全文获取类型
收费全文 | 493篇 |
免费 | 182篇 |
国内免费 | 513篇 |
专业分类
测绘学 | 11篇 |
大气科学 | 772篇 |
地球物理 | 67篇 |
地质学 | 29篇 |
海洋学 | 266篇 |
天文学 | 2篇 |
综合类 | 21篇 |
自然地理 | 20篇 |
出版年
2024年 | 8篇 |
2023年 | 16篇 |
2022年 | 39篇 |
2021年 | 30篇 |
2020年 | 54篇 |
2019年 | 41篇 |
2018年 | 47篇 |
2017年 | 40篇 |
2016年 | 36篇 |
2015年 | 25篇 |
2014年 | 53篇 |
2013年 | 71篇 |
2012年 | 52篇 |
2011年 | 43篇 |
2010年 | 42篇 |
2009年 | 40篇 |
2008年 | 58篇 |
2007年 | 68篇 |
2006年 | 54篇 |
2005年 | 61篇 |
2004年 | 48篇 |
2003年 | 40篇 |
2002年 | 37篇 |
2001年 | 26篇 |
2000年 | 23篇 |
1999年 | 26篇 |
1998年 | 28篇 |
1997年 | 12篇 |
1996年 | 9篇 |
1995年 | 20篇 |
1994年 | 9篇 |
1993年 | 11篇 |
1992年 | 10篇 |
1991年 | 5篇 |
1990年 | 1篇 |
1987年 | 2篇 |
1986年 | 1篇 |
1985年 | 1篇 |
1980年 | 1篇 |
排序方式: 共有1188条查询结果,搜索用时 140 毫秒
61.
利用高空资料、地面资料和红外卫星云图资料,对发生在浙江中北部的9012台风倒槽暴雨的机制进行分析,揭示了该台风倒槽的结构和暴雨的环境场。并进一步研究了产生暴雨的中尺度暴雨云团及其周围的垂直气流分布与地面降水的对应关系。对暴雨云团所对应的高、中、低(地面)层系统亦进行了分析。 相似文献
62.
徐文金 《南京气象学院学报》1995,18(2):242-247
分析了8807号台风所引发的局地特大暴雨成因:(1)台风提供了足够的水汽;(2)台风螺旋状云雨区和太阳辐射不均匀,形成了低层中尺度锋区,为暴雨发生提供极不稳定能量和触发条件;(3)局地地形和摩擦因子使湖北省宜昌地区成为这次对流云发展较有利的地点;(4)高空的中尺度降压系统和涡度因子加强了对流云团的发展。 相似文献
63.
A case of mesoscale convective complex(MCC)which evolved into a vortex is documented in this paper.As theMCC entered into the dissipating phase,a well-defined spirally banded structure became visible in the satellite image.The blackbody temperature(TBB)of the residual cold-cloud-shield indicates the vortex existed in the layer from 400 to250 hPa.According to the upper air analysis,the upper level vortex was an anticyclone.The MCC-generated vortex wasvisualized in the satellite images because it was located in the subtropical high where the wind field was very weak. 相似文献
64.
使用气象卫星资料,分析了1989年7月发生在四川东部的4个中尺度对流系统的特征,第一个系统是由3个对流云团合并而成,生成后快速向前移动,第二个为向后传播。第三个系统生成后,系统的西南部不断生成新的对流单体,使之维持准静止状态,最后一个系统的初期呈胞状结构,后与冷锋结合,成为冷锋云系的一部分,这4个系统都是西南低涡暖切变形势下的产物,随着形势演变,其大尺度环境略有差异。 相似文献
65.
东北地区中尺度对流复合体的卫星云图特征 总被引:5,自引:0,他引:5
通过10年(1983-1992年)卫星云图资料的分析,综合归纳了东北地区中尺度对流复合体(NMCC)的基本特征及其发展演变过程,由于受地理条件的影响,NMCC与美国大平原以及我国西北和华北平原上的MCC有明显差别,作为一类特殊的对流性天气系统,NMCC与一般中尺度对流云图特征有明显差异。 相似文献
66.
Tao Zuyu Wang Hongqing Bai Jie Zhu Wenqin Shi Dingpu Yang Hongmei 《Acta Meteorologica Sinica》1995,9(2):184-189
A case of mesoscale convective complex(MCC) which evolved into a vortex is documented in this paper.As the MCC entered into the dissipating phase,a well-defined spirally banded structure became visible in the satellite image.The blackbody temperature(TBB) of the residual cold-cloud-shield indicates the vortex existed in the layer from 400 to 250 hPa.According to the upper air analysis,the upper level vortex was an anticyclone.The MCC-generated vortex was visualized in the satellite images because it was located in the subtropical high where the wind field was very weak. 相似文献
67.
Hydrodynamical Modeling Of Oceanic Vortices 总被引:1,自引:0,他引:1
Xavier Carton 《Surveys in Geophysics》2001,22(3):179-263
Mesoscale coherent vortices are numerous in the ocean.Though they possess various structures in temperature and salinity,they are all long-lived, fairly intense and mostly circular. Thephysical variable which best describes the rotation and the density anomaly associated with coherent vortices is potential vorticity. It is diagnostically related to velocity and pressure, when the vortex is stationary. Stationary vortices can be monopolar (circular or elliptical) or multipolar; their stability analysis shows thattransitions between the various stationary shapes are possible when they become unstable. But stable vortices can also undergo unsteady evolutions when perturbed by environmental effects, likelarge-scale shear or strain fields, -effect or topography. Changes in vortex shapes can also result from vortex interactions. such as the pairing, merger or vertical alignment of two vortices, which depend on their relative polarities and depths. Such interactions transfer energy and enstrophy between scales, and are essential in two-dimensional and in geostrophic turbulence. Finally, in relation with the observations, we describe a few mechanisms of vortex generation. 相似文献
68.
S. Abhilash Someshwar Das S. R. Kalsi M. Das Gupta K. Mohankumar John P. George S. K. Banerjee S. B. Thampi D. Pradhan 《Pure and Applied Geophysics》2007,164(8-9):1491-1509
Pre-monsoon rainfall around Kolkata (northeastern part of India) is mostly of convective origin as 80% of the seasonal rainfall
is produced by Mesoscale Convective Systems (MCS). Accurate prediction of the intensity and structure of these convective
cloud clusters becomes challenging, mostly because the convective clouds within these clusters are short lived and the inaccuracy
in the models initial state to represent the mesoscale details of the true atmospheric state. Besides the role in observing
the internal structure of the precipitating systems, Doppler Weather Radar (DWR) provides an important data source for mesoscale
and microscale weather analysis and forecasting. An attempt has been made to initialize the storm-scale numerical model using
retrieved wind fields from single Doppler radar. In the present study, Doppler wind velocities from the Kolkata Doppler weather
radar are assimilated into a mesoscale model, MM5 model using the three-dimensional variational data assimilation (3DVAR)
system for the prediction of intense convective events that occurred during 0600 UTC on 5 May and 0000 UTC on 7 May, 2005.
In order to evaluate the impact of the DWR wind data in simulating these severe storms, three experiments were carried out.
The results show that assimilation of Doppler radar wind data has a positive impact on the prediction of intensity, organization
and propagation of rain bands associated with these mesoscale convective systems. The assimilation system has to be modified
further to incorporate the radar reflectivity data so that simulation of the microphysical and thermodynamic structure of
these convective storms can be improved. 相似文献
69.
An Experiment Using the High Resolution Eta and WRF Models to Forecast Heavy Precipitation over India 总被引:1,自引:0,他引:1
Y. V. Rama Rao H. R. Hatwar Ahmad Kamal Salah Y. Sudhakar 《Pure and Applied Geophysics》2007,164(8-9):1593-1615
In the present study using the Weather Research and Forecasting (WRF) and Eta models, recent heavy rainfall events that occurred
(i) over parts of Maharastra during 26 to 27 July, 2005, (ii) over coastal Tamilnadu and south coastal Andhra Pradesh during
24 to 28 October, 2005, and (iii) the tropical cyclone of 30 September to 3 October, 2004/Monsoon Depression of 2 to 5 October
2004, that developed during the withdrawal phase of the southwest monsoon season of 2004 have been investigated. Also sensitivity
experiments have been conducted with the WRF model to test the impact of microphysical and cumulus parameterization schemes
in capturing the extreme weather events. The results show that the WRF model with the microphysical process and cumulus parameterization
schemes of Ferrier et al. and Betts-Miller-Janjic was able to capture the heavy rainfall events better than the other schemes. It is also observed
that the WRF model was able to predict mesoscale rainfall more realistically in comparison to the Eta model of the same resolution. 相似文献
70.
大气中对称不稳定机制的动力学分析及暴雨的分析与预报 总被引:1,自引:0,他引:1
用气块法从力学角度对对称不稳定机制及在对称不稳定条件下产生的环流进行分析,更全面地定义了对称不稳定及它的产生机制和中尺度环流形成的过程。对暴雨个例诊断分析表明,有些强降水区在降水前和降水过程中存在着不对称不稳定,说明对称不稳定条件下形成的环流对暴雨有引发和加强作用。在以往研究原基础上,总结出了利用常规观测资料分析对称不是否存在,及其能量大小的方法,用它来预报是否降水及降水的强度,从而提高降水预报准确率。 相似文献