全文获取类型
收费全文 | 2828篇 |
免费 | 314篇 |
国内免费 | 287篇 |
专业分类
测绘学 | 150篇 |
大气科学 | 204篇 |
地球物理 | 550篇 |
地质学 | 850篇 |
海洋学 | 766篇 |
天文学 | 3篇 |
综合类 | 163篇 |
自然地理 | 743篇 |
出版年
2024年 | 5篇 |
2023年 | 25篇 |
2022年 | 93篇 |
2021年 | 94篇 |
2020年 | 101篇 |
2019年 | 116篇 |
2018年 | 94篇 |
2017年 | 126篇 |
2016年 | 135篇 |
2015年 | 122篇 |
2014年 | 187篇 |
2013年 | 175篇 |
2012年 | 145篇 |
2011年 | 194篇 |
2010年 | 136篇 |
2009年 | 208篇 |
2008年 | 183篇 |
2007年 | 200篇 |
2006年 | 151篇 |
2005年 | 145篇 |
2004年 | 107篇 |
2003年 | 102篇 |
2002年 | 87篇 |
2001年 | 74篇 |
2000年 | 77篇 |
1999年 | 49篇 |
1998年 | 50篇 |
1997年 | 52篇 |
1996年 | 24篇 |
1995年 | 41篇 |
1994年 | 24篇 |
1993年 | 17篇 |
1992年 | 17篇 |
1991年 | 14篇 |
1990年 | 10篇 |
1989年 | 14篇 |
1988年 | 7篇 |
1987年 | 2篇 |
1986年 | 1篇 |
1985年 | 4篇 |
1984年 | 7篇 |
1983年 | 7篇 |
1982年 | 2篇 |
1981年 | 1篇 |
1979年 | 2篇 |
1978年 | 1篇 |
1971年 | 1篇 |
排序方式: 共有3429条查询结果,搜索用时 15 毫秒
41.
闽浙沿岸上升流的数值模拟 总被引:1,自引:1,他引:1
本文将闽浙沿岸作为研究海区,采用坐标下三维斜压非线性的浅海陆架模式,综合考虑风、边界流(台湾暖流、黑潮、长江冲淡水)及地形等动力因子对上升流形成的影响,较好地模拟了闽浙沿岸上升流的分布。得出夏季闽浙沿岸近海岸区域有三个比较强的上升流中心,分别位于2520′N,12000′E、2640′N,12015′E、2720′N,12045′E附近,并且在对闽浙沿岸水文结构的模拟中,同样得出夏季沿岸的低温高盐区与计算出的三个较强的上升中心一致。冬季沿岸上升流的强度和范围都明显减弱,但在2520′N,12000′E和2600′N,12030′E及2830′~3000′N,12200′E附近仍有相对较强的上升流存在。 相似文献
42.
Particularly Sensitive Sea Areas (PSSAs) are a tool designed to protect vulnerable marine areas from vessel-source pollution through measures approved by the governing body, the International Maritime Organisation. Recent developments triggered by the proposal to designate, amongst others, a large part of the Western European Atlantic a PSSA have brought the instrument to a decisive stage. Although the proposal appears to be lawful, its implications for the concept, which this paper seeks to assess, are questionable. The significance of the instrument is at risk if it is overused. As a consequence, new protective mechanisms should be contemplated. 相似文献
43.
介绍了浙江东南沿海的台州市及所属玉环县、温州市及所属乐清市、瓯海区等地面实施海洋“蓝色工程”的丰富实践和新鲜经验。文中借鉴浙东南沿海大开发的成功经验,结合我国东部沿海其它地区特别是苏北沿海的实际,提出了做出滩涂开发利用、发展海洋经济的总体战略构想。 相似文献
44.
This paper explores the application of the US Sea Grant model of applied research, extension, and education to two case studies in Latin America: Coastal Ecuador and the Gulf of Fonseca. The analysis is based on a series of meetings and roundtables with in-country partners and leaders of the US Sea Grant program. We conclude that the Sea Grant model provides an institutional structure that Latin America lacks and the model's features would improve governance of marine and coastal resources through more effective linkages between coastal communities, universities, and policy/decision makers at local, national, and international levels. 相似文献
45.
46.
海岸带是影响人类活动的重要地带,海岸带专题地图能够详细表示出海岸带的特性。随着海洋经济的发展,海岸图的需求日益增加。从地图的数学要素出发,提出目前海岸图绘制存在的问题,并从地图学、海洋学、遥感地学的角度,对地图投影的选择、坐标系转换、比例尺对海岸图编绘的影响及控制点的确定等问题进行了综合分析。 相似文献
47.
J. Nicholson I. Broker J. A. Roelvink D. Price J. M. Tanguy L. Moreno 《Coastal Engineering》1997,31(1-4)
Five different coastal area morphodynamic models have been set up to run on the same offshore breakwater layout and an intercomparison carried out on the hydrodynamic and morphodynamic output produced by each scheme. In addition, the predicted morphodynamics was checked against available laboratory and field data.It is concluded that the models are capable of producing realistic estimates for the dominant morphodynamic features associated with offshore breakwaters. Coupling of the wave, current and sediment transport components of each scheme is shown to yield bathymetry which attains a state of equilibrium, unlike models which are based on the initial transport field only. 相似文献
48.
A phase-resolving wave transformation module is combined with an intra-wave sediment transport module to calculate the on-/offshore sediment transport rates. The wave module is based on the Boussinesq equations extended into the surf zone. The vertical variation of the mean undertow and the intra-wave sediment concentrations are calculated. The net sediment transport rates are calculated, and the equation for conservation of sediment is solved to predict the beach profile evolution. The results of the present paper showed that the undertow contribution to the sediment transport rates is not dominating in all parts of the surf zone, even for eroding beaches, suggesting that other contributions should not be neglected. The present model also showed that for the same offshore wave energy the time series of the oscillatory motion is important and that the effect of wave groups cannot be disregarded. 相似文献
49.
50.