全文获取类型
收费全文 | 1766篇 |
免费 | 386篇 |
国内免费 | 707篇 |
专业分类
测绘学 | 22篇 |
大气科学 | 921篇 |
地球物理 | 477篇 |
地质学 | 434篇 |
海洋学 | 592篇 |
天文学 | 57篇 |
综合类 | 88篇 |
自然地理 | 268篇 |
出版年
2024年 | 8篇 |
2023年 | 27篇 |
2022年 | 58篇 |
2021年 | 74篇 |
2020年 | 74篇 |
2019年 | 73篇 |
2018年 | 75篇 |
2017年 | 83篇 |
2016年 | 85篇 |
2015年 | 94篇 |
2014年 | 130篇 |
2013年 | 122篇 |
2012年 | 137篇 |
2011年 | 132篇 |
2010年 | 100篇 |
2009年 | 155篇 |
2008年 | 152篇 |
2007年 | 180篇 |
2006年 | 154篇 |
2005年 | 111篇 |
2004年 | 118篇 |
2003年 | 100篇 |
2002年 | 92篇 |
2001年 | 78篇 |
2000年 | 68篇 |
1999年 | 54篇 |
1998年 | 53篇 |
1997年 | 53篇 |
1996年 | 50篇 |
1995年 | 44篇 |
1994年 | 39篇 |
1993年 | 21篇 |
1992年 | 13篇 |
1991年 | 7篇 |
1990年 | 12篇 |
1989年 | 6篇 |
1988年 | 14篇 |
1987年 | 4篇 |
1986年 | 3篇 |
1985年 | 2篇 |
1983年 | 1篇 |
1980年 | 2篇 |
1978年 | 1篇 |
排序方式: 共有2859条查询结果,搜索用时 15 毫秒
991.
992.
为了评估安徽省寿县国家气候观象台新增的近地层通量观测系统业务运行状况,利用2007年9月—2008年8月寿县近地层通量系统观测资料,分析了农田下垫面能量平衡情况。结果表明:全年能量平衡比率平均为0.89,但不同条件下存在差异:白天明显大于夜间,春、夏、秋季明显大于冬季,裸地和麦、稻田明显大于雪地,晴、昙、阴、雨天气情况下差异不大。总体来说,能量不平衡是通量观测中较为普遍的现象,一般认为不平衡程度在10%~30%为合理范围,寿县国家气候观象台全年的能量不平衡程度 (11%) 恰好属于这个范围,并接近不平衡程度的下限,说明涡度相关法在淮河流域农田生态系统通量观测中可靠性较高。 相似文献
993.
994.
995.
996.
997.
Patrick Martin Richard S. LampittMary Jane Perry Richard SandersCraig Lee Eric D'Asaro 《Deep Sea Research Part I: Oceanographic Research Papers》2011,58(4):338-349
Spring diatom blooms are important for sequestering atmospheric CO2 below the permanent thermocline in the form of particulate organic carbon (POC). We measured downward POC flux during a sub-polar North Atlantic spring bloom at 100 m using thorium-234 (234Th) disequilibria, and below 100 m using neutrally buoyant drifting sediment traps. The cruise followed a Lagrangian float, and a pronounced diatom bloom occurred in a 600 km2 area around the float. Particle flux was low during the first three weeks of the bloom, between 10 and 30 mg POC m−2 d−1. Then, nearly 20 days after the bloom had started, export as diagnosed from 234Th rose to 360-620 mg POC m−2 d−1, co-incident with silicate depletion in the surface mixed layer. Sediment traps at 600 and 750 m depth collected 160 and 150 mg POC m−2 d−1, with a settled volume of particles of 1000-1500 mL m−2 d−1. This implies that 25-43% of the 100 m POC export sank below 750 m. The sinking particles were ungrazed diatom aggregates that contained transparent exopolymer particles (TEP). We conclude that diatom blooms can lead to substantial particle export that is transferred efficiently through the mesopelagic. We also present an improved method of calibrating the Alcian Blue solution against Gum Xanthan for TEP measurements. 相似文献
998.
为了更准确地计算由平台晃动所带来的通量观测误差, 从平台晃动与风速仪测点位置变化角度以分层平均消除垂向均值差异的办法建立了新的涡相关通量误差矫正模型。结果是: 在中高海况下由平台晃动引起的通量观测误差是显著的。有鉴于此, 将晃动平台视为固定平台来处理的常用通量计算公式在中高海况下可能会给出严重失真的结果, 建议采用新公... 相似文献
999.
NCEP再分析资料和浮标观测资料计算海气热通量的比较 总被引:1,自引:0,他引:1
对来自于美国国家环境预报中心公布的NCEP1、NCEP2 再分析资料和来自于定点布放在黄海北部的浮标观测资料进行了比较和分析。结果是: NCEP 再分析资料中的海表气象参数(风速、湿度、气温、海表温度)是可信的。在统计意义上, NCEP2 给出的海表气象参数比NCEP1 与浮标观测值更接近,而净辐射通量则是NCEP1 ... 相似文献
1000.
To investigate the values of 10-m drag coefficient (CD) in different coastal areas under the influence of tropical cyclones, the present study used the observational data from four towers in different coastal areas of the South China Sea (SCS) during six tropical cyclone (TC) passages, and employed the eddy covariance method and the flux profile method. The analysis of footprint showed that the fluxes at Zhizai Island (ZZI), Sanjiao Island (SJI) and Donghai Island (DHI) were influenced basically by the ocean, and the flux at Shangyang Town (SYT) was influenced mainly by the land. The results showed that the dependence relationships of CD on 10-m wind speed (U10) in four different coastal areas under the influence of TCs were different. CD at ZZI and SJI initially increased and then decreased as U10 increased, similar to the pattern over the ocean. CD at ZZI and SJI represented the values over shallow water with seawater depths of ~7 m and ~2 m, respectively. Moreover, the critical wind speed at which CD peaked gradually decreased as the seawater depth became shallower in the coastal areas. CD at DHI and SYT decreased monotonously as U10 increased, similar to the pattern over the land. CD at DHI represented the value over the transition zone from shallow water to coastal land, and CD at SYT represented the value over the coastal land. Meanwhile, the eddy covariance method and the flux profile method were compared at ZZI and SYT during TC passages. It was found that their CD values obtained by the two methods were close. Finally, the parameterizations of observed u* and CD as a function of U10 over four different coastal areas were given under the influence of high winds. These parameterizations of observed C may be used in high-resolution numerical models for landfalling TC forecast. 相似文献