您现在的位置: 首页> 研究主题> 热带气象

热带气象

热带气象的相关文献在1989年到2019年内共计87篇,主要集中在大气科学(气象学)、海洋学、信息与知识传播 等领域,其中期刊论文86篇、会议论文1篇、专利文献10226篇;相关期刊22种,包括新世纪周刊、应用气象学报、高原山地气象研究等; 相关会议1种,包括中国气象学会2003年年会等;热带气象的相关文献由188位作者贡献,包括陈联寿、任福民、余晖等。

热带气象—发文量

期刊论文>

论文:86 占比:0.83%

会议论文>

论文:1 占比:0.01%

专利文献>

论文:10226 占比:99.16%

总计:10313篇

热带气象—发文趋势图

热带气象

-研究学者

  • 陈联寿
  • 任福民
  • 余晖
  • 刘春霞
  • 房佳蓓
  • 杨修群
  • 端义宏
  • 于华英
  • 何金海
  • 刘纪元

热带气象

-相关会议

  • 期刊论文
  • 会议论文
  • 专利文献

搜索

排序:

年份

    • 端义宏1; 梁旭东1
    • 摘要: 应世界气象组织(WMO)邀请,中国气象科学研究院端义宏和梁旭东研究员参加了由世界气象组织世界天气研究计划(WWRP)热带气象工作组于2018年9月10-13日在新西兰奥克兰举办的第11次热带气象工作组会议及热带气旋全预警系统概念(Total Warning System Concept)科学讨论会。
    • 端义宏
    • 摘要: 2017年9月20-23日,WMO天气研究计划热带气象工作组(WGT-MR/WWRP/WMO)第11次会议在中国香港召开。
    • 徐晶; 王玉清; 刘欣; 任福民; 刘璐; 刘昊炎
    • 摘要: 1概况2018年4月16—20日,美国气象学会(AMS)第33届飓风与热带气象国际研讨会在佛罗里达Ponte Vedra举行。此次盛会吸引了来自全球近700名科学家、一线业务专家和研究生参加,会议口头报告约480个、墙报290个。
    • 吴亚丽; 陈德辉
    • 摘要: The quantitative precipitation forecast(QPF) in very-short range(0-12 hours) has been investigated in this paper by using a convective-scale(3km) GRAPES_Meso model. At first, a latent heat nudging(LHN) scheme to assimilate the hourly intensified surface precipitation data was set up to enhance the initialization of GRAPES_Meso integration. And then based on the LHN scheme, a convective-scale prediction system was built up in considering the initial "triggering"uncertainties by means of multi-scale initial analysis(MSIA), such as the three-dimensional variational data assimilation(3DVAR), the traditional LHN method(VAR0LHN3), the cycling LHN method(CYCLING), the spatial filtering(SS) and the temporal filtering(DFI) LHN methods. Furthermore, the probability matching(PM) method was used to generate the QPF in very-short range by combining the precipitation forecasts of the five runs. The experiments for one month were carried out to validate the MSIA and PM method for QPF in very-short range.The numerical simulation results showed that:(1) in comparison with the control run, the CYCLING run could generate the smaller-scale initial moist increments and was better for reducing the spin-up time and triggering the convection in a very-short time;(2) the DFI runs could generate the initial analysis fields with relatively larger-scale initial increments and trigger the weaker convections at the beginning time(0-3h) of integration, but enhance them at latter time(6-12h);(3) by combining the five runs with different convection triggering features, the PM method could significantly improve the QPF in very-short range in comparison to any single run. Therefore, the QPF with a small size of combining members proposed here is quite prospective in operation for its lower computation cost and better performance.
    • 何钰; 李国平
    • 摘要: By using barotropic model equations, this article analyzed the characteristics of Rossby waves, the propagation features of wave energy and the influence of dynamic and thermal effects of the Tibetan Plateau on Rossby waves,and the focus is on discussing the plateau's topographic gradient effects on atmospheric Rossby waves. Then based on the WRF3.2 and the NCEP/NCAR FNL reanalysis data, we devised comparative tests of changing the plateau's topographic gradient and simulated a process of persistent heavy rain that happened in May 2010 in South China. The results are shown as follows. The Tibetan Plateau's topography is conducive to the formation of atmospheric Rossby waves. while the plateau's terrain, its friction and heating effects can all make the atmospheric Rossby waves develop into the planetary waves; The effects of plateau's north and south slopes on the Rossby wave' phase velocity is opposite,and when the slope reached a certain value can the quasi-steady normal fluctuations be generated; Simultaneously, due to the plateau's topographic gradient, descending motion appears at the west side of the plateau while ascending motion appears at the east side, and the vertical movement increased with the amplification of topographic gradients. The plateau's topographic gradient also obviously amplified the precipitation in South China, and the rainfall area increased with the amplification of topographic gradients and gradually moved from south to north and from west to east, which is conducive to the occurrence and development of convective activities in the downstream areas of the Tibetan Plateau;Moreover, for the plateau's dynamic and thermal effects, the Rossby wave' propagation shows upstream effects of energy dispersion, so the plateau can then affect the weather in downstream areas. Moreover, the wave group velocity increased with the degree of topographic slope.
    • 李泓; 骆婧瑶; 陈葆德
    • 摘要: A hybrid GSI(Grid-point Statistical Interpolation)-ETKF(Ensemble Transform Kalman Filter) data assimilation system has been recently developed for the WRF(Weather Research and Forecasting) model and tested with simulated observations for tropical cyclone(TC) forecast. This system is based on the existing GSI but with ensemble background information incorporated. As a follow-up, this work extends the new system to assimilate real observations to further understand the hybrid scheme. As a first effort to explore the system with real observations, relatively coarse grid resolution(27 km) is used. A case study of typhoon Muifa(2011) is performed to assimilate real observations including conventional in-situ and satellite data. The hybrid system with flow-dependent ensemble covariance shows significant improvements with respect to track forecast compared to the standard GSI system which in theory is three dimensional variational analysis(3DVAR). By comparing the analyses, analysis increments and forecasts, the hybrid system is found to be potentially able to recognize the existence of TC vortex, adjust its position systematically, better describe the asymmetric structure of typhoon Muifa and maintain the dynamic and thermodynamic balance in typhoon initial field. In addition, a cold-start hybrid approach by using the global ensembles to provide flow-dependent error is tested and similar results are revealed with those from cycled GSI-ETKF approach.
    • 刘瑞霞; 张兴赢; 刘杰; 刘雅各
    • 摘要: The variation of the atmospheric Carbon Dioxide(CO_2) concentration plays an important role in global climate and agriculture.We analyzed the spatial-temporal characteristics of CO_2 in the China region and around the globe with the CO_2 column mixing ratios observed by the Japanese GOSAT satellite(Greenhouse Gases Observing Satellite).In order to make sure that the accuracy of the CO_2 data retrieved by the satellite meets the needs of the climate characteristics analyses,we ran a validation on the CO_2 column mixing ratios retrieved by the satellite against the ground-based TCCON(Total Carbon Column Observing Network) observation data.The result shows that the two sets of data have a correlation coefficient of higher than 0.7,and a bias of within 2.2 ppmv.Therefore,the GOSAT CO_2 data can be used for the climate characteristics analysis of global CO_2.Our analysis on the spatial-temporal characteristics of the CO_2 column mixing ratios observed during the period of June 2009 through January 2014 proved that,with the impact of the natural emission of near ground CO_2 and human activities,the global CO_2 concentration has a significant latitudinal characteristics with its highest level averaging 390 ppmv in the 0-40?N latitudinal zone in the Northern Hemisphere,and 387 ppmv in the Southern Hemisphere.China has a relatively higher CO_2 concentration with the highest level exceeding 398 ppmv,and the eastern area higher than the western area.The variation of global CO_2 concentration shows a seasonal pattern,i.e.the CO_2 concentration reaches its highest in spring in the Northern Hemisphere averaging more than 392 ppmv,second highest in winter,and lowest in summer averaging less than 387 ppmv.It fluctuates the most in the Northern Hemisphere with an average concentration of 392.5 ppmv in April,and 385.5 ppmv in July.While in the Southern Hemisphere,the seasonal fluctuation is smaller with the highest concentration occurring in July.Over the recent years,the global CO_2 concentration has shown an elevating trend with an average annual increase rate of 1.58 ppmv per year.It is a challenge that the human kind has to face to slow down the increase of the CO_2 concentration.
    • 王瑞春; 龚建东; 张林; 薛谌彬
    • 摘要: This paper further explores the estimating and expressing of dynamic balance constraints using statistical methods in GRAPES-3DVAR(Version GM). Unlike the single-level scheme which only considers the coupling between mass and wind at one level, the multi-level scheme considers the coupling between their vertical profiles and calculates the balanced mass field at each layer using the rotational wind at all model levels. A reformed ridge regression method is used in the new scheme to avoid the multicollinearity problem and reduce the noises caused by unbalanced mesoscale disturbances. The results of numerical experiments show that the new scheme can get more reasonable vertical mass field, reduce the magnitude of the adjustment by the initialization, and improve the potential temperature analysis performance. Furthermore, the results of forecast verification in January(winter) and July(summer) both confirm that the new scheme can significantly improve the temperature forecast accuracy andbring slight positive effects to the pressure and wind forecast.
    • 岑思弦; 巩远发; 赖欣; 彭亮
    • 摘要: NCEP/NCAR reanalysis data and a 30-year precipitation dataset of observed daily rainfall from 109 gauge stations are utilized in this paper.Using the REOF we analyzed the spatial distribution of precipitation in the 109 stations in the Yangtze River Basin in Meiyu periods from 1978 to 2007.The result showed that the spatial distribution of precipitation in the Yangtze River Basin can be divided into the south and north part.As a result,relationships between an atmospheric heating source(hereafter called ) over the Asian region and the precipitation on the south and north side of Yangtze River in Meiyu periods were separately studied in this paper.The results are shown as follows.The flood/drought to the north of Yangtze River(NYR) was mainly related to the over the East Asia summer monsoon region:when the over the Philippines through Western Pacific and the south China was weakened(strengthened),it would probably result in the flood(drought) in NYR;and the precipitation on the south side of Yangtze River(SYR)was related to the over the east Asia and Indian summer monsoon region:when the over the areas from south China to the northern East China Sea and Yellow Sea and south-eastern Japan was strengthened(weakened),and the over the areas from the Bay of Bengal to south-eastern Tibetan Plateau was weakened(strengthened),it will lead to flood(drought) in SYR.
  • 查看更多

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号