基于CLDAS资料的内蒙古干旱监测分析   总被引：5，自引：1，他引：4  

孙小龙  宋海清  李平  李云鹏  武荣盛 《气象》2015,41(10):1245-1252

以内蒙古地区为研究区域,对中国气象局陆面数据同化系统（CMA Land Data Assimilation System,CLDAS）的土壤湿度和降水数据进行了评估,使用土壤相对湿度法和连续无降水日数法监测2014年夏季干旱,并选择干旱年（2014年）和湿润年（2013年）与标准化降水指数和降水百分位指数法进行验证分析。结果表明：CLDAS资料能够很好地再现日土壤相对湿度动态变化情况和降水落区与量级,能够满足干旱监测的需求;基于CLDAS数据的土壤相对湿度法可以方便、快捷地监测干旱日变化和区域性变化,连续无有效降水日数法对评估长时间、持续性干旱较为有效;CLDAS同化数据在时效性、分辨率、代表性上能够满足气象服务的需求,可作为观测资料的重要补充广泛应用于业务和科研,特别是对于地广人稀且气象站点相对较少的内蒙古地区气象服务潜力巨大。  相似文献   

印度-欧亚碰撞与洋-陆碰撞的差异   总被引：1，自引：0，他引：1       下载免费PDF全文

曾融生  吴庆举  丁志峰  朱露培 《地震学报》2007,29(1):1-10

观测的证据充分表明，印度——欧亚的缝合带雅鲁藏布江上存在自南向北的地壳俯冲带，它穿过莫霍面，深度大约达到100 km. 喜马拉雅中可能存在多重的地壳俯冲. 它们有别于海洋碰撞时所产生的整个岩石圈俯冲. 作者观测到雅鲁藏布江以北上地幔的板片构造，它可以解释为印度向欧亚俯冲时上地幔岩石圈的痕迹. 它们说明与洋——陆的俯冲不同，印度向欧亚俯冲时，地壳与上地幔岩石圈出现拆层现象. 综合现有的地壳上地幔构造，显示在不同地质年代中，印度与欧亚之间产生自南向北以及自北向南相反方向的俯冲，而且俯冲带周围出现某些速度异常区.   相似文献   

Depth distribution of Moho and tectonic framework in eastern Asian continent and its adjacent ocean areas   总被引：3，自引：0，他引：3  

滕吉文  曾融生  闫雅芬  张慧 《中国科学D辑(英文版)》2003,46(5):428-446

It is the essence of the study on the dynamics of eastern Asian continent to investigate the ef-fects of geophysical field and the process of the deep block boundaries, and furthermore, to estab-lish a geodynamic physical-mathematical model based on the d…  相似文献   

The upper mantle structure of the Tibetan Plateau and its implication for the continent-continent collision   总被引：1，自引：0，他引：1  

WU Qingju  ZENG Rongsheng & ZHAO Wenjin . Institute of Geophysics  China Earthquake Administration  Beijing  China  . Institute of Geology  China Academy of Geological Sciences  Beijing  China 《中国科学D辑(英文版)》2005,48(8):1158-1164

The present continent had been assembled by the accretion of a series of terrains after their mutual colli-sions. Thus, the continental collision process plays an important role in the tectonics, the deformation and the movement in the continent. The Indo-Eurasian colli-sion had not only produced the grand geological structures and landscape, such as the Himalayan Mountain and the Tibetan Plateau, but also played a decisive role in the tectonic deformation and seismic-ity of Eastern Asia si…  相似文献   

The Role of β-effect and a Uniform Current on Tropical Cyclone Intensity   总被引：8，自引：3，他引：5  

DUAN Yihong  WU Rongsheng  YU Hui  LIANG Xudong  Johnny C L CHAN 《大气科学进展》2004,21(1):75-86

A limited-area primitive equation model is used to study the role of the β-effect and a uniform current on tropical cyclone (TC) intensity.It is found that TC intensity is reduced in a non-quiescent environment compared with the case of no uniform current.On an f-plane,the rate of intensification of a tropical cyclone is larger than that of the uniform flow.A TC on a β-plane intensifies slower than one on an f-plane.The main physical characteristic that distinguishes the experiments is the asymmetric thermodynamic (including convective) and dynamic structures present when either a uniform flow or β-effect is introduced.But a fairly symmetric TC structure is simulated on an f-plane.The magnitude of the warm core and the associated subsidence are found to be responsible for such simulated intensity changes.On an f-plane,the convection tends to be symmetric,which results in strong upper-level convergence near the center and hence strong forced subsidence and a very warm core.On the other hand,horizontal advection of temperature cancels part of the adiabatic heating and results in less warming of the core,and hence the TC is not as intense.This advective process is due to the tilt of the vortex as a result of the β-effect.A similar situation occurs in the presence of a uniform flow.Thus,the asymmetric horizontal advection of temperature plays an important role in the temperature distribution.Dynamically,the asymmetric angular momentum (AM) flux is very small on an f-plane throughout the troposphere.However,the total AM exports at the upper levels for a TC either on aβ-plane or with a uniform flow environment are larger because of an increase of the asymmetric as well as symmetric AM export on the plane at radii ＞450 km,and hence there is a lesser intensification.  相似文献   

The Major Research Advances of Mesoscale Weather Dynamics in China Since 2003   总被引：1，自引：0，他引：1  

陆汉城  高守亭  谈哲敏  周晓平  伍荣生 《大气科学进展》2007,24(6):1049-1059

This paper reviews the main theoretical progress of mesoscale weather dynamics since 2003, including： （1） The dynamic mechanisms of balanced and unbalanced flow are applied to study the genesis and development problems of mesoscale circulation. The symmetric instability and transverse-wave instability are analyzed in line and vortex atmosphere convection, and further research has been done on nonlinear convective symmetric instability. The interaction between forced convection and unstable convection and the wave characteristics of mesoscale motion are also discussed. （2） Intermediate atmosphere dynamic boundary layer models are developed. The complicated nonlinear interaction is analyzed theoretically between the atmospheric boundary layer and the free atmosphere. The structure of the topography boundary layer, atmospheric frontogenesis, the structure and circulation of the low-level front and other boundary layer dynamic problems are discussed. （3） The formation and development of meso-β-scale rainstorms under the background of the East-Asia atmosphere circulation are diagnosed with the variation of MPV （moist potential vorticity） anomalies. And some physical vectors are modified and applied in the moist atmosphere.  相似文献   

Adakite-like porphyries from the southern Tibetan continental collision zones: evidence for slab melt metasomatism   总被引：21，自引：0，他引：21  

Yongfeng Gao  Zengqian Hou  Balz S. Kamber  Ruihua Wei  Xiangjin Meng  Rongsheng Zhao 《Contributions to Mineralogy and Petrology》2007,153(1):105-120

We present new whole rock trace element and Pb-isotope data for a suite of Neogene adakitic rocks that formed during the post-collisional stage of the India-Asia collision in an east-west- trending array along the Yalu Tsangpo suture. Compared to classic ‘adakites’ that form along certain active convergent plate margins, the Tibetan adakitic rocks show even stronger enrichment in incompatible elements (i.e. Rb, Ba, Th, K and LREEs) and even larger variation in radiogenic (Pb, Sr, Nd) isotope ratios. Tibetan adakitic rocks have extraordinarily low HREE (Yb: 0.34–0.61 ppm) and Y (3.71–6.79 ppm), high Sr/Y (66–196), high Dy_n/Yb_n and La_n/Yb_n. They show strong evidence of binary mixing both in isotopic space (Sr-Nd, common Pb, thorogenic Pb) and trace element systematics. The majority of the adakitic rocks in south Tibet, including published and our new data, have variational Mg# (0.32–0.70), clear Nb (and HFSE) enrichment, the lowest initial ⁸⁷Sr/⁸⁶Sr and ²⁰⁶Pb/²⁰⁴Pb ratios, and the highest ¹⁴⁴Nd/¹⁴³Nd ratios of all Neogene volcanic rocks in south Tibet. These results indicate an involvement of slab melts in petrogenesis. Major and trace element characteristics of the isotopically more enriched adakites are compatible with derivation from subducted sediment but not with assimilation of crustal material. Thus, the south Tibetan adakitic magmas are inferred to have been derived from an upper mantle source metasomatised by slab-derived melts. An interesting observation is that temporally coeval and spatially related lamproites could be genetically related to the adakitic rocks in representing partial melts of distinct mantle domains metasomatised by subducted sediment. Our favoured geodynamic interpretation is that along-strike variation in south Tibetan post-collisional magma compositions may be related to release of slab melts and fluids along the former subduction zone resulting in compositionally distinct mantle domains.  相似文献   

GPS单历元定位新算法用于滑坡监测di   总被引：2，自引：0，他引：2       下载免费PDF全文

刘根友  朱耀仲  周蓉生 《地震学报》2005,27(4):402-408

在滑坡变形较大时，常规GPS静态观测方式满足不了滑坡实时监测的需要. 本文结合滑坡变形的特点，利用GPS单历元定位新方法frac34;单历元阻尼LAMBDA方法，对滑坡实时形变进行了监测试验. 该方法不需要考虑GPS载波相位测量中棘手的周跳问题，每一历元即可搜索到正确的整周模糊度，从而获得监测点厘米级精度的坐标. 采用平滑方法后可以分辨出毫米级精度的坐标和滑动速度，扩大了GPS形变监测的应用范围. 本文简要介绍了新方法的原理，并使用低价位的单频GPS接收机，在江西省一个实测滑坡中取得了较好的应用效果.    相似文献   

有限区域伴随模式中适定空间边界条件的理论研究   总被引：2，自引：0，他引：2  

Wang Yuan  Wu Rongsheng 《大气科学进展》2001,18(6):1081-1089

从理论上论证了借助于同伦方法构造的适定空间边界条件确保有限区域上伴随模式产生的超定边界条件问题得到解决，同时又能维持伴随模式中边界处理的优化特征。从某种意义上讲，伴随模式超定空间边界条件的存在是不可避免的，这是因为数据同化过程必须引进和采用给定的观测资料，而它们在模式空间边界上的定义往往是超定的。我们提出的空间边界条件的算法构架事实上是在数据同化过程中综合运用了张弛滤波、考虑外部强迫的辐射边界条件以及与观测相容的狄里希利边界条件。显然，对于该理论构架所涉及到的具体数值处理方法在中尺度模式中都十分成熟易行。  相似文献   

The Conservation of Helicity in Hurricane Andrew （1992） and the Formation of the Spiral Rainband   总被引：5，自引：0，他引：5  

XU Yamei  WU Rongsheng 《大气科学进展》2003,20(6):940-950

The characteristics of helicity in a hurricane are presented by calculating the MM5 model output in addition to theoretical analysis. It is found that helicity in a hurricane mainly depends on its horizontal component, whose magnitude is about 100 to 1000 times larger than its vertical component. It is also found that helicity is approximately conserved in the hurricane. Since the fluid has the intention to adjust the wind shear to satisfy the conservation of helicity, the horizontal vorticity is even larger than the vertical vorticity, and the three-dimensional vortices slant to the horizontal plane except in the inner eye. There are significant horizontal vortices and inhomogeneous helical flows in the hurricane. The formation of the spiral rainband is discussed by using the law of horizontal helical flows. It is closely related to the horizontal strong vortices and inhomogeneous helical flows.  相似文献