全文获取类型
收费全文 | 88篇 |
免费 | 14篇 |
国内免费 | 19篇 |
专业分类
测绘学 | 13篇 |
大气科学 | 16篇 |
地球物理 | 8篇 |
地质学 | 24篇 |
海洋学 | 38篇 |
综合类 | 3篇 |
自然地理 | 19篇 |
出版年
2024年 | 1篇 |
2023年 | 4篇 |
2022年 | 6篇 |
2021年 | 13篇 |
2020年 | 6篇 |
2019年 | 2篇 |
2018年 | 5篇 |
2017年 | 5篇 |
2016年 | 2篇 |
2015年 | 3篇 |
2014年 | 3篇 |
2013年 | 4篇 |
2012年 | 4篇 |
2011年 | 5篇 |
2010年 | 1篇 |
2009年 | 3篇 |
2008年 | 14篇 |
2007年 | 9篇 |
2006年 | 2篇 |
2005年 | 3篇 |
2004年 | 1篇 |
2002年 | 3篇 |
2001年 | 2篇 |
1999年 | 1篇 |
1998年 | 1篇 |
1997年 | 3篇 |
1995年 | 3篇 |
1994年 | 1篇 |
1993年 | 1篇 |
1992年 | 2篇 |
1991年 | 2篇 |
1990年 | 1篇 |
1989年 | 2篇 |
1987年 | 1篇 |
1986年 | 1篇 |
1980年 | 1篇 |
排序方式: 共有121条查询结果,搜索用时 831 毫秒
61.
Vertical variability in the bio-optical properties of seawater in the northern South China Sea(NSCS) including inherent optical properties(IOPs) and chlorophyll a concentration(Chl) were studied on the basis of in situ data collected in summer 2008 using an absorption/attenuation spectrophotometer. An empirical model was developed to estimate Chl profiles based on the absorption line height at long wavelengths, with a relative root mean square error of 37.03%. Bio-optical properties exhibited large horizontal and vertical spatial variability. As influenced by coastal upwelling and the Zhujiang River(Pearl River) discharge, both IOPs and Chl exhibited high values in the surface waters of the inner shelf, which tended to decrease with distance offshore. Subsurface maximum layers of IOPs and Chl were observed in the middle and outer shelf regions, along with significantly higher values of attenuation coefficients beneath this layer that rapidly increased towards the bottom. In the open ocean, both IOPs and Chl exhibited consistent variability, with the subsurface maximum layer typically located at34–84 m. Phytoplankton were found to be one of the major components in determining the vertical variability of bio-optical properties, with their vertical dynamics influenced by both physical forcing and light attenuation effects. The depth of the subsurface maximum layer was found to be closely related to the fluctuation of the oceanic thermocline and the depth of the euphotic zone, which also affected the total integrated biomass of the upper ocean. Typically high values of attenuation coefficients observed in the bottom waters of the continental shelf reflected the transport of particulate matter over the bottom boundary layer. Our results reveal large spatial differences in bio-optical profiles in response to complex marine ecodynamics in the NSCS. From the perspective of marine research, high-resolution optical measurements are clearly advantageous over conventional bottle sampling. 相似文献
62.
为了研究河南省植被指数变化特征,采用最大值合成法(MVC)对MODIS-NDVI和MODIS-EVI两种指数产品进行处理,然后进行时空变化分析,得到归一化植被指数(NDVI)与增强型植被指数(EVI)两种指数产品的特点,实验结果表明:1)在时间分布特征上,两种植被指数均随季节呈现规律性变化,并且最大值均出现在7月或8月,但EVI相比NDVI更具季节性规律,能够更好地反映高植被覆盖区的植被季节性变化特征;2)在空间分布特征上,两种植被指数的区域性都非常明显,但在高植被覆盖区,NDVI出现饱和现象,而EVI未出现饱和现象。 相似文献
63.
Upwelling occurs on the coast of Java between June and October, forced by local alongshore winds associated with the southeasterly monsoon. This causes variations in phytoplankton community composition in the upwelling zone compared with the surrounding offshore area. Based on pigments analysis with subsequent calculations of group contributions to total chlorophyll a(Chl a) using CHEMTAX, we studied the distribution and composition of phytoplankton assemblages in the subsurface chlorophyll maximum along the south coast of Java and the influence of upwelling. Nineteen phytoplankton pigments were identified using high-performance liquid chromatography, and CHEMTAX analysis associated these to ten major phytoplankton groups. The phytoplankton community in the coastal area influenced by upwelling was characterized by high Chl a and fucoxanthin concentrations, indicating the dominance of diatoms. In contrast, in the offshore area, the Chl a and fucoxanthin concentrations declined to very low levels and the community was dominated by haptophytes represented by 19′-Hexanoyloxyfucoxanthin. Accordingly, microphytoplankton was found to be the major size class in the coastal area influenced by upwelling, while nanophytoplankton was most abundant in the offshore area. Low concentrations of other accessory pigments indicated less contribution from dinoflagellates,prasinophytes, chlorophytes and cryptophytes. Photo-pigment indices revealed that photosynthetic carotenoids(PSCs) were the largest component of the pigment pool, exceeding the proportion of Chl a, with the average PSCTP up to 0.62. These distribution trends can mainly be explained by phytoplankton adaption strategies to upwelling and subsurface conditions by changing species composition and adjusting the pigment pool. 相似文献
64.
图像配准是将不同时期、不同视点或从不同传感器获得的同一地域目标的图像对准的过程[1-5],其主要目的是消除或减少参考图像和待配准图像之间由于成像条件不同所引起的几何形变,从而获得具有几何一致性的两幅图像。本文针对基于灰度图像配准算法中传统的梯度配准法执行效率低的 相似文献
65.
66.
根据黄浦江百余年潮位资料分析,存在较显著的准周期性,从而提出周期最大值法。首先通过周期分析,选择基本周期步长;然后由周期单元取样,按照周期最大值的随机性,结合历史调查特大值,进行频率分析。因此,这些极值变量,均是近于或属于严重风暴潮条件,则外延稀遇频率的设计潮位成果,较为合理可靠,可供大中型水利水电工程设计研究参考。 相似文献
67.
各地正午太阳高度的最大值与最小值,存在着以一年为周期的变化。其分布又随地点和时间体现出不同的差异性;还存在着明显的规律性。 相似文献
68.
69.
中南半岛地区夏季降水日变化特征 总被引:4,自引:0,他引:4
利用TRMM(Tropical Rainfall Measuring Mission)3B42RT和3G68 PR 1998-2005年8 a的观测资料,研究了中南半岛地区夏季(6-8月)降水日变化特征.结果表明:整个夏季,中南半岛西侧沿海和长山山脉西侧迎风坡为降水大值区和降水日方差大值区.陆地上平原地区和远海海面降水主要出现在16-19LST(local standard time);沿海海面在07-10LST达到降水最大值.降水在白天由沿海分别向内陆和远海海面传播;夜间,降水从远海海面向沿海地区回传,但没有发现内陆向沿海地区回传.长山山脉西侧迎风坡的一南一北两个区域,表现出明显不同的降水日变化特征,其原因与降水的传播有关.01-04LST,降水大值区出现在泰国湾东部沿海,并向中南半岛岛内传播,16-19LST在长山山脉西南侧形成降水大值区,之后降水进一步沿山脉向西北传播,并于次日01-04LST传到长山山脉西北侧区域,通过降水的这种传播特征从而导致长山山脉迎风坡一侧不同的降水日变化特征. 相似文献
70.
目前,针对利用无人机技术在山地起伏大、山体植被密集区域,难以获取地面点及DEM等问题,本文提出了一种结合布料模拟算法和改进的局部最大值算法,利用树顶点、树高等植被信息,提取地面点,进而生成整个区域的DEM的方法。以中国传统村落德夯村为例,利用植被系数和高程信息将点云分割为植被密集区和非植被密集区两个部分。在非植被密集区,通过布料模拟算法和改进的局部最大值算法分别提取地面点和树顶点,计算平均树高;在植被密集区,通过该区域的树顶点推算得到植被密集区的近似地面点,最终将两部分的地面点云进行TIN插值得到该地区的DEM。试验结果表明,利用此方法生成的DEM均方根误差,在非植被密集区达0.037 m,植被密集区可达1.606 m,整体平均误差达1.492 m,总体精度较好,基本可以满足村落尺度空间分析的需求。 相似文献