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   1598篇
  免费   256篇
  国内免费   343篇
测绘学   106篇
大气科学   303篇
地球物理   394篇
地质学   750篇
海洋学   172篇
天文学   129篇
综合类   176篇
自然地理   167篇
  2024年   9篇
  2023年   24篇
  2022年   78篇
  2021年   89篇
  2020年   58篇
  2019年   100篇
  2018年   74篇
  2017年   79篇
  2016年   88篇
  2015年   63篇
  2014年   97篇
  2013年   71篇
  2012年   74篇
  2011年   75篇
  2010年   94篇
  2009年   93篇
  2008年   95篇
  2007年   81篇
  2006年   57篇
  2005年   68篇
  2004年   26篇
  2003年   41篇
  2002年   36篇
  2001年   42篇
  2000年   69篇
  1999年   82篇
  1998年   60篇
  1997年   50篇
  1996年   59篇
  1995年   48篇
  1994年   42篇
  1993年   35篇
  1992年   22篇
  1991年   22篇
  1990年   17篇
  1989年   24篇
  1988年   17篇
  1987年   7篇
  1986年   6篇
  1985年   4篇
  1984年   2篇
  1983年   5篇
  1982年   5篇
  1981年   1篇
  1979年   3篇
  1978年   1篇
  1977年   2篇
  1958年   2篇
排序方式: 共有2197条查询结果,搜索用时 31 毫秒
941.
利用2016年春、夏季节陕西99个国家站的气温逐1 h观测数据,对ECMWF高分辨率数值模式对陕西国家站0~72 h逐3 h和78~240 h逐6 h的气温预报性能进行评估。结果表明,陕西大部分地区,气温预报误差≤1 ℃和≤2 ℃的准确率在72 h之前分别为30%~50%和55%~85%,96 h之后分别为10%~30%和25%~55%,夏季的准确率高于春季,20:00起报的准确率略高于08:00起报。随着预报时效的增加,模式的气温预报能力和稳定性波浪式下降,日变化特征明显,23:00至次日11:00时段的预报能力和稳定性好于14:00—20:00时段。模式的气温预报值与观测值有很好的相关性,但是模式和实际观测站的地形高度差异会对气温预报质量产生较大影响。基于气温垂直变率和模式与实际观测站的地形高度差异进行的高度差订正,可以适当提高模式的气温预报水平,文中提出的几种气温预报的高度差订正方法,对陕西大部分地区的气温预报为正订正效果,但还存在一些问题,有待进一步研究。  相似文献   
942.
Dai  Jun  Wang  Huizan  Zhang  Weimin  An  Yuzhu  Zhang  Ren 《中国海洋湖沼学报》2020,38(6):1654-1675
Journal of Oceanology and Limnology - As in-situ observations are sparse, targeted observations of a specific mesoscale eddy are rare. Therefore, it is difficult to study the three-dimensional...  相似文献   
943.
Insufficient vertical mixing in the upper ocean during summer is a common problem of oceanic circulation and climate models. The turbulence associated with non-breaking waves is widely believed to effectively solve this problem. In many studies, non-breaking surface wave processes are attributed to the effects of Langmuir circulations(LCs). In the present work, the influences of LCs on the upper-ocean thermal structure are examined by using one-and three-dimensional ocean circulation, as well as climate, models. The results indicated that the effect of vertical mixing enhanced by LCs is limited to the upper ocean. The models evaluated, including those considering LC effects alone and the combined effects of LCs and wave breaking, failed to produce a reasonable summertime thermocline, resulting in a large cold bias in the subsurface layer. Therefore, while they can slightly reduce the biases of mixed layer depths and sea surface temperatures in models, LCs are insufficient to solve the problem of insufficient vertical mixing. Moreover, restriction of non-breaking surface wave-induced processes in LCs may be questionable.  相似文献   
944.
945.
946.
947.
Interactions between turbulence, suspended sediment concentration (SSC), settling velocity, effective density, fractal dimension, and floc size were studied on the tide-dominated, muddy coastal shelf of the southwestern Yellow Sea, China. The measurements were carried out in July 2013 at two sites located in water depths of 21.2 and 22.1 m. Negative correlations were observed between shear rate, SSC, effective density, and mean floc size, which supports the results of previous numerical, experimental, and field studies. A significant positive correlation was observed between near-bed SSC and shear rate, an indication that SSC variations are controlled by turbulence and re-suspension. In addition, significant linear relationships were found between settling velocity and other parameters (floc size, turbulence, SSC, effective density, and fractal dimension) at the two sites, indicating that the controlling factors on settling velocity are spatially variable. Principal component analysis was applied to determine the relative importance of turbulence, flocculation ability, and SSC as controls on floc size in situ. The relative contributions of turbulence, flocculation ability, and SSC to floc size (at both sites) were ~33.0%, 30.3%, and 29.7%, respectively, this being a new field-based quantitative analysis of the controls on floc size. The findings demonstrate that, in nature, flocculation ability affects floc size to the same degree as turbulence and SSC. Therefore, predictions of floc size in coastal marine environments require constraints not only on turbulence and SSC, but also on flocculation ability.  相似文献   
948.
949.
Phaeodactylum tricornutum is a potential livestock for the combined production of eicosapentaenoic acid (EPA) and fucoxanthin. In this study, six marine diatom strains identified as P. tricornutum were cultured and their total lipid, fatty acid composition and major photosynthetic pigments determined. It was found that the cell dry weight concentration and mean growth rate ranged between 0.24–0.36 g/L and 0.31–0.33/d, respectively. Among the strains, SCSIO771 presented the highest total lipid content, followed by SCSIO828, and the prominent fatty acids in all strains were C16:0, C16:1, C18:1, and C20:5 (EPA). Polyunsaturated fatty acids, including C16:2, C18:2, and EPA, comprised a significant proportion of the total fatty acids. EPA was markedly high in all strains, with the highest in SCSIO828 at 25.65% of total fatty acids. Fucoxanthin was the most abundant pigment in all strains, with the highest in SCSIO828 as well, at 5.50 mg/g. The collective results suggested that strain SCSIO828 could be considered a good candidate for the concurrent production of EPA and fucoxanthin.  相似文献   
950.
The accurate estimation of evapotranspiration (ET) is essential for assessing water availability and requirements of regional-scale terrestrial ecosystems, and for understanding the hydrological cycle in alpine ecosystems. In this study, two large-scale weighing lysimeters were employed to estimate the magnitude and dynamics of actual evapotranspiration in a humid alpine Kobresia meadow from January 2018 to December 2019 on the northeastern Qinghai-Tibetan Plateau (QTP). The results showed that daily ETa averaged 2.24 ± 0.10 mm day −1 throughout the study period, with values of 3.89 ± 0.14 and 0.81 ± 0.06 mm day−1 during the growing season and non-growing season, respectively. The cumulative ETa during the study period was 937.39 mm, exceeding precipitation (684.20 mm) received at the site during the same period by 37%, suggesting that almost all precipitation in the lysimeters was returned to the atmosphere by evapotranspiration. Furthermore, the cumulative ETa (805.04 mm) was almost equal to the maximum potential evapotranspiration estimated by the FAO-56 reference evapotranspiration (ET0) (801.94 mm) during the growing season, but the cumulative ETa (132.25 mm) was 113.72% less than the minimum equilibrium ETeq) (282.86 mm) during the non-growing season due to the limited surface moisture in frozen soil. The crop coefficient (Kc) also showed a distinct seasonal pattern, with a monthly average of 1.01 during the growing season. Structural equation model (SEM) and boosted regression tree (BRT) show that net radiation and air temperature were the most important factors affecting daily ETa during the whole study period and growing season, but that non-growing season ETa was dominated by soil water content and net radiation. The daily Kc was dominated by net radiation. Furthermore, both ETa and Kc were also affected by aboveground biomass.  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