全文获取类型
收费全文 | 1465篇 |
免费 | 252篇 |
国内免费 | 519篇 |
专业分类
测绘学 | 300篇 |
大气科学 | 453篇 |
地球物理 | 144篇 |
地质学 | 731篇 |
海洋学 | 209篇 |
天文学 | 11篇 |
综合类 | 135篇 |
自然地理 | 253篇 |
出版年
2024年 | 3篇 |
2023年 | 24篇 |
2022年 | 66篇 |
2021年 | 76篇 |
2020年 | 79篇 |
2019年 | 89篇 |
2018年 | 77篇 |
2017年 | 95篇 |
2016年 | 84篇 |
2015年 | 96篇 |
2014年 | 121篇 |
2013年 | 140篇 |
2012年 | 104篇 |
2011年 | 93篇 |
2010年 | 88篇 |
2009年 | 97篇 |
2008年 | 84篇 |
2007年 | 91篇 |
2006年 | 111篇 |
2005年 | 85篇 |
2004年 | 82篇 |
2003年 | 47篇 |
2002年 | 54篇 |
2001年 | 52篇 |
2000年 | 42篇 |
1999年 | 33篇 |
1998年 | 34篇 |
1997年 | 49篇 |
1996年 | 31篇 |
1995年 | 15篇 |
1994年 | 21篇 |
1993年 | 12篇 |
1992年 | 14篇 |
1991年 | 8篇 |
1990年 | 6篇 |
1989年 | 6篇 |
1988年 | 8篇 |
1987年 | 5篇 |
1986年 | 4篇 |
1985年 | 3篇 |
1984年 | 3篇 |
1982年 | 2篇 |
1979年 | 1篇 |
1977年 | 1篇 |
排序方式: 共有2236条查询结果,搜索用时 109 毫秒
941.
942.
为探究江西省北部茶区春霜冻发生特点,深入开展茶叶春霜冻灾害定量评估工作,采用实地调查方式,获取江西省北部12个茶场2018年4月7—9日春霜冻的灾情资料和同期气象观测资料,采用加权求和法构建茶叶春霜冻灾害损失定量评估模型,对春霜冻灾害县进行灾害定量评估和检验。结果表明:婺源、浮梁等江西省北部茶叶主产县达到轻—重度春霜冻气象灾害等级,灾害指标等级计算结果与实地灾情调查结果较一致;轻度、中度、重度气象灾害等级的茶场减产率依次为10%—30%、30%—50%和50%以上;根据不同气象灾害等级的受灾面积及其减产率构建江西省北部茶叶春霜冻灾害损失定量评估模型,计算得到此次春霜冻灾害过程造成婺源县春茶直接经济损失为1.23亿元,模型评估结果和实际灾情相一致,模型能较为客观、准确的评估春霜冻灾害对茶叶生产造成的损失。 相似文献
943.
Barnaby Clark Juha Suomalainen Petri Pellikka 《International Journal of Applied Earth Observation and Geoinformation》2011
SPOT satellites have been imaging Earth's surface since SPOT 1 was launched in 1986. It is argued that absolute atmospheric correction is a prerequisite for quantitative remote sensing. Areas where land cover changes are occurring rapidly are also often areas most lacking in situ data which would allow full use of radiative transfer models for reflectance factor retrieval (RFR). Consequently, this study details the proposed historical empirical line method (HELM) for RFR from multi-temporal SPOT imagery. HELM is designed for use in landscape level studies in circumstances where no detailed overpass concurrent atmospheric or meteorological data are available, but where there is field access to the research site(s) and a goniometer or spectrometer is available. SPOT data are complicated by the ±27° off-nadir cross track viewing. Calibration to nadir only surface reflectance factor (ρs) is denoted as HELM-1, whilst calibration to ρs modelling imagery illumination and view geometries is termed HELM-2. Comparisons of field measured ρs with those derived from HELM corrected SPOT imagery, covering Helsinki, Finland, and Taita Hills, Kenya, indicated HELM-1 RFR absolute accuracy was ±0.02ρs in the visible and near infrared (VIS/NIR) bands and ±0.03ρs in the shortwave infrared (SWIR), whilst HELM-2 performance was ±0.03ρs in the VIS/NIR and ±0.04ρs in the SWIR. This represented band specific relative errors of 10–15%. HELM-1 and HELM-2 RFR were significantly better than at-satellite reflectance (ρSAT), indicating HELM was effective in reducing atmospheric effects. However, neither HELM approach reduced variability in mean ρs between multi-temporal images, compared to ρSAT. HELM-1 calibration error is dependent on surface characteristics and scene illumination and view geometry. Based on multiangular ρs measurements of vegetation-free ground targets, calibration error was negligible in the forward scattering direction, even at maximum off-nadir view. However, error exceeds 0.02ρs where off-nadir viewing was ≥20° in the backscattering direction within ±55° azimuth of the principal plane. Overall, HELM-1 results were commensurate with an identified VIS/NIR 0.02ρs accuracy benchmark. HELM thus increases applicability of SPOT data to quantitative remote sensing studies. 相似文献
944.
945.
946.
947.
948.
单多普勒雷达反演热带气旋近中心风场的VAP扩展应用方法 总被引:3,自引:3,他引:0
在尝试运用VAP方法和扩展VAP(EVAP)方法,对"韦帕"台风期间移动天气雷达(CINRAD/CCJ)观测基数据进行单雷达风场反演时,发现部分区域出现风向、风速不合理的情况.分析认为,在热带气旋近中心区域风向风速变化均较剧烈,而上述两种算法的假定条件难以准确代表风场的实际变化.根据热带气旋发展成熟阶段的气旋环流近似轴对称的特点,文中提出一种新的假定条件,即在与热带气旋中心等距离的圆周上局地风速不变、风向均匀变化,对VAP方法进行扩展应用,称为EVAPTC(EVAP for Tropical Cyclone)方法.对理想模型流场试验及对实际个例的反演结果表明,EVAPTC方法简便,反演误差相对较小,能够基本反映出台风近中心的环流特点,尤其是螺旋云带上的风场特征.例如"韦帕"台风螺旋云带内侧有明显的辐合气流进入螺旋云带,螺旋云带尾部的外围气流绕着云体移动,螺旋云带上的强回波区存在着风场扰动等. 相似文献
949.
The mobile incoherent Doppler lidar(MIDL),which was jointly developed by State Key Laboratory of Severe Weather(LaSW) of the Chinese Academy of Meteorological Sciences(CAMS) and Ocean University of China,provided meteorological services during the Olympic sailing events in Qingdao in 2008.In this study,two experiments were performed based on these measurements.First,the capabilities of MIDL detection of sea-surface winds were investigated by comparing its radial velocities with those from a sea buoy.MIDL radial velocity was almost consistent with sea-buoy data;both reflected the changes in wind with time.However,the MIDL data was 0.5 m s 1 lower on average than the sea-buoy data due to differences in detection principle,sample volume,sample interval,spatial and temporal resolution.Second,the wind fields during the Olympic sailing events were calculated using a four-dimensional variation data assimilation(4DVAR) algorithm and were evaluated by comparing them with data from a sea buoy.The results show that the calculations made with the 4DVAR wind retrieval method are able to simulate the fine retrieval of sea-surface wind data-the retrieved wind fields were consistent with those of sea-buoy data.Overall,the correlation coefficient of wind direction was 0.93,and the correlation coefficient of wind speed was 0.70.The distribution of retrieval wind fields was consistent with that of MIDL radial velocity;the root-mean-square error between them had an average of only 1.52 m s 1. 相似文献
950.
人工神经网络法反演晴空大气湿度廓线的研究 总被引:4,自引:0,他引:4
高光谱分辨率大气红外探测器AIRS(Atmospheric Infrared Sounder)作为第一个超高光谱大气红外探测仪,开辟了卫星大气探测的新时代.以无线电探空值与SARTA(Stand-Alone Radiative Transfer Algorithm辐射传输模式)v1.05版的前向模式模拟出的AIRS辐射... 相似文献