首页 | 本学科首页   官方微博 | 高级检索  
文章检索
  按 检索   检索词:      
出版年份:   被引次数:   他引次数: 提示:输入*表示无穷大
  收费全文   284篇
  免费   32篇
  国内免费   32篇
测绘学   33篇
大气科学   22篇
地球物理   13篇
地质学   66篇
海洋学   87篇
天文学   1篇
综合类   47篇
自然地理   79篇
  2024年   4篇
  2023年   5篇
  2022年   8篇
  2021年   10篇
  2020年   3篇
  2019年   9篇
  2018年   7篇
  2017年   6篇
  2016年   6篇
  2015年   8篇
  2014年   31篇
  2013年   21篇
  2012年   12篇
  2011年   18篇
  2010年   20篇
  2009年   29篇
  2008年   23篇
  2007年   8篇
  2006年   10篇
  2005年   6篇
  2004年   5篇
  2003年   9篇
  2002年   4篇
  2001年   6篇
  2000年   5篇
  1999年   8篇
  1998年   5篇
  1997年   12篇
  1996年   8篇
  1995年   5篇
  1994年   14篇
  1993年   4篇
  1992年   9篇
  1991年   5篇
  1990年   1篇
  1989年   3篇
  1959年   1篇
排序方式: 共有348条查询结果,搜索用时 31 毫秒
11.
汽车运输安全管理中的问题与对策   总被引:2,自引:0,他引:2  
  相似文献   
12.
13.
《地理教学》2005,(2):47-47
据俄罗斯媒体2004年12月31日报道,俄政府已决定由俄国营石油运输公司修建一条从泰舍特至纳霍德卡的石油运输管道,预计该管道输油能力为每年8000万吨。  相似文献   
14.
The origin of the Ryukyu Current(RC) and the formation of its subsurface velocity core were investigated using a 23-year(1993–2015) global Hybrid Coordinate Ocean Model(HYCOM) dataset. The volume transport of the RC comes from the Kuroshio eastward branch(KEB) east of Taiwan and part of the North Pacific Subtropical Gyre(pNPSG). From the surface to 2 000 m depth, the KEB(p-NPSG) transport contributes 41.5%(58.5%) to the mean total RC transport. The KEB originally forms the subsurface velocity core of the RC east of Taiwan due to blockage of the subsurface Kuroshio by the Ilan Ridge(sill depth: 700 m). Above 700 m, the Kuroshio can enter the East China Sea(ECS) over the Ilan Ridge, meanwhile, the blocked Kuroshio below 700 m turns to the right and flows along the Ryukyu Islands. With the RC flowing northeastward, the p-NPSG contribution strengthens the subsurface maximum structure of the RC owing to the blockage of the Ryukyu Ridge. In the surface layer, the pNPSG cannot form a stable northeastward current due to frequent disturbance by mesoscale eddies and water exchange through the gaps(with net volume transport into ECS) between the Ryukyu Islands.  相似文献   
15.
深海经济问题国际研究动态及启示   总被引:1,自引:0,他引:1  
深海经济问题已经成为国际学术界关于海洋经济问题研究的新领域.文章从深海资源与环境、深海渔业、深海工业和深海运输等方面对深海经济国际文献进行了初步梳理,以期为我国深海经济问题的深入研究提供借鉴.  相似文献   
16.
There exists a tongueshaped swelldominance pool known as Swell Pool (SP) in the Eastern Pacific region. The monthlymean wave transports (WT) for each month of 2000 is computed using the wave products of ECMWF reanalysis data. By comparing the 2000 monthlymean WT and monthlymean wind field from QUICKSCAT, large differences are found between the wave transport direction and the wind direction over the Eastern Pacific. This may serve as an evidence for the existence of the SP in this region. The work done in this study indicates that the sources of swell in the Tropical Eastern Pacific (TEP) are in the westerly regions of the Southern and Northern Pacific.  相似文献   
17.
A dual channel difference (DCD) method is applied to detect nighttime sea fog/stratus over the Huanghai Sea using the infrared (IR) data of shortwave (3.5–4.0 μm) and longwave (10.3–11.3 μm) channels from the Multi-functional Transport Satellite (MTSAT)-1R, i.e., shortwave minus longwave brightness temperature difference (SLTD). Twenty-four sea fog events over the Huanghai Sea during March to July of 2006 and 2007 are chosen to determine a suitable value of SLTD for nighttime sea fog/stratus detection, and ...  相似文献   
18.
The results of the new concept of coastal sea circulation are demonstrated by numerical simulations for the first time. The numerical experiments in three types of rectangular model seas illustrate the dependence of circulation on tidal phases due to the convectively nonlinear effect which is estimated by a newly defined drift dispersion in-dex. Then, the present theory is applied in the Bohai Sea of China. At the Bohai Straits and the Huanghe River mouth area the circulation direction even reverses owing to different initial tidal phases which shows that the the-ory copes with nonlinearity well. The calculated M2 tide-induced residual circulation shows that a clockwise gyre exists in the center of an anticlockwise gyre in the central Bohai Sea due to the topographic features. In the Bo-hai Gulf the tide induced circulation shows a 3D structure with outflow at the surface and the inflow at the bottom which can partly explains the spread of the Huanghe River fresh water out of the Bohai Gulf and the inflow of the sediment from the Huanghe River.  相似文献   
19.
The Luzon Strait is the main impact pathway of the Kuroshio on the circulation in South China Sea (SCS). Based on the analysis of the 1997–2007 altimeter data and 2005–2006 output data from a high resolution global HYCOM model, the total Luzon Strait Transport (LST) has remarkable subseasonal oscillations with a typical period of 90 to 120 days, and an average value of 1.9 Sv into SCS. Further spectrum analysis shows that the temporal variability of the LST at different depth is remarkable different. In the upper layer (0–300 m), westward inflow has significant seasonal and subseasonal variability. In the bottom layer (below 1 200 m), eastward outflow exhibits remarkable seasonal variability, while subseasonal variability is also clear. In the intermediate layer, the westward inflow is slightly bigger than the eastward outflow, and both of them have obvious seasonal and subseasonal variability. Because the seasonal variation of westward inflow and eastward outflow is opposite, the total transport of intermediate layer exhibits significant 50–150 days variation, without obvious seasonal signals. The westward Rossby waves with a period of 90 to 120 days in the Western Pacific have very clear correlationship with the Luzon Strait Transport, this indicates that the interaction between these westward Rossby waves and Kuroshio might be the possible mechanism of the subseasonal variation of the LST.  相似文献   
20.
为了解决天然气资源利用问题,我国在广东、福建等沿海地区开始布局液化天然气(LNG)接受站,从国外输入LNG。LNG从输出地到输入地需要通过LNG船运输。为了解决LNG的运输需求,需要生产运输LNG的LNG船。中国已在上海市建造14.7万m3的LNG船舶,并积极开展新一代大型LNG船舶的研发工作。根据我国LNG船舶的建造与发展,已与国际LNG船舶市场接执,今后将在国际LNG船市场占有重要地位。  相似文献   
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号