全文获取类型
收费全文 | 111篇 |
免费 | 38篇 |
国内免费 | 68篇 |
专业分类
大气科学 | 167篇 |
地球物理 | 19篇 |
地质学 | 10篇 |
海洋学 | 17篇 |
自然地理 | 4篇 |
出版年
2024年 | 2篇 |
2023年 | 3篇 |
2022年 | 5篇 |
2021年 | 6篇 |
2020年 | 13篇 |
2019年 | 10篇 |
2018年 | 4篇 |
2017年 | 6篇 |
2016年 | 6篇 |
2015年 | 9篇 |
2014年 | 5篇 |
2013年 | 11篇 |
2012年 | 6篇 |
2011年 | 8篇 |
2010年 | 5篇 |
2009年 | 11篇 |
2008年 | 9篇 |
2007年 | 17篇 |
2006年 | 2篇 |
2005年 | 10篇 |
2004年 | 5篇 |
2003年 | 12篇 |
2002年 | 5篇 |
2001年 | 6篇 |
2000年 | 1篇 |
1999年 | 5篇 |
1998年 | 13篇 |
1997年 | 2篇 |
1996年 | 1篇 |
1995年 | 4篇 |
1994年 | 4篇 |
1993年 | 6篇 |
1992年 | 1篇 |
1991年 | 1篇 |
1990年 | 1篇 |
1988年 | 1篇 |
1987年 | 1篇 |
排序方式: 共有217条查询结果,搜索用时 31 毫秒
41.
利用海南岛上常规观测资料,雷达、葵花卫星等非常规观测资料,欧洲中心再分析资料和NCEP全球实时海温,对比分析了2018年3月3日海南冰雹的环境条件及其中尺度特征。结果表明:(1)3月2—4日,大尺度环流特征为中层干冷的W—SW急流、低层SW暖气流及地面西南低压槽。(2)3日的区域大气层结处于稳定转变为不稳定的状态,局地增长的不稳定能量在海风锋的触发下强烈释放,适宜的0~6km垂直风切变,0℃、20℃高度有利于对流单体发展成雹暴单体。(3)2日海南岛附近区域层结稳定,CAPE值偏低;4日海南岛处于低层大风核入口前侧,水汽辐散,海风锋垂直环流被抑制,这些都不利于强对流的发展。(4)此次降雹单体具有多个雷达回波特征,当移入多普勒雷达静锥区后,利用风廓线雷达资料可监测到高层急流脉动下传,0~5km、0~3km垂直风切变相继增大的特征,对判断风暴的演变具有重要参考意义。(5)初生对流单体在地面辐合线和儋州中部露点锋交界处生成,在海风锋北端和海口-澄迈北部露点锋重叠区发展为雹暴单体,雹暴单体前沿的露点锋有新生单体的传播。 相似文献
42.
贺兰山区气候若干问题 总被引:14,自引:0,他引:14
本文主要利用宁夏区农业厅和区气象局气候资料中心于1985年3月,组织的贺兰山中部剖面考察期间11个气象站点的观测资料,在国内首次对贺兰山的气候特征进行了较为系统的研究。本文主要阐述了贺兰山东麓的冷湖效应,东坡磷矿点典型的山谷风现象,雨季的最大降水高度,以及研究确定了剖面上西坡日照百分率随高度的真实分布。 相似文献
43.
Following the collapse of the New York World Trade Center (WTC) towers on September 11, 2001, Local, State, and Federal agencies initiated numerous air monitoring activities to better understand the ongoing impacts of emissions from the disaster. The collapse of the World Trade Center towers and associated fires that lasted for several weeks resulted at times in a noticeable plume of material that was dispersed around the Metropolitan New York City (NYC) area. In general, the plume was only noticeable for a short period of time following September 11, and only apparent close to the World Trade Center site. A study of the estimated pathway which the plume of WTC material would likely follow was completed to support the United States Environmental Protection Agency’s 2002 initial exposure assessments. In this study, the WTC emissions were simulated using the CALMET-CALPUFF model in order to examine the general spatial and temporal dispersion patterns over NYC. This paper presents the results of the CALPUFF plume model in terms of plume dilution and location, since the exact source strength remains unknown. Independent observations of PM2.5 are used to support the general dispersion features calculated by the model. Results indicate that the simulated plume matched well with an abnormal increase (600–1000% of normal) in PM2.5 two nights after the WTC collapse as the plume rotated north to southeast, towards parts of NYC. Very little if any evidence of the plume signature was noted during a similar flow scenario a week after September 11. This leads to the conclusion that other than areas within a few kilometers from the WTC site, the PM2.5 plume was not observable over NYC’s background concentration after the first few days. 相似文献
44.
Observations from two SOund Detection And Ranging (SODAR) units, a 10 m micrometeorological tower and five Automated Surface Observing Stations (ASOS) were examined during several synoptic scale flow regimes over New York City after the World Trade Center disaster on September 11, 2001. An ARPS model numerical simulation was conducted to explore the complex mesoscale boundary layer structure over New York City. The numerical investigation examined the urban heat island, urban roughness effect and sea breeze structure over the New York City region. Estimated roughness lengths varied from 0.7 m with flow from the water to 4 m with flow through Manhattan. A nighttime mixed layer was observed over lower Manhattan, indicating the existence of an urban heat island. The ARPS model simulated a sea-breeze front moving through lower Manhattan during the study period consistent with the observations from the SODARs and the 10-m tower observations. Wind simulations showed a slowing and cyclonic turning of the 10-m air flow as the air moved over New York City from the ocean. Vertical profiles of simulated TKE and wind speeds showed a maximum in TKE over lower Manhattan during nighttime conditions. It appears that this TKE maximum is directly related to the influences of the urban heat island. 相似文献
45.
The influence of the main large-scale wind directions on thermally driven mesoscale circulations at the Baltic southwest coast, southeast of Sweden, is examined. The aim of the study is to highlight small-scale alterations in the coastal atmospheric boundary layer. A numerical three-dimensional mesoscale model is used in this study, which is focused on an overall behaviour of the coastal jets, drainage flows, sea breezes, and a low-level eddy-type flow in particular. It is shown that synoptic conditions, together with the moderate terrain of the southeast of Sweden (max. height h0 206 m), governs the coastal mesoscale dynamics triggered by the land-sea temperature difference T. The subtle nature of coastal low-level jets and sea breezes is revealed; their patterns are dictated by the interplay between synoptic airflow, coastline orientation, and T.The simulations show that coastal jets typically occur during nighttime and vary in height, intensity and position with respect to the coast; they interact with downslope flows and the background wind. For the assigned land surface temperature (varying ±8 K from the sea temperature) and the opposing constant geostrophic wind 8 m s-1, the drainage flow is more robust to the opposing ambient flow than the sea breeze later on. Depending on the part of the coast under consideration, and the prevailing ambient wind, the sea breeze can be suppressed or enhanced, stationary at the coast or rapidly penetrating inland, locked up in phase with another dynamic system or almost independently self-evolving. A low-level eddy structure is analyzed. It is governed by tilting, divergence and horizontal advection terms. The horizontal extent of the coastal effects agrees roughly with the Rossby radius of deformation. 相似文献
46.
47.
48.
利用常规气象观测资料、多普勒气象雷达资料、浙江省自动站加密资料、NCEP/FNL再分析资料,结合高分辨率中尺度数值模式WRF对杭州湾地区2016年7月28日一次海风锋触发雷暴天气的发生、发展演变特征进行数值模拟。结果表明:1)海风锋是此次强雷暴天气过程的主要触发系统。2)中尺度模式WRF较好地模拟出此次雷暴过程的降水和低层风场、温度场分布以及海风锋水平垂直结构。3)海风锋对局地比湿及涡度特征的加强有明显的促进作用,为雷暴的发生发展提供有利的水汽和动力条件。4)分析对流参数演变曲线的突变位置,对雷暴发生的时间有一定的指示和预报意义,杭州湾南侧单纯的海风锋也可以触发雷暴的发生发展。 相似文献
49.
青岛近海夏季海风特征及其预报方法研究 总被引:3,自引:1,他引:2
采用2003~2006年7~9月青岛以及沿海地区自动站资料、探空资料对青岛近海海风进行了统计分析.平均而言,青岛近海7~8月海风发生频率为30%~35%,9月海风发生频率为25%;海风开始时间平均为10:00~12:00,结束时间可以持续到18:00~19:00;海风在垂直方向上厚度为500~600 m左右.青岛近海海风的发生与否取决于青岛上空低层925 hPa风速大小、低层大气稳定度、海陆温差以及海平面气压差四方面的综合效应.通常,925 hPa风速达到8 m/s,系统风较强时不利于海风建立;当低层大气不稳定时,有利于触发海风环流的建立;海陆温差达到4 ℃以上时,青岛近海易出现海风;此外,当地转风为离岸风时,海阳站或日照站与青岛本站08:00时海平面气压差>1 hPa时,当日一般不会出现海风.综合以上预报因子及其指标,通过建立逻辑回归模型,初步实现了夏季青岛近海海风能否发生的客观预报,并在2007年举行的国际帆船赛期间得到了应用. 相似文献
50.
Sea-breeze-initiated rainfall over the east coast of India during the Indian southwest monsoon 总被引:1,自引:0,他引:1
Matthew Simpson Hari Warrior Sethu Raman P. A. Aswathanarayana U. C. Mohanty R. Suresh 《Natural Hazards》2007,42(2):401-413
Sea-breeze-initiated convection and precipitation have been investigated along the east coast of India during the Indian southwest
monsoon season. Sea-breeze circulation was observed on approximately 70–80% of days during the summer months (June–August)
along the Chennai coast. Average sea-breeze wind speeds are greater at rural locations than in the urban region of Chennai.
Sea-breeze circulation was shown to be the dominant mechanism initiating rainfall during the Indian southwest monsoon season.
Approximately 80% of the total rainfall observed during the southwest monsoon over Chennai is directly related to convection
initiated by sea-breeze circulation. 相似文献