共查询到18条相似文献，搜索用时 234 毫秒
1.
多重网格法在加速自适应网络生成中的应用 总被引：2，自引：0，他引：2
多重网格法是７０年代以来发展起来的用于加速迭代收敛的一种行之有效的方法,它能过采用不同疏密的网格距来“消除”不同频率范围内的误差分量的办法。加速了迭代的收敛速度,具有收敛速度快,收敛精度高以及节省ＣＰＵ时间等特点。 相似文献
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将多重网格法应用于MM5中来加速自适应网格的生成,并用这种方法来模拟2002年6月17-18日发生在江南和华南的暴雨过程。试验表明：在收敛精度要求高的情况下自适应模式模拟结果的精度高于均匀网格模式,且多重网格法有助于提高运算效率。 相似文献
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基于并行可扩展科学计算工具集求解GRAPES全球非静力模式亥姆霍兹问题 总被引：1，自引：1，他引：0
亥姆霍兹方程是非静力平衡大气模式动力内核的主要计算瓶颈之一,其离散矩阵性态差,采用常见预条件Krylov迭代往往收敛很慢。随着全球非静力平衡大气模式时空分辨率的不断提高,亥姆霍兹方程求解面临求解精度和计算时间的双重困难。在高分辨率情况下,迭代计算步数和计算量剧增,而且很多传统的预条件迭代求解方法不收敛,迫切需要研究收敛性和并行可扩展性兼备的预条件迭代方法。为此,在安腾机群上建立了基于并行可扩展科学计算工具集(PETSc)的GRAPES全球非静力平衡模式亥姆霍兹问题并行解法器对比研究平台,结合高性能预条件库(hypre),完成了对GRAPES在用解法器、代数多重网格、并行不完全LU分解(EUCLID)及加性Schwarz区域分解等一系列克雷洛夫预条件迭代的分析对比。结果显示PETSc结合高性能预条件库的并行方案是解决GRAPES模式三维亥姆霍兹方程高效并行计算的一个有效途径,其中以代数多重网格预条件迭代的性能最突出;并行加速比分析显示,代数多重网格预条件迭代的并行可扩展性明显优于GRAPES现有解法器,更适用于更高精度和较大规模并行计算。 相似文献
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自适应网格模式在暴雨数值模拟中的应用 总被引：2，自引：4，他引：2
基于变分原理，自适应网格技术能根据数值模式的特点，在模式解梯度大的地区自动加密网格，提高模式的分辨率。将其应用于MM4模式中，采用多重网格法以加速自适应网格的生成。对1996年8月4日至5日发生在华北的特大台风暴雨过程，用自适应网格模式和均匀网格模式进行了数值模拟和动力诊断分析，以研究自适应网格模式在天气预报和模拟应用中的特点。试验表明，采用自适应网格后计算稳定，对所关心的天气系统及其降水的模拟精度均高于均匀网格模式，对形势场、风场的模拟精度也有明显改善。 相似文献
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日本气象厅电子计算中心大河内芳雄在对500毫巴等压面上台风移动的正压预报中试用多重套网格法收到一定成效。在实验中采用辐散正压模式,网格间隔和时间步长列在表1中;在极射赤面投影地图上,北半球四步细网格套用的范围如图1所示。时间积分用欧拉向后方案,在四步细网格套用范围内计算所用 相似文献
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天气雷达测定区域降水量方法的改进与比较 总被引：9，自引：1，他引：9
讨论变分校准法用于雷达－雨量计系统联合探测降水。由雷达反射率因子Ｚ和地面降水强度Ｉ实时地获得最优Ｚ－Ｉ关系，在求解欧拉方程时采用多重网格法，不仅可提高计算结果的精度，还可大大提高计算速度。 相似文献
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本文在简要介绍了多网格法的基本思想和本文所用的经改进的地气耦合非定常距平模式的基础上，用多网格法求解地气耦合非定常距平模式中的位势倾向方程—椭圆型方程。通过对1982～1989年6～8月的北半球环流季节预报试验表明，由于使用多网格法，迭代精度提高了，克服了原模式预报的距平场过分光滑振幅偏小的缺点，很好地解出了模式中对长期天气预报起关键作用的大尺度低频信号。在高低两种精度下进行的比较试验表明:多网格法较逐步超松弛法可以使计算速度提高1倍以上。高精度较低精度多网格法更为有效。 相似文献
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一种新的雷电日及雷电参数统计方法 总被引：6，自引：3，他引：3
为更好地应用雷电定位系统的自动监测数据统计雷电日及雷电参数,利用滇中地区1987～2006年49个气象站点雷电观测资料和2005～2006年闪电定位探测资料,在对比分析气象观测雷电资料与闪电定位探测雷电资料的基础上,提出了一种新的适用于自动监测雷电日的统计方法--网格法.网格法划分统计区域详细、合理,其雷电日统计值与传统气象雷电日有可比性.长期气象雷电日资料是选定网格大小的参考标尺,滇中地区取0.175°×0.175°网格统计值为其年平均雷电日,取0.3°×0.3°网格统计值为其最大雷电日.用网格法对雷电参数进行统计结果显示:滇中地区雷电日和雷电密度有显著的局地变化特征,地闪密度与闪电强度成反比关系.此结论为防雷工程设计、雷电灾害评估和雷电成因分析提供了较好的理论基础. 相似文献
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A coupled atmosphere/mixed-layer ocean energy balance model of intermediate complexity is used to examine the feasibility of a technique to accelerate the model's convergence rate while using equilibrium asynchronous coupling (EAC). EAC consists of an iterative sequence of integrations of an atmospheric model driven to equilibrium with fixed SSTs, the output of which is used to drive an ocean model to equilibrium. In an attempt to accelerate a radiatively perturbed climate to its final equilibrium state, we superimpose on the EAC scheme a mixed-flux condition, in which a portion of the turbulent air-sea heat flux from the most recent atmospheric leg is used in the present oceanic integration. In sensitivity tests using enhanced insolation, this mixed-flux approach strongly hastens the model's convergence rate, whose acceleration is regionally dependent: the tropics show the strongest sensitivity to the mixed-flux condition, while polar regions are least affected. This geographic variation stems from the presence of polar sea-ice, which promotes a temperature inversion and thereby causes a seasonal change in the sign of the total turbulent air-sea heat flux. Potential applications and limitations of this accelerated EAC method are also discussed. 相似文献
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Using real analysis data of 1°×1° resolution of the National Center for Environmental
Prediction/National Center for Atmospheric Research (NCEP/NCAR), the nondivergent wind component
and irrotational wind component obtained by the harmonic-cosine(H-C) method, and the wind structure of
Typhoon Fung-Wong (coded 0808 in China) in 2008 was analyzed. The results indicated that the
irrotational component was advantageous over the total wind in reflecting both the changes in convergent
height and the asymmetrical convergence of Fung-Wong. In Fung-Wong, the nondivergent component was
larger than the irrotational component, but the latter was much more variable than the former, which was
obtained only from the wind partition method. Further analyses on the irrotational component
demonstrated that the location of the convergent center at lower levels was almost the same as the
divergent center during the development of Fung-Wong, and its convergent level was high in its life cycle,
with the most highest up to 400 hPa when it became stronger. After the typhoon landed in the provinces of
Taiwan and Fujian, respectively, its convergent center at lower levels was slowly detached from the
divergent center at high levels and the convergent height was also depressed from high levels to lower
levels. Gradually, this weakened the intensity of Fung-Wong. This kind of weakening was slow and
Fung-Wong maintained its circulation for a long time over land because of its very thick convergent height.
Analyses on wind partitioning provided one possible explanation to why Fung-Wong stayed for a long time
after it landed. Furthermore, the asymmetric vertical ascending motion was induced by the asymmetric
convergence at lower levels. In general, when typhoons (such as Fung-Wong) land, the rainfall region
coincides with that of the convergence region (indicated by the irrotational component at lower layers).
This means that the possible rainfall regions may be diagnosed from the convergent area of the irrotational
component. For an observational experiment on typhoons, the convergent region may be considered as a
key observational region. 相似文献
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l.IntroductionWithhighlydevelopingofmodernscientifictechnologyandincessantupdatingoftheobservationalsystem,manykindsofnewsourcesofobservationaldataarereadilyobtained,suchassatellitedataandradardata.Ithasbeenacriticalproblemtopuzzleresearcherstoeffectivelyemploythesedatainnumericalcalculation.4DVARtechniquehasgraduallybeenaveryimportanttoolinthemainstreamofnumericalweatherprediction,becauseitisofstrongcapabilityofcombiningandextractingtheusefulinformationfromallkindsofobservationaldata.Thedat… 相似文献
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Based on the daily regional mean rainfall,the Z-index method is used to identify persistent flood and drought events lasting for at least 10 days over a region where Dongting Lake and Poyang Lake sit(referred to as the"two-lake region"hereafter).The National Centers for Environmental Prediction(NCEP)reanalysis data are then utilized to perform a preliminary diagnostic analysis on these events.The results indicate that the composite standardized geopotential height at 500 hPa presents two different meridional wave trains from north to south over the East Asian-Pacific region,i.e.,a"-+-"pattern for the droughts and a"+-+"pattern for the floods,respectively.The developing,maintaining and decaying phases in the drought and flood events are closely related to the intensity and location of a subtropical high and an extra-tropical blocking high.It is shown that the East Asian summer monsoon is strong(weak)with the occurrence of persistent drought(flood)events.Droughts(floods)are accompanied by a weak(strong)tropical convergent system and a strong(weak)subtropical convergent system.Furthermore,the persistent drought(flood)events are associated with a divergence(convergence)of vertically integrated water vapor flux.In the vertical profile of water vapor flux,divergence(convergence)in the mid-and lower-levels and convergence(divergence)in the higher levels are evident in the droughts(floods).Both the divergence in the droughts and the convergence in floods are strongest at 850 hPa. 相似文献
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利用上下解构造辅助方程,结合Leray-Schauder度理论研究二阶p-Laplacian方程多点边值问题正解的存在性,并用单调迭代技巧与拟线性化方法讨论了正解迭代序列的收敛性. 相似文献
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利用常规天气图实况资料和NCEP每6 h 1次、2.5°×2.5°再分析资料及NOAA的GBL资料,对2009年6月28—30日安徽南部一次暴雨过程进行物理量诊断分析,同时使用HYSPLIT后向轨迹模式对水汽来源进行模拟。结果表明：高空辐散和低空辐合同时存在而导致的上升运动是此次暴雨的动力条件;来自孟加拉湾和南海充足的水汽来源是暴雨产生的前提条件;同时低空辐合产生切变诱发的不稳定能量释放,促使了大暴雨过程的产生。 相似文献
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In this paper, the coupling schemes of atmosphere-ocean climate models are discussed with one-dimensional advection equations.
The convergence and stability for synchronous and asynchronous schemes are demonstrated and compared.
Conclusions inferred from the analysis are given below. The synchronous scheme as well as the asynchronous-implicit scheme
in this model are stable for arbitrary integrating time intervals. The asynchronous explicit scheme is unstable under certain
conditions, which depend upon advection velocities and heat exchange parameters in the atmosphere and oceans. With both synchronous
and asynchronous stable schemes the discrete solutions converge to their unique exact ones. Advections in the atmosphere and
ocean accelerate the rate of convergence of the asynchronous-implicit scheme. It is suggusted that the asynchronous-implicit
coupling scheme is a stable and efficient method for most climatic simulations. 相似文献
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In this paper, the coupling schemes of atmosphere-ocean climate models are discussed with one-dimensional advection equations. The convergence and stability for synchronous and asynchronous schemes are demonstrated and compared.Conclusions inferred from the analysis are given below. The synchronous scheme as well as the asynchronous-implicit scheme in this model are stable for arbitrary integrating time intervals. The asynchronous explicit scheme is unstable under certain conditions, which depend upon advection velocities and heat exchange parameters in the atmosphere and oceans. With both synchronous and asynchronous stable schemes the discrete solutions converge to their unique exact ones. Advections in the atmosphere and ocean accelerate the rate of convergence of the asynchronous-implicit scheme. It is suggusted that the asynchronous-implicit coupling scheme is a stable and efficient method for most climatic simulations. 相似文献