全文获取类型
收费全文 | 3431篇 |
免费 | 1050篇 |
国内免费 | 1340篇 |
专业分类
测绘学 | 583篇 |
大气科学 | 481篇 |
地球物理 | 766篇 |
地质学 | 2478篇 |
海洋学 | 697篇 |
天文学 | 27篇 |
综合类 | 309篇 |
自然地理 | 480篇 |
出版年
2024年 | 30篇 |
2023年 | 75篇 |
2022年 | 247篇 |
2021年 | 281篇 |
2020年 | 184篇 |
2019年 | 275篇 |
2018年 | 209篇 |
2017年 | 224篇 |
2016年 | 210篇 |
2015年 | 251篇 |
2014年 | 225篇 |
2013年 | 348篇 |
2012年 | 322篇 |
2011年 | 303篇 |
2010年 | 317篇 |
2009年 | 309篇 |
2008年 | 316篇 |
2007年 | 320篇 |
2006年 | 299篇 |
2005年 | 271篇 |
2004年 | 190篇 |
2003年 | 126篇 |
2002年 | 144篇 |
2001年 | 118篇 |
2000年 | 76篇 |
1999年 | 53篇 |
1998年 | 15篇 |
1997年 | 8篇 |
1996年 | 5篇 |
1995年 | 4篇 |
1994年 | 4篇 |
1993年 | 3篇 |
1992年 | 7篇 |
1991年 | 5篇 |
1990年 | 7篇 |
1988年 | 3篇 |
1987年 | 3篇 |
1986年 | 3篇 |
1979年 | 2篇 |
1976年 | 1篇 |
1974年 | 1篇 |
1973年 | 2篇 |
1965年 | 1篇 |
1957年 | 2篇 |
1954年 | 6篇 |
1949年 | 1篇 |
1944年 | 2篇 |
1937年 | 4篇 |
1934年 | 1篇 |
1933年 | 3篇 |
排序方式: 共有5821条查询结果,搜索用时 15 毫秒
991.
992.
以上海市为例,探索中国新型自主的FY-3A/MERSI数据在典型大城市热环境研究中的应用模式,包括实时监测与同化数值预报两个方面。结果表明:FY-3A/MERSI反演的250 m地表温度及其他衍生指标能够客观呈现城市热场格局及热岛效应,精细揭示出上海市区—近郊—远郊的地温明显分异,热岛由中心城区呈放射性面状过渡到远郊以乡镇为中心的团块状,其形成与下垫面介质关系密切。同化FY-3A/MERSI数据产品的中尺度数值模式,耦合城市冠层参数化方案,可实现250 m格网0~48 h城市近地层气温空间精细化预报,提取1 h间隔的热环境日演变特征将有助于在不同天气形式下进行热环境灾害潜式预报及机理分析。预报结果在时空分辨率方面明显优于常规数值预报,并避免了卫星云污染的影响,说明FY-3A卫星探测资料能有效改善模式背景场与初始场。 相似文献
993.
994.
995.
996.
应用VAN法、波形分析法、潮汐谐波分析等对华北地区观测资料质量较好的地电场台进行研究,结果表明,华北地区地电场波形日变幅度范围为2.35—11.12 mV/km;VAN法在华北地区有一定的震例对应,如2003年5月22日河北唐山ML 4.1、2006年7月4日河北文安ML 5.1、2010年3月6日河北滦县ML 4.7... 相似文献
997.
To analyze the effects of gas cannons on clouds and precipitation, multisource observational data, including those from National Centers for Environmental Prediction (NCEP) reanalysis, Hangzhou and Huzhou new-generation weather radars, laser disdrometer, ground-based automatic weather station, wind profiler radar, and Lin''an C-band dual polarization radar, were adopted in this study. Based on the variational dual-Doppler wind retrieval method and the polarimetric variables obtained by the dual-polarization radar, we analyzed the microphysical processes and the variations in the macro - and microphysical quantities in clouds from the perspective of the synoptic background before precipitation enhancement, the polarization echo characteristics before, during and after enhancement, and the evolution of the fine three-dimensional kinematic structure and the microphysical structure. The results show that the precipitation enhancement operation promoted the development of radar echoes and prolonged their duration, and both the horizontal and vertical wind speeds increased. The dual-polarization radar echo showed that the diameter of the precipitation particles increased, and the concentration of raindrops increased after precipitation enhancement. The raindrops were lifted to a height corresponding to 0 to -20 ℃ due to vertical updrafts. Based on the disdrometer data during precipitation enhancement, the concentration of small raindrops (lgNw) showed a significant increase, and the mass-weighted diameter Dm value decreased, indicating that the precipitation enhancement operation played a certain“lubricating”effect. After the precipitation enhancement, the concentration of raindrops did not change much compared with that during the enhancement process, while the Dm increased, corresponding to an increase in rain intensity. The results suggest the positive effect of gas cannons on precipitation enhancement. 相似文献
998.
2022年春季(3—5月)北半球极涡呈单极型分布,形状狭长,极涡强度与历史同期相当。北半球中高纬度西风带呈4波型分布。3月,我国北方的大部分地区及北部海域受西北气流控制;4月,东亚大槽加深,高压脊区较历史同期偏强;5月,中高纬环流调整为“两槽两脊”型。我国近海出现12次大风过程,其中冷空气大风过程4次,冷空气和温带气旋共同影响的大风过程3次,温带气旋大风过程4次,冷空气与热带气旋共同影响的大风过程1次。近海共出现10次比较明显的海雾过程,其中3月4次,4月3次,5月3次。西北太平洋和南海有2个热带气旋生成,接近常年同期平均值;全球其他海域有12个热带气旋生成,较历史同期平均值偏少5.7个。近海浪高2.0 m以上的海浪过程有12次,总日数为44 d。春季各月我国近海海面温度整体呈上升趋势,北方海域升温幅度大于南方海域。 相似文献
999.
Haze pollution in early winter(December and January) in the Yangtze River Delta(YRD) and in North China(NC)are both severe;however, their monthly variations are significantly different. In this study, the dominant large-scale atmospheric circulations and local meteorological conditions were investigated and compared over the YRD and NC in each month. Results showed that the YRD(NC) is dominated by the so-called Scandinavia(East Atlantic/West Russia)pattern in December, and these circulations weaken in January. The East Asian December and January monsoons over the YRD and NC have negative correlations with the number of haze days. The local descending motion facilitates less removal of haze pollution over the YRD, while the local ascending motion facilitates less removal of haze pollution over NC in January, despite a weaker relationship in December. Additionally, the monthly variations of atmospheric circulations showed that adverse meteorological conditions restrict the vertical(horizontal) dispersion of haze pollution in December(January) over the YRD, while the associated local weather conditions are similar in these two months over NC. 相似文献
1000.
The seasonal and diurnal variations of cloud systems are profoundly affected by the large-scale and local environments. In this study, a one-year-long simulation was conducted using a two-dimensional cloud-resolving model over the Eastern Tibetan Plateau (ETP) and two subregions of Eastern China: Southern East China and Central East China. Deep convective clouds (DCCs) rarely occur in the cold season over ETP, whereas DCCs appear in Eastern China throughout the year, and the ETP DCCs are approximately 20%?30% shallower than those over Eastern China. Most strong rainfall events (precipitation intensity, PI> 2.5 mm h?1) in Eastern China are related to warm-season DCCs with ice cloud processes. Because of the high elevation of the ETP, the warm-season freezing level is lower than in Eastern China, providing favorable conditions for ice cloud processes. DCCs are responsible for the diurnal variations of warm-season rainfall in all three regions. Warm-season DCCs over the ETP have the greatest total cloud water content and frequency in the afternoon, resulting in an afternoon rainfall peak. In addition, rainfall events in the ETP also exhibit a nocturnal peak in spring, summer, and autumn due to DCCs. Strong surface heat fluxes around noon can trigger or promote DCCs in spring, summer, and autumn over the ETP but produce only cumulus clouds in winter due to the cold and dry environment. 相似文献