全文获取类型
收费全文 | 9424篇 |
免费 | 1941篇 |
国内免费 | 2825篇 |
专业分类
测绘学 | 1225篇 |
大气科学 | 2081篇 |
地球物理 | 1952篇 |
地质学 | 4599篇 |
海洋学 | 1546篇 |
天文学 | 299篇 |
综合类 | 1001篇 |
自然地理 | 1487篇 |
出版年
2024年 | 83篇 |
2023年 | 176篇 |
2022年 | 582篇 |
2021年 | 693篇 |
2020年 | 532篇 |
2019年 | 592篇 |
2018年 | 605篇 |
2017年 | 589篇 |
2016年 | 575篇 |
2015年 | 634篇 |
2014年 | 648篇 |
2013年 | 709篇 |
2012年 | 795篇 |
2011年 | 750篇 |
2010年 | 691篇 |
2009年 | 719篇 |
2008年 | 656篇 |
2007年 | 571篇 |
2006年 | 500篇 |
2005年 | 427篇 |
2004年 | 280篇 |
2003年 | 277篇 |
2002年 | 310篇 |
2001年 | 257篇 |
2000年 | 215篇 |
1999年 | 194篇 |
1998年 | 200篇 |
1997年 | 161篇 |
1996年 | 110篇 |
1995年 | 112篇 |
1994年 | 112篇 |
1993年 | 88篇 |
1992年 | 69篇 |
1991年 | 66篇 |
1990年 | 44篇 |
1989年 | 34篇 |
1988年 | 32篇 |
1987年 | 25篇 |
1986年 | 22篇 |
1985年 | 5篇 |
1984年 | 8篇 |
1983年 | 8篇 |
1982年 | 7篇 |
1981年 | 3篇 |
1980年 | 5篇 |
1979年 | 8篇 |
1978年 | 1篇 |
1958年 | 4篇 |
1957年 | 3篇 |
1954年 | 3篇 |
排序方式: 共有10000条查询结果,搜索用时 218 毫秒
991.
Distinct quasi-biweekly features of the subtropical East Asian monsoon during early and late summers 总被引:2,自引:0,他引:2
Jing Yang Qing Bao Bin Wang Dao-Yi Gong Haozhe He Miao-Ni Gao 《Climate Dynamics》2014,42(5-6):1469-1486
Using Global Precipitation Climatology Project daily rainfall and ERA interim reanalysis data, we investigate the distinct characteristic of quasi-biweekly variation (QBV: 12–20 days) over East Asia (EA) during early (June 10–July 20) and late (July 21–August 31) summer. The QBV maximum variance is found over the core region of EA (30°–40°N, 110°–130°E), which includes eastern China (lower reaches of the Yellow, Huaihe, and Yangtze rivers) and the Korean Peninsula. At both its peak wet and dry phases, QBV over the core region has a baroclinic structure, but with different spatial distributions, different lower-level prevalent wind anomalies, and different upper-level major circulation anomalies in the two subseasons. Meanwhile, the two subseasons have different propagating tracks prior to reaching the peak phase, and different precursors associated with the local genesis of QBV. Furthermore, during the transition from the peak dry to peak wet phase of QBV, the major monsoon circulations have different behaviors that tropical monsoon trough extends eastward in early summer but retreats westward in late summer and the South Asia high (SAH) and western North Pacific (WNP) subtropical high move toward (away from) each other in early (late) summer. The abrupt change of mean state in mid to late July, which includes the northward migration of westerly jet, SAH and WNP, and the weakening and broken of westerly jet, is considered the root cause of the change in behavior of QBV. Finally, we indicate that the tropical monsoon trough and midlatitude westerly jet are possible sources of QBV over subtropical EA in both subseasons and provide useful guidance for 2–3 week predictions over EA. 相似文献
992.
Drought variability at the northern fringe of the Asian summer monsoon region over the past millennia 总被引:3,自引:0,他引:3
Bao Yang Shuyuan Kang Fredrik Charpentier Ljungqvist Minhui He Yan Zhao Chun Qin 《Climate Dynamics》2014,43(3-4):845-859
The northern fringe of the Asian summer monsoon region (NASM) in China refers to the most northwestern extent of the Asian summer monsoon. Understanding the characteristics and underlying mechanisms of drought variability at long and short time-scales in the NASM region is of great importance, because present and future water shortages are of great concern. Here, we used newly developed and existing tree-ring, historical documentary and instrumental data available for the region to identify spatial and temporal patterns, and possible mechanisms of drought variability, over the past two millennia. We found that drought variations were roughly consistent in the western (the Qilian Mountains and Hexi Corridor) and eastern (the Great Bend of the Yellow River, referred to as GBYR) parts of the NASM on decadal to centennial timescales. We also identified the spatial extent of typical multi-decadal GBYR drought events based on historical dryness/wetness data and the Monsoon Asia Drought Atlas. It was found that the two periods of drought, in AD 1625–1644 and 1975–1999, exhibited similar patterns: specifically, a wet west and a dry east in the NASM. Spatial characteristics of wetness and dryness were also broadly similar over these two periods, such that when drought occurred in the Karakoram Mountains, western Tianshan Mountains, the Pamirs, Mongolia, most of East Asia, the eastern Himalayas and Southeast Asia, a wet climate dominated in most parts of the Indian subcontinent. We suggest that the warm temperature anomalies in the tropical Pacific might have been mainly responsible for the recent 1975–1999 drought. Possible causes of the drought of 1625–1644 were the combined effects of the weakened Asian summer monsoon and an associated southward shift of the Pacific Intertropical Convergence Zone. These changes occurred due to a combination of Tibetan Plateau cooling together with more general Northern Hemisphere cooling, rather than being solely due to changes in the sea surface temperature of the tropical Pacific. Our results provide a benchmark for comparing and validating paleo-simulations from general circulation model of the variability of the Asian summer monsoon at decadal to centennial timescales. 相似文献
993.
994.
为探究ASTER GDEMV3、SRTM1 DEM和AW3D30 DEM 3种开源DEM数据的高程精度,本文以高精度ICESat-2 ATLAS测高数据为参考数据,利用GIS统计分析、误差相关分析及数理统计对DEM的高程精度进行对比评价。结果表明:①AW3D30的质量最稳定;SRTM1 DEM在平原精度最高;在高原山地精度由高到低依次为AW3D30 DEM、ASTER GDEMV3、SRTM1 DEM。②DEM数据高程精度受地表覆盖影响较大,且与地形因素密切相关,在相同地表覆盖的两个研究区中DEM数据高程精度表现情况不一致,SRTM在平原地表覆盖下精度表现最好,平均误差为3.15 m,AW3D30 DEM在山地地表覆盖下精度表现最好,平均误差为7.61 m。③坡度对DEM数据的高程精度影响较大,在两个研究区3种DEM数据的高程误差均随坡度的增加而增加;坡向对DEM数据的高程精度影响较小,未发现明显的规律。 相似文献
996.
针对当前滑坡稳定性评价方法难以准确获取评价结果的突出问题,本文提出了一种融合地下水、工程地质钻孔信息及灌溉资料等工程地质资料与GNSS观测的黄土滑坡稳定性评价方法。首先,基于高分辨率影像、高精度DEM、地层地貌等多源异构数据,建立滑坡精细三维地质模型体;然后,将滑坡外部高精度GNSS监测数据作为模型外部约束条件,进一步构建起融合工程地质资料与GNSS观测的黄土滑坡稳定性综合评价模型。本文方法能够将滑坡外部大地测量高精度监测数据与工程地质数值模拟手段有机融合,实现了滑坡外部形变信息与内部变形机制的有效耦合。通过我国典型黄土滑坡域甘肃黑方台党川实际发生的两起滑坡失稳事件验证表明,本文方法可有效地提高滑坡稳定性评价结果的精度及可靠性,获取了与试验区域滑坡实际失稳情况相一致的结果:HF06/07 GNSS监测点首先失稳,其次是HF09监测点失稳,最后是HF05监测点失稳。基于本文方法获取的滑坡失稳顺序与实际滑坡发生顺序高度一致,显著优于现有的滑坡失稳数值模拟法。 相似文献
997.
998.
999.
依托珠江流域某冲填土场地工程实例,介绍了真空预压法的施工参数及应用效果,另对“薄弱部位”泥浆搅拌桩密封墙处地层的强度进行了定量分析,结果表明真空预压法适用于此类场地,加固效果明显,但密封墙位置强度降幅较大,需采取换填等措施二次处理后才能使用,可为其他类似工程提供参考经验. 相似文献
1000.
东沙隆起珠江组生物礁是珠江口盆地重要的储层类型,礁灰岩主要为珊瑚藻灰岩,分为骨架岩、粘结岩及障积岩。研究区生物礁发育于开阔台地、台地边缘及台地前缘斜坡3类沉积相中,生物礁类型可分为台内点礁、台地边缘堡礁及台缘斜坡塔礁,以台地边缘堡礁为主。珠江组沉积早期,东沙隆起发育滨岸砂质沉积;中期海水逐渐淹没东沙隆起,形成镶边浅水碳酸盐台地,发育生物礁;晚期海侵台地逐渐淹没消亡,被浅海陆棚泥质沉积代替。流花台地厚度最大,最厚达563m,台地顶面地震强反射使外形轮廓清晰,台地内部中-弱振幅至空白反射,连续性降低;惠州台地厚度较流花台地薄,厚度多大于100m,顶界面强反射轮廓清晰,内部层状反射能量强-中振幅、高-中连续、中-低频,局部空白反射;陆丰台地厚约30m,只有一个高连续的强振幅。生物礁地震响应以丘形、箱型、低丘-透镜状为特征,礁顶常为强振幅,内部为波状、有时见前积结构,翼部可见上超和披覆现象等。 相似文献