An Amplification Mechanism of Intraseasonal Long Rossby Wave in Subtropical Ocean   总被引：3，自引：0，他引：3  

Xiaopei?LinEmail author  Dexing?Wu  Qiang?Li  Jian?Lan 《Journal of Oceanography》2005,61(2):369-378

The satellite altimeter data reveal that intraseasonal long Rossby wave is amplified in the western part of subtropical ocean. Based on a two and half layer ocean model we infer that the intraseasonal long Rossby wave may be amplified by the baroclinic instability. According to the baroclinic instability criterion derived from the two and half layer model, we calculate the baroclinic instability area of the Subtropical North Pacific Ocean based on Levitus98 data. The baroclinic instability area is well in accord with the amplification area of the intraseasonal long Rossby wave, and this also proves that the baroclinic instability is the main amplification mechanism of the intraseasonal long Rossby wave in the subtropical ocean. The consistency between the baroclinic instability area and potential vorticity (PV) pool is further proved in this paper, therefore, we have confidence that the intraseasonal long Rossby wave is amplified in the PV pool. Due to the relatively large ocean basin and weak ventilation, the PV pool is much larger in the North Pacific Ocean than in the North Atlantic Ocean, and this is the reason for the difference of wave amplification areas of these two Oceans.  相似文献   

Second order potential vorticity and its potential applications   总被引：1，自引：0，他引：1  

ShouTing Gao  PengCheng Xu  Na Li  YuShu Zhou 《中国科学:地球科学(英文版)》2014,57(10):2428-2434

A new invariant, the second order potential vorticity (SPV), is derived in this paper. SPV is the dot product of vorticity and the potential vorticity (PV) gradient, and is proven conservative for a compressible, adiabatic and frictionless atmosphere. Research shows that the new invariant may be used to indicate the evolution of PV, because SPV includes all the information that determines PV evolution: the wind field, and the PV gradient. Furthermore, SPV is capable of diagnosing heavy precipitation because of the strong signals it presents in areas of heavy rainfall. SPV also shows great potential as a comprehensive conserved quantity for indicating the dynamical tropopause and baroclinic instability.  相似文献   

吉林省不同水系的高锰酸盐指数、化学需氧量和总有机碳的相关关系比较   总被引：1，自引：0，他引：1  

袁懋  董德明  花修艺  张立辉 《地理科学》2008,28(2):286-290

通过对吉林省四大水系的主要河流在2005~2006年内采样,测其高锰酸盐指数(PV)、化学需氧量(COD)和总有机碳(TOC),用最小二乘法对PV—TOC、COD—TOC和COD—PV进行线性回归,并进行相关关系的显著性检验,建立吉林省四大水系主要河流PV—TOC、COD—TOC和COD—PV的定量关系模型。结果表明,吉林省四大水系主要河流中PV—TOC、COD—TOC和COD—PV之间均具有显著的线性相关关系,不同水系的线性相关关系之间存在一定的差异。  相似文献   

光伏屋顶项目发电系统设计与分析     

王艳国 《中国勘察设计》2012,(1):81-83

基于建筑屋顶面积大、无遮阳等具有可利用光伏屋顶发电的有利条件,本文以山西某市职中校区内的建筑物为例,从气象条件、系统运行方式、光伏电池方阵设计及并网电气设计等方面提出了综合优化设计方案。  相似文献   

THE IMPACTS OF INTERACTION OF A TYPHOON WITH THE MIDLATITUDE TROUGH ON ITS TRACK AFTER THE RECURVATURE     

王凯  陈华  王金梅 《热带气象学报(英文版)》2017,23(2):202-209

Three typhoon cases are selected to conduct a series of simulations that are initialized from sequential analyses. The results show that the forecast error in crucial area where a tropical cyclone (TC) interactes with the upstream trough is highly correlated to the track forecast error after the TC recurvature. Furthermore, sensitivity experiments confirm that the developments of the midlatitude downstream circulations and then the TC track after its recurvature are highly sensitive to the TC intensity and its location relative to the upstream trough, which can give an example or one way of sensitivity of the TC track to the TC-trough interaction. If the TC interacts with the upstream trough more strongly (e.g., the TC being intensified or getting closer to the upstream trough), the downstream circulations will be more meridional, thus the TC track will be more northerly and westerly; otherwise, the downstream circulations will be more zonal, and the TC track will be more southerly and easterly.  相似文献   

人工订正位涡改进模式初始场技术研究     

宫宇  徐珺  代刊  杨寅  杨舒楠 《气象》2016,42(12):1498-1505

面对数值天气预报模式发展中的制约,如今气象界提出了预报员数据同化(data assimilation,DA)的理念,即将预报员的能力有机地融入到数值预报模式中以便发挥各自的优势。人工订正位涡改进模式初始场技术即充分体现了这一理念,其原理是利用了在中、高纬度气旋性环流场中,位涡(potential vortictiy,PV)场和卫星水汽图像(satellite water vapor imagery,WV)较好的对应关系检验数值预报,进而利用位涡的可反演性通过人工修改位涡场来订正数值预报,并已在部分国家实践中证明有着显著的改进模式预报性能的效果。本研究将通过分析对流层中高层的动力活跃区、位涡分布和卫星水汽图像暗区的关系检验模式偏差,进而通过人工订正位涡场和位涡反演,实现对模式初始场的修改,为预报员主观订正模式初始场、改进模式预报能力提供完整的技术流程。  相似文献   

屋顶光伏为基础的农村新型能源系统战略研究   总被引：1，自引：0，他引：1  

江亿  胡姗 《气候变化研究进展》2022,18(3):272-282

当前我国农村仍然面临着经济发展、清洁用能、环境保护、减少碳排放等多重问题,文中对我国农村地区发展屋顶光伏系统的资源潜力、技术方案、融资模式和重要意义进行了深入探讨和定量分析,结果表明,我国农村地区面临着能源、环境、经济发展的多重问题,“双碳”战略给解决“三农”问题提供了新的发展契机。发展以农村屋顶光伏系统为基础的新型农村能源系统是解决“三农”问题、实现乡村振兴的重点工作,也是我国建成新型电力系统、实现能源系统低碳转型的突破口和着力点。  相似文献   

Synoptic and dynamic analysis of a flash flood-inducing heavy rainfall event in arid and semi-arid central-northern Iran and its simulation using the WRF model     

《Dynamics of Atmospheres and Oceans》2021

The synoptic and dynamic aspects of heavy rainfall occurred on 5th May 2017 and caused flash flooding in arid and semi-arid central-northern Iran is analyzed by the Weather Research and Forecasting (WRF) model. This system synoptically is attributed to a surface low-pressure centered over southern Iran extended to the central parts, linking to a mid-tropospheric tilted-trough over western Iran, and advecting significant moisture from the Mediterranean Sea and the Red Sea to the studied area. The dynamical analysis revealed that the penetration of the upper-tropospheric potential vorticity streamer up to 300 hPa level was not related to such heavy rainfall. Contrarily, the low-level factors such as extensive moisture advection, mid-tropospheric diabatic processes such as the latent heat release, daytime deep convection, and topographical impact of Zagros Mountains were found as the key factors leading to this system. This study also examines 11 different convection schemes simulated by the WRF model and verified against rainfall observation. The forecast skills of the output simulations suggest the Grell-Devenyi scheme as the superior configuration in simulating observed precipitation of the event over the area.  相似文献   

PV Perspective of Impacts on Downstream Extreme Rainfall Event of a Tibetan Plateau Vortex Collaborating with a Southwest China Vortex     

Guanshun ZHANG  Jiangyu MAO  Yimin LIU  Guoxiong WU 《大气科学进展》2021,38(11):1835-1851

An extreme rainfall event occurred over the middle and lower reaches of the Yangtze Basin(MLY) during the end of June 2016, which was attributable to a Tibetan Plateau(TP) Vortex(TPV) in conjunction with a Southwest China Vortex(SWCV). The physical mechanism for this event was investigated from Potential Vorticity(PV) and omega perspectives based on MERRA-2 reanalysis data. The cyclogenesis of the TPV over the northwestern TP along with the lowertropospheric SWCV was found to involve a midtropospheric large-scale flow reconfiguration across western and eastern China with the formation of a high-amplitude Rossby wave. Subsequently, the eastward-moving TPV coalesced vertically with the SWCV over the eastern Sichuan Basin due to the positive vertical gradient of the TPV-related PV advection,leading the lower-tropospheric jet associated with moisture transport to intensify greatly and converge over the downstream MLY. The merged TPV-SWCV specially facilitated the upper-tropospheric isentropic-gliding ascending motion over the MLY. With the TPV-embedded mid-tropospheric trough migrating continuously eastward, the almost stagnant SWCV was re-separated from the overlying TPV, forming a more eastward-tilted high-PV configuration to trigger stronger ascending motion including isentropic-gliding, isentropic-displacement, and diabatic heating-related ascending components over the MLY. This led to more intense rainfall. Quantitative PV diagnoses demonstrate that both the coalescence and subsequent re-separation processes of the TPV with the SWCV were largely dominated by horizontal PV advection and PV generation due to vertically nonuniform diabatic heating, as well as the feedback of condensation latent heating on the isentropicdisplacement vertical velocity.  相似文献   

Formation and Replacement Mechanism of the Concentric Eyewall of Super Typhoon Muifa (1109)     

黄朗  文映方  刘宇迪 《热带气象学报(英文版)》2022,28(4):425-444

Based on high-fidelity numerical simulation by using the Weather Research and Forecast (WRF) model, we analyzed the formation and replacement mechanism of the concentric eyewall of Super Typhoon Muifa (1109) from the aspects of the potential vorticity (PV), dynamic/ thermodynamic structure change, sea surface flux, and water vapor content. Observational data and sensitivity tests were also adopted to verify the results. We found that: (1) The abnormal increase of the PV in the rain zone is mainly due to the condensation latent heat. Sufficient water vapor conditions are beneficial to the formation of the outer eyewall structure, and when the environmental water vapor content is larger, the intensity of the outer eyewall becomes greater. (2) After the formation of the typhoon’s outer eyewall, in the area where the outer eyewall is located, the increase of inertial stability contributes to the decrease of the intensity of the inner eyewall. When the intensity of the outer eyewall is larger, the divergence and subsidence motion in the upper layer of the outer eyewall has a greater weakening effect on the intensity of the inner eyewall. (3) The increase of potential temperature of the outer eyewall is mainly due to the condensation latent heat release and the warming of dry air subsidence motion in the moat area. (4) The increase of sea surface heat flux can prolong the concentric eyewall replacement process.  相似文献