerical Modeling for Atmospheric Sciences Geophysical Fluid Dynamics Institute of Atmospheric Physics Chinese Academy of Sciences Beijing China 《中国科学D辑(英文版)》2005,48(2):250-257
Based on the 1958-1999 monthly averaged reanalysis data of the National Center for Environmental Prediction (NCEP)/National Center for Atmospheric Research (NCAR) and the rainfall data of 160 Chinese surface stations, the relationship between rainfall and the atmospheric circulation anomaly over East Asia (EA) in July and the sensible heating (SH) over the Tibetan Plateau (TP) from April to June (AMJ) is investigated by using the rotational experimental orthogonal function (REOF) method. The results show that the TP is an isolated heating source in this period. The lagged correlation analysis between the first rotational principal component (RPC) of SH over the TP in May and rainfall of EA in July demonstrates that strong SH over the TP before July leads to a positive rainfall anomaly over the TP, the valley between the Yangtze River and Huaihe River, and the regions south and southeast of the TP, and the Sichuan Basin and Yunnan-Guizhou Plateau, but less rainfall anomaly over the regions north, northeas 相似文献
173.
174.
Joseph Morgan 《Marine Policy》1984,8(4):299-310
If problems of ocean management are to be solved the seas must be divided up into appropriate regions. Regional boundaries can be based on factors of physical geography or on economic, political or management principles. South-east Asia, with complicated land-sea boundaries, provides a number of examples of different types of marine regions, which can be used as case study examples of problems and solutions in regionalizing the oceans. Eight regional types and locations are described and discussed, and it is concluded that regional arrangements for management or the solution of problems are at present limited to three: the Malacca-Singapore Straits, Andaman Sea and Celebes Sea. 相似文献
175.
南海北部一百万年以来的表层古生产力变化:来自ODP1144站的蛋白石记录 总被引:7,自引:1,他引:6
通过南海北部ODP 1144站蛋白石含量测定及其堆积速率的计算,并结合氧同位素记录等相关资料,获得南海北部1050ka以来高分辨率的表层古生产力变化与冰期旋回和东亚季风的关系。约900ka以来,蛋白石含量及其堆积速率较900ka以前明显增加,反映了“中更新世革命”事件之后,全球气候变冷,并导致表层生产力的提高。由于第四纪冰期旋回中的冬、夏季风的加强,加上1144站特殊的地理位置,使该站在冰期时表层生产力增加,间冰期时表层生产力降低。浮游有孔虫氧同位素记录与蛋白石含量及其堆积速率的时间序列频谱分析结果显示,三者均出现了相对应的偏心率周期、斜率周期和岁差周期,说明该站表层生产力的变化主要受地球轨道周期的驱动。 相似文献
176.
CunDe Xiao ZhongQin Li Lin Zhao ShiChang Kang YuanQing He Xiang Qin XiaoBo He 《寒旱区科学》2012,4(1):0001-0012
In coordination with Global Cryosphere Watch (GCW) initiated by World Meteorology Administration (WMO), a regional observation
network is proposed based on existing stations/sites over High Asia and cryospheric elements required by GCW. Thus,
High Asian Cryosphere (HAC) network is preliminary designed, composing of seven "supersites", each containing several reference
sites. The network covers major mountain ranges in High Asia, such as East Tianshan, Qilian, Tanggula, Nyainqentanglha,
Himalayas as well as the central and eastern Qinghai-Xizang (Tibet) Plateau. Although multiple cryospheric elements were observed
at the existing HAC network, many others, which are required by Integrated Global Observation System-Cryosphere
Theme (IGOS-Cryosphere), are not yet included. More comprehensive observations are necessary to be included into "supersites"
of HAC, so that the basic requirements for validation of satellite data, assimilation and coupled regional models can be met. 相似文献
177.
The authors investigate monsoon change in East Asia in the 21st century under the Special Report on Emissions Scenarios (SRES) A1B scenario using the results of a regional climate model, RegCM3, with a high horizontal resolution. First, the authors evaluate the model’s performance compared with NCEP-NCAR reanalysis data, showing that the model can reliably reproduce the basic climatology of both winter and summer monsoons over East Asia. Next, it is found that the winter monsoon in East Asia would slightly weaken in the 21st century with spatial differences. Over northern East China, anomalous southerly winds would dominate in the mid-and late-21st century because the zonal land-sea thermal contrast is expected to become smaller, due to a stronger warming trend over land than over ocean. However, the intensity of the summer monsoon in East Asia shows a statistically significant upward trend over this century because the zonal land-sea thermal contrast between East Asia and the western North Pacific would become larger, which, in turn, would lead to larger sea level pressure gradients throughout East Asia and extending to the adjacent ocean. 相似文献
178.
The Impact of Mid- and High-Latitude Rossby Wave Activities
on the Medium-Range Evolution of the EAP Pattern During
the Pre-Rainy Period of South China
下载免费PDF全文
![点击此处可从《Acta Meteorologica Sinica》网站下载免费的PDF全文](/ch/ext_images/free.gif)
Based on the NCEP DOE AMIP II daily reanalysis data (1979{2005), the evolution of the East Asia/Pacific(EAP) teleconnection pattern during the pre-rainy period of South China is studied on the medium-range time scale. It is found that positive and negative EAP patterns share a similar generation process. In the middle and upper troposphere, Rossby wave packets emanating from the northeast Atlantic or Europe propagate toward East Asia along the Eurasian continent waveguide and finally give rise to the three anomaly centers of the EAP pattern over East Asia. Among the three anomaly centers, the western Pacific subtropical center appears the latest. Rossby wave packets propagate from the high latitude anomaly center toward the mid-latitude and the subtropical ones. The enhancement and maintenance of the subtropical anomaly center is closely associated with the subtropical jet waveguide and the incoming Rossby wave packets from the upstream. In the lower troposphere, Rossby wave packets emanate from the subtropical Asia toward East Asia.
Positive and negative EAP patterns could not be regarded as "mirrors" to each other with simply re-
versed phase. For the positive pattern, the positive height anomaly center around the Scandinavia Peninsula keeps its strength and position during the mature period, and the Rossby wave packets thus propagate persistently toward East Asia, facilitating a longer mature time of the positive pattern. As for the formation of the negative EAP pattern, however, the incoming Rossby wave energy from the upstream contributes to both the enhancement and southeastward movement of the negative anomaly belt from the Yenisei River to the Bering Strait and the positive anomaly center around Mongolia. At the peak time, the two anomlous circulations are evolved into the Northeast Asia and the mid-latitude anomaly centers of the negative pattern, respectively. The energy dispersion of Rossby wave packets is relatively fast due to the predominant zonal circulation in the extratropics, causing a shorter mature period of the negative pattern.
During the pre-rainy period of South China, the prevalence of the EAP pattern signiˉcantly affects the rainfall over the region south of the Yangtze River. The positive (negative) EAP pattern tends to causepositive (negative) precipitation anomalies in that region. This is di?erent from the earlier research findingsbased on monthly mean data. 相似文献
179.
180.
2007年淮河流域暴雨期间大气环流特征分析 总被引:6,自引:3,他引:3
利用NCAR/NCEP再分析资料及国家气象信息中心30年气候平均降水资料,通过动力诊断与分析手段研究了2007年6—7月发生在我国淮河流域的暴雨。结果表明,淮河流域的环流垂直结构和降水有着非常好的对应关系。暴雨期间,鄂霍茨克海阻高与乌拉尔山阻高这种双阻高形势对于淮河流域的持续降水提供了很好的条件;南亚高压高层(200 hPa)基本为正散度区,低层(850 hPa)为负散度区,上下层强烈的抽吸结构对暴雨的发生也是非常有利的条件,同时,在淮河暴雨期问,南亚高压(200 hPa)与500 hPa西太平洋副热带高压有着相向而行的移动路径;位涡对于分析冷空气的活动,有着比较清晰的意义,暴雨发生前,有明显的正位涡异常从高纬度向低纬度伸展。大气非绝热加热分析结果显示,视热源和视水汽汇两者的高值中心与相应时段暴雨中心位置一致。 相似文献