全文获取类型
收费全文 | 3885篇 |
免费 | 864篇 |
国内免费 | 644篇 |
专业分类
测绘学 | 81篇 |
大气科学 | 203篇 |
地球物理 | 2884篇 |
地质学 | 1099篇 |
海洋学 | 598篇 |
天文学 | 9篇 |
综合类 | 181篇 |
自然地理 | 338篇 |
出版年
2024年 | 15篇 |
2023年 | 57篇 |
2022年 | 133篇 |
2021年 | 153篇 |
2020年 | 204篇 |
2019年 | 210篇 |
2018年 | 184篇 |
2017年 | 192篇 |
2016年 | 182篇 |
2015年 | 230篇 |
2014年 | 289篇 |
2013年 | 240篇 |
2012年 | 250篇 |
2011年 | 271篇 |
2010年 | 252篇 |
2009年 | 254篇 |
2008年 | 246篇 |
2007年 | 276篇 |
2006年 | 230篇 |
2005年 | 208篇 |
2004年 | 197篇 |
2003年 | 170篇 |
2002年 | 154篇 |
2001年 | 111篇 |
2000年 | 114篇 |
1999年 | 104篇 |
1998年 | 97篇 |
1997年 | 88篇 |
1996年 | 78篇 |
1995年 | 51篇 |
1994年 | 39篇 |
1993年 | 32篇 |
1992年 | 22篇 |
1991年 | 15篇 |
1990年 | 11篇 |
1989年 | 9篇 |
1988年 | 5篇 |
1987年 | 6篇 |
1986年 | 2篇 |
1985年 | 4篇 |
1984年 | 2篇 |
1983年 | 1篇 |
1982年 | 2篇 |
1979年 | 2篇 |
1954年 | 1篇 |
排序方式: 共有5393条查询结果,搜索用时 641 毫秒
991.
992.
993.
994.
995.
A three-dimensional model study on ocean dynamic response to traveling cyclone over the Huanghai Sea
On the basis of numerical simulation of the mean circulation and relevant thermal-salinity fields in June with a three-dimensional ocean model (ECOM-si), the model outputs are used as first guess of initial fields for numerical integration of the model equations and the numerical results are applied to investigating the dynamical responses of the Huanghai Sea and the East China Sea (HECS) in the course of a weak land-to-sea cyclone‘s passage over the Huanghai Sea on 15-16 June 1999. Predominance of the dynamic impact of cyclone over the thermal one in June in the HECS is justified using observations and model simulations.The cyclone and its surrounding weather system, i.e,, subtropical high ridge to its south could influence current and thermal fields in the Bohai Sea, the Huanghai Sea and the northern East China Sea even though the intensity of cyclone was rather weak. The response of oceanic currents to the wind stresses driven by the cyclone and its southern subtropical high were strongly characterized by the wind drift with its extent of equivalent scale of cyclone in the horizontal and of Ekman layer in the vertical. The sea response at a given site was closely related to the transient local wind speed and direction,especially was sensitive to the local wind direction,which is demonstrated at three points locating at the southern and western Huanghai Sea and the northern East China Sea. So the sea responses at locations differed considerably from one another. Current responded to the wind stress in a simple way:directly to the wind-driven current and subsequent gradient current and slope current, etc., whereas sea temperature responded to the wind stress in two ways: directly to the cyclone-induced cooling and indirectly to water movements both in the horizontal and the vertical by the cyclone‘ s wind stress. So the sea temperature variation under the influence of cyclone was more complicate than the current. The HECS in response to the cyclone and its ambient weather system was likely to be a fast process and such a response could last at least for more than 1d. Current increased with the duration of wind stress exerted on the surface and decreased with the increasing depth. Affected by the cyclone, the maximum sea surface temperature decreased by almost 1.6℃ during the 24h cyclone. 相似文献
996.
黄河高含沙量水体在弱潮陆相河口入海,80 %的泥沙在河口附近快速堆积。过去研究发现,黄河三角洲潮滩表层沉积物呈现非均匀固结状态。为了揭示该现象产生的机制,在黄河刁口流路三角洲叶瓣潮坪上,现场取土配置黄河口快速沉积形成的流体状堆积物,研究快速沉积的粉质海床土在波浪和潮波作用下的孔压响应及非均匀固结过程。利用静力触探、十字板剪切试验、孔隙水压力监测等原位测试手段,实时测定快速沉积的海床土强度和孔压变化过程。研究发现,快速沉积的粉质土在自重作用下的固结速度很快,正常固结完成后,强度随时间的发展依然不断增加,沿深度方向出现类似原状土体的固结非均匀现象和似超固结状态;在波浪和潮波作用下快速沉积粉质土孔压沿深度出现非均匀变化,在波浪作用下出现了超静孔压的积累。分析发现,该固结状态和强度沿深度方向非均匀变化是由于土体在潮波及潮波和波浪的联合作用下形成的;潮滩表层土体在波浪荷载长期作用下形成硬壳层。 相似文献
997.
在考虑横观各向同性含液饱和多孔介质固体骨架和流体可压缩性以及固体骨架的黏弹性特征下,基于横观各向同性含液饱和多孔介质u-w形式的三维动力控制方程,以固相位移u、液相相对位移w为基本未知量,综合运用Laplace变换、双重Fourier变换等方法,在直角坐标系下通过引入中间变量,将六元2阶动力控制方程组化为两组各含4个未知变量的常微分方程组,给出了直角坐标系下横观各向同性含液饱和多孔介质三维黏弹性动力反应的积分形式一般解;作为理论推导的验证,通过引入初始条件和边界条件,对横观各向同性含液饱和多孔介质半空间黏弹性瞬态反应问题进行了求解。解答的退化验证表明,所推导的理论解是正确的。 相似文献
998.
中国西北近45a来极端低温事件及其对区域增暖的响应 总被引:9,自引:2,他引:7
利用中国西北五省(区)1960-2004年100个台站逐日最低温度资料,通过百分位法定义了不同台站的逐日极端低温阈值,对近45 a来西北地区逐年极端低温事件发生频次进行了时空诊断,并分析其同西北区域性增暖的响应.结果表明:一致性异常分布是中国西北年极端低温事件发生频次的最主要空间模态;中国西北年极端低温事件发生频次的空间分布可分为以下5个关键区:北疆区、青海北部区、西北东部区、南疆区及青南高原区;年极端低温事件发生频次除了青南高原区表现为微弱的减少趋势外,北疆区、青海北部区、西北东部区和南疆区均表现为显著的减少趋势,并且发生了突变现象.在年极端低温事件发生频次的各主要空间分区中,13~15 a和7~8 a的周期在所有分区中反映得比较清楚;年极端低温事件发生频次对西北区域性增暖呈显著负响应. 相似文献
999.
Neolithic culture series in the Yishu River Basin developed in the order of Beixin culture-Dawenkou culture-Longshan culture-Yueshi culture. During the early and middle stage of Longshan culture (4600-4300 cal. yr BP), the climate in the Yishu River Basin was warm and wet. Paddy-oriented agriculture planted paddy was very developed. The society was flourishing with great amount of archaeological sites. The cooling starting in 4200 cal. yr BP made the paddies shortfall in output or even no seeds were gathered. This situation intensified the discrepancy between population and resource. The scarcity in natural resource led to substantial decrease in population and subsequent drop in archaeological sites. About 4000 cal. yr BP Longshan culture was displaced by Yueshi culture which was relatively un- derdeveloped, simple and unsophisticated. 相似文献
1000.