基于中国台湾地区主持的侵台台风之飞机侦察及下投式探空仪观测实验(Dropwindsonde Observations for Typhoon Surveillance near the Taiwan Region,DOTSTAR)获得的高分辨率下投式探空仪探测资料,分析了2003年9月—2012年8月所有发生...基于中国台湾地区主持的侵台台风之飞机侦察及下投式探空仪观测实验(Dropwindsonde Observations for Typhoon Surveillance near the Taiwan Region,DOTSTAR)获得的高分辨率下投式探空仪探测资料,分析了2003年9月—2012年8月所有发生在中国台湾地区附近海域的台风型大气波导事件,遴选出一次由0920号超强台风"卢碧"引起的强台风型海上大气波导过程作为研究对象。利用欧洲中期数值预报中心(ECMWF)再分析资料(水平分辨率0.125°×0.125°),对此次波导的生成原因进行了分析;基于WRF模式比较了不同初始化方法对台风强度、尺度和周围台风型大气波导的模拟能力。结果表明,此次强台风型大气波导发生在台风环流西北侧外围的弱下沉运动区,其形成与850 hPa高度附近北方强干空气平流导致湿度随高度锐减密切相关。在数值模拟中运用台风动力初始化方法,可以有效改进台风强度、路径和尺度的模拟效果,进而有利于改善台风型大气波导尤其是波导层所在高度的模拟效果。台风外围出现的大气波导通常以悬空波导为主,模拟效果与台风螺旋雨带和内核尺度的模拟关系密切,而与台风强度和眼墙结构关系不大。中尺度数值模式WRF具有模拟台风型大气波导的能力,是研究台风型大气波导的有力手段。展开更多
Variable thicknesses in the lowest half-ηmodel level (LML) are often used in atmospheric models to compute surface diagnostic fields such as surface latent and sensible heat fluxes.The effects of the LML on simulat...Variable thicknesses in the lowest half-ηmodel level (LML) are often used in atmospheric models to compute surface diagnostic fields such as surface latent and sensible heat fluxes.The effects of the LML on simulated tropical cyclone (TC)evolution were investigated in this study using the Weather Research and Forecasting (WRF) model.The results demonstrated notable influences of the LML on TC evolution when the LML was placed below 12 m.The TC intensification rate decreased progressively with a lowering of the LML,but its ultimate intensity change was relatively small.The maximum 10-m winds showed different behavior to minimum sea level pressure and azimuthally-averaged tangential winds,and thus the windpressure relationship was changed accordingly by varying the LML.The TC circulation was more contracted in association with a higher LML.Surface latent heat fluxes were enhanced greatly by elevating the LML,wherein the wind speed at the LML played a dominant role.The changes in the wind speed at the LML were dependent not only on their profile differences,but also the different heights they were taken from.Due to the enhanced surface heat fluxes,more intense latent heat release occurred in the eyewall,which boosted the storm's intensification.A higher LML tended to produce a stronger storm,and therefore the surface friction was reinforced,which in turn induced stronger boundary layer inflow together with increased diabatic heating.展开更多
远海悬空波导陷获层底的位置通常与边界层浅云的云顶有很好的对应,气溶胶与边界层浅云的相互作用及其产生的辐射强迫将改变悬空波导的结构.文中利用天气预报-化学(weather research and forecasting-chemistry,WRF-Chem)模式通过设计不...远海悬空波导陷获层底的位置通常与边界层浅云的云顶有很好的对应,气溶胶与边界层浅云的相互作用及其产生的辐射强迫将改变悬空波导的结构.文中利用天气预报-化学(weather research and forecasting-chemistry,WRF-Chem)模式通过设计不包含完整气溶胶-云-辐射的EXP0试验(相当于WRF模式)和包含完整气溶胶-云-辐射相互作用(即气溶胶直接和间接效应)的EXP1试验,对2016年5月观测到的一次珍贵的远海高压型超强悬空波导过程进行了模拟分析.结果表明:远海高压天气形势下,EXP1试验模拟的由气溶胶活化后形成的云滴数浓度比EXP0试验云滴数浓度预设常值(100个cm-3)偏低;当伴随边界层浅云出现时,EXP1试验模拟的波导顶高和强度较EXP0试验更接近于实测;夜间进行的3次观测位于高压中心附近的无云区,此时气溶胶的直接和间接效应均可忽略,因此两组试验模拟的差异极小.这一结果从侧面说明,在有边界层浅云出现的远海区域,包含完整气溶胶-云-辐射效应的WRF-Chem模式有利于提高悬空波导特征量的模拟效果.展开更多
Previous work showed that some tropical cyclones (TCs) in the western Pacific Ocean undergo sudden track reversal, and the onset, maintenance and decay of blocking highs (BHs) coexisted with 19 of the studied TCs ...Previous work showed that some tropical cyclones (TCs) in the western Pacific Ocean undergo sudden track reversal, and the onset, maintenance and decay of blocking highs (BHs) coexisted with 19 of the studied TCs with sudden track reversal. In these cases, the phase relations between the BH, the continental high (CH), the subtropical high (SH) and the suddenly reversed TCs could be classified into types A, B, C and D. Types C and D were the focal point of this follow-up study, in which Typhoon Pabuk (2007) and Lupit (2009) were employed to conduct numerical simulations. The results showed that the reversed tracks of Pabuk (2007) and Lupit (2009) could have been affected by the BH, particularly in terms of the turning location and the trend of movement after turning. Specifically, the two main features for Pabuk (2007) in the BH perturbations were the deflection of its turning point and a distinct anticlockwise rotation. Lupit (2009) deviated to the southwest and finally made landfall in the Philippines, or experienced further eastward movement, in the perturbed BH. The impact mechanisms can be attributed to the change in the vorticity field transported from the BH, leading to an intensity variation of midlatitude systems. BHs may have a positive feedback effect on the strength of the westerly trough (TR), as indicated by a weakened and strengthened TR corresponding to negative and positive BH perturbations, respectively.展开更多
To study the potential effect of sea spray on the evolution of typhoons,two kinds of sea spray flux parameterization schemes developed by Andreas (2005) and Andreas and Wang (2006) and Fairall et al. (1994) respective...To study the potential effect of sea spray on the evolution of typhoons,two kinds of sea spray flux parameterization schemes developed by Andreas (2005) and Andreas and Wang (2006) and Fairall et al. (1994) respectively are incorporated into the regional atmospheric Mesoscale Model version 3.6 (MM5V3) of Pennsylvania State University/National Center for Atmospheric Research (PSU/NCAR) and the coupled atmosphere-sea spray modeling system is applied to simulate a Western Pacific super ty-phoon Ewiniar in 2006. The simulation results demonstrate that sea spray can lead to a significant increase in heat fluxes at the air-sea interface and the simulated typhoon’s intensity. Compared with the results without sea spray,the minimum sea level pressure reduces about 8hPa after taking account of sea spray by Fairall et al.’s parameterization (1994) and about 5hPa by Andreas’ (2005) and Andreas and Wang’s (2006) parameterization at the end of the model integration,while the maximum 10m wind speed increases about 17% and 15% on average,respectively,through the entire simulation time period. Taking sea spray into account also causes significant changes in Tropical Cyclone (TC) structure due to an enhancement of water vapor and heat transferred from the sea sur-face to the air; therefore,the center structure of the typhoon becomes more clearly defined and the wind speed around the typhoon eye is stronger in numerical experiments. The simulations show that different sea spray flux parameterizations make different modi-fications to the TC structure.展开更多
This paper proposes a rain considered geophysical model function (GMF), to be noted as GMF plus Rain. GMF plus Rain is based on the basic raidative transfer model with attenuation and scattering effects of rain on r...This paper proposes a rain considered geophysical model function (GMF), to be noted as GMF plus Rain. GMF plus Rain is based on the basic raidative transfer model with attenuation and scattering effects of rain on radar signal considered. Combined with the NSCAT2 GMF and the rain correction model, the GMF plus Rain model is used to retrieve the ocean wind vectors from the collocated QuikSCAT and SSM/I rain rate data for typhoon Melor. The resulting wind speed estimates of typhoon Melor show improved agreement with the wind fields derived from the best track analysis of Japan Meteorological Agency (JMA). The results imply that compared with the GMF model, the GMF plus Rain model can improve the precision of wind retrieval under the rain condition. Then, a new general algorithm of locating the eye of typhoon through the normalized radar cross section (NRCS) is proposed. The implementation of this algorithm in the ten QuikSCAT observations of typhoon Melor suggests that this algorithm is effective.展开更多
Based on best track data of tropical cyclones(TCs) from the Japan Meteorological Agency, the characteristics of suddenly reversed TCs(SRTCs), which have turning angles usually approaching 180°, are statistica...Based on best track data of tropical cyclones(TCs) from the Japan Meteorological Agency, the characteristics of suddenly reversed TCs(SRTCs), which have turning angles usually approaching 180°, are statistically analyzed from 1949 to 2011 over the western North Pacific Ocean. The typical large-scale circulation patterns of SRTCs are investigated using reanalysis data and dynamical composite analysis. Results show that turnings mainly occur in low latitudes between 10°N and 20°N,and mainly west of 135°E. The majority of SRTCs reach their peak intensity at, or slightly before, the turning time and subsequently decrease at some variable rate. Specifically, SRTCs are divided into four types, each containing two groups(i.e.eight groups in total) in terms of the moving-direction changes. The moving speed of all SRTC types except the south–north type decreases to its lowest during the 24 h, corresponding to a significant reduction in the primary steering components.According to the analysis of the 13 typical flow patterns found in this study, we suggest that sudden track changes are caused by the reversal steering flow. The original balance of the background flow patterns are broken up by new systems, e.g. binary TCs or dispersion-induced anticyclones. Additionally, sudden track changes are often due to double ridge variations of the subtropical high or weakened/strengthened high pressure in the east and west, respectively.展开更多
A nuclear accident involving the leaking of radioactive pollutants occurred at the Fukushima Nuclear Power Plant in Japan,following an earthquake and subsequent tsunami on March 11,2011.Using official Japanese data on...A nuclear accident involving the leaking of radioactive pollutants occurred at the Fukushima Nuclear Power Plant in Japan,following an earthquake and subsequent tsunami on March 11,2011.Using official Japanese data on pollutant emissions during the accident,this study simulates the dispersion of nuclear pollutants.The source term of the nuclear leakage of radioactive material is designed using PM2.5as the tracer of radioactive pollutants,and the study considers dry and wet deposition processes.A coupled-model system is constructed from the air-quality model Models-3/CMAQ and the Weather Research and Forecasting atmospheric model.The transport path and distribution of radioactive pollutants over long and short distances are simulated with different model horizontal resolutions of 30 and 4 km respectively.The long-distance simulation shows that,following the Fukushima nuclear accident,under the effect of westerly winds,radioactive pollutants are transported generally towards the eastern Pacific and reach the American continent after 5 days,but their concentration is only about 10–7 times the concentration near the Fukushima Nuclear Power Plant.The time required for pollutants to reach the United States is basically consistent with measurements made in California on March 18.Because the upper westerly wind is faster than the lower westerly wind,the distribution of pollutants tilts eastward in terms of its vertical structure.The short-distance(local)highresolution simulation indicates that strong winds and precipitation associated with a cyclone can accelerate the deposition,diffusion and transport of pollutions,and local cyclonic circulation can change the transport path of pollutants,even resulting in repeated effects of pollution in some areas.Pollutants disperse to southeastern Honshu,Japan,on March 14,2011,agreeing well with the timing of local observations of increases in the absorbed dose rate.Results also show that radioactive pollutants from the Fukushima nuclear accident are mainly transported and diffuse eastward,resulting in a relatively short-term impact on the Japanese mainland even under the influence of the cyclone system.Therefore,in terms of atmospheric conditions,the location of the Fukushima Nuclear Power Plant is appropriate and could serve as a reference to site selection and protection of other nuclear facilities.展开更多
Traditional variational data assimilation(VDA) with only one regularization parameter constraint cannot produce optimal error tuning for all observations. In this paper, a new data assimilation method of "four di...Traditional variational data assimilation(VDA) with only one regularization parameter constraint cannot produce optimal error tuning for all observations. In this paper, a new data assimilation method of "four dimensional variational data assimilation(4D-Var) with multiple regularization parameters as a weak constraint(Tikh-4D-Var)" is proposed by imposing different regularization parameters for different observations. Meanwhile, a new multiple regularization parameters selection method, which is suitable for actual high-dimensional data assimilation system, is proposed based on the posterior information of 4D-Var system. Compared with the traditional single regularization parameter selection method, computation of the proposed multiple regularization parameters selection method is smaller. Based on WRF3.3.1 4D-Var data assimilation system, initialization and simulation of typhoon Chaba(2010) with the new Tikh-4D-Var method are compared with its counterpart 4D-Var to demonstrate the effectiveness of the new method. Results show that the new Tikh-4D-Var method can accelerate the convergence with less iterations. Moreover, compared with 4D-Var method, the typhoon track, intensity(including center surface pressure and maximum wind speed) and structure prediction are obviously improved with Tikh-4D-Var method for 72-h prediction. In addition, the accuracy of the observation error variances can be reflected by the multiple regularization parameters.展开更多
文摘基于中国台湾地区主持的侵台台风之飞机侦察及下投式探空仪观测实验(Dropwindsonde Observations for Typhoon Surveillance near the Taiwan Region,DOTSTAR)获得的高分辨率下投式探空仪探测资料,分析了2003年9月—2012年8月所有发生在中国台湾地区附近海域的台风型大气波导事件,遴选出一次由0920号超强台风"卢碧"引起的强台风型海上大气波导过程作为研究对象。利用欧洲中期数值预报中心(ECMWF)再分析资料(水平分辨率0.125°×0.125°),对此次波导的生成原因进行了分析;基于WRF模式比较了不同初始化方法对台风强度、尺度和周围台风型大气波导的模拟能力。结果表明,此次强台风型大气波导发生在台风环流西北侧外围的弱下沉运动区,其形成与850 hPa高度附近北方强干空气平流导致湿度随高度锐减密切相关。在数值模拟中运用台风动力初始化方法,可以有效改进台风强度、路径和尺度的模拟效果,进而有利于改善台风型大气波导尤其是波导层所在高度的模拟效果。台风外围出现的大气波导通常以悬空波导为主,模拟效果与台风螺旋雨带和内核尺度的模拟关系密切,而与台风强度和眼墙结构关系不大。中尺度数值模式WRF具有模拟台风型大气波导的能力,是研究台风型大气波导的有力手段。
基金supported by the National Public Benefit (Meteorology) Research Foundation of China (Grant No. GYHY201106004)the National Natural Science Foundation of China (Grant Nos. 41005029, 41105065 and 41230421)
文摘Variable thicknesses in the lowest half-ηmodel level (LML) are often used in atmospheric models to compute surface diagnostic fields such as surface latent and sensible heat fluxes.The effects of the LML on simulated tropical cyclone (TC)evolution were investigated in this study using the Weather Research and Forecasting (WRF) model.The results demonstrated notable influences of the LML on TC evolution when the LML was placed below 12 m.The TC intensification rate decreased progressively with a lowering of the LML,but its ultimate intensity change was relatively small.The maximum 10-m winds showed different behavior to minimum sea level pressure and azimuthally-averaged tangential winds,and thus the windpressure relationship was changed accordingly by varying the LML.The TC circulation was more contracted in association with a higher LML.Surface latent heat fluxes were enhanced greatly by elevating the LML,wherein the wind speed at the LML played a dominant role.The changes in the wind speed at the LML were dependent not only on their profile differences,but also the different heights they were taken from.Due to the enhanced surface heat fluxes,more intense latent heat release occurred in the eyewall,which boosted the storm's intensification.A higher LML tended to produce a stronger storm,and therefore the surface friction was reinforced,which in turn induced stronger boundary layer inflow together with increased diabatic heating.
文摘远海悬空波导陷获层底的位置通常与边界层浅云的云顶有很好的对应,气溶胶与边界层浅云的相互作用及其产生的辐射强迫将改变悬空波导的结构.文中利用天气预报-化学(weather research and forecasting-chemistry,WRF-Chem)模式通过设计不包含完整气溶胶-云-辐射的EXP0试验(相当于WRF模式)和包含完整气溶胶-云-辐射相互作用(即气溶胶直接和间接效应)的EXP1试验,对2016年5月观测到的一次珍贵的远海高压型超强悬空波导过程进行了模拟分析.结果表明:远海高压天气形势下,EXP1试验模拟的由气溶胶活化后形成的云滴数浓度比EXP0试验云滴数浓度预设常值(100个cm-3)偏低;当伴随边界层浅云出现时,EXP1试验模拟的波导顶高和强度较EXP0试验更接近于实测;夜间进行的3次观测位于高压中心附近的无云区,此时气溶胶的直接和间接效应均可忽略,因此两组试验模拟的差异极小.这一结果从侧面说明,在有边界层浅云出现的远海区域,包含完整气溶胶-云-辐射效应的WRF-Chem模式有利于提高悬空波导特征量的模拟效果.
基金supported by the National Natural Science Foundation of China(Grant No.41230421)the 973 project(Grant Nos.2015CB452802 and 2013CB430101)of the Ministry of Science and Technology,China
文摘Previous work showed that some tropical cyclones (TCs) in the western Pacific Ocean undergo sudden track reversal, and the onset, maintenance and decay of blocking highs (BHs) coexisted with 19 of the studied TCs with sudden track reversal. In these cases, the phase relations between the BH, the continental high (CH), the subtropical high (SH) and the suddenly reversed TCs could be classified into types A, B, C and D. Types C and D were the focal point of this follow-up study, in which Typhoon Pabuk (2007) and Lupit (2009) were employed to conduct numerical simulations. The results showed that the reversed tracks of Pabuk (2007) and Lupit (2009) could have been affected by the BH, particularly in terms of the turning location and the trend of movement after turning. Specifically, the two main features for Pabuk (2007) in the BH perturbations were the deflection of its turning point and a distinct anticlockwise rotation. Lupit (2009) deviated to the southwest and finally made landfall in the Philippines, or experienced further eastward movement, in the perturbed BH. The impact mechanisms can be attributed to the change in the vorticity field transported from the BH, leading to an intensity variation of midlatitude systems. BHs may have a positive feedback effect on the strength of the westerly trough (TR), as indicated by a weakened and strengthened TR corresponding to negative and positive BH perturbations, respectively.
基金the National Natural Science Foundation of China (No 40333025)the Open Project of Shanghai Typhoon Institute of China Meteorological Administration (No 2006STB02) in combination with the Doctoral Visit Project of Ocean University of China
文摘To study the potential effect of sea spray on the evolution of typhoons,two kinds of sea spray flux parameterization schemes developed by Andreas (2005) and Andreas and Wang (2006) and Fairall et al. (1994) respectively are incorporated into the regional atmospheric Mesoscale Model version 3.6 (MM5V3) of Pennsylvania State University/National Center for Atmospheric Research (PSU/NCAR) and the coupled atmosphere-sea spray modeling system is applied to simulate a Western Pacific super ty-phoon Ewiniar in 2006. The simulation results demonstrate that sea spray can lead to a significant increase in heat fluxes at the air-sea interface and the simulated typhoon’s intensity. Compared with the results without sea spray,the minimum sea level pressure reduces about 8hPa after taking account of sea spray by Fairall et al.’s parameterization (1994) and about 5hPa by Andreas’ (2005) and Andreas and Wang’s (2006) parameterization at the end of the model integration,while the maximum 10m wind speed increases about 17% and 15% on average,respectively,through the entire simulation time period. Taking sea spray into account also causes significant changes in Tropical Cyclone (TC) structure due to an enhancement of water vapor and heat transferred from the sea sur-face to the air; therefore,the center structure of the typhoon becomes more clearly defined and the wind speed around the typhoon eye is stronger in numerical experiments. The simulations show that different sea spray flux parameterizations make different modi-fications to the TC structure.
基金The National Natural Science Foundation of China under contract Nos 41005029,41105012 and 41105063the National Public Benefit (Meteorology) Research Foundation of China under contract No.GYHY201106004
文摘This paper proposes a rain considered geophysical model function (GMF), to be noted as GMF plus Rain. GMF plus Rain is based on the basic raidative transfer model with attenuation and scattering effects of rain on radar signal considered. Combined with the NSCAT2 GMF and the rain correction model, the GMF plus Rain model is used to retrieve the ocean wind vectors from the collocated QuikSCAT and SSM/I rain rate data for typhoon Melor. The resulting wind speed estimates of typhoon Melor show improved agreement with the wind fields derived from the best track analysis of Japan Meteorological Agency (JMA). The results imply that compared with the GMF model, the GMF plus Rain model can improve the precision of wind retrieval under the rain condition. Then, a new general algorithm of locating the eye of typhoon through the normalized radar cross section (NRCS) is proposed. The implementation of this algorithm in the ten QuikSCAT observations of typhoon Melor suggests that this algorithm is effective.
基金supported by the National Natural Science Foundation of China (Grant Nos. 41230421, 41005029 and 41105065)the National Public Benefit (Meteorology) Research Foundation of China (Grant No. GYHY201106004)
文摘Based on best track data of tropical cyclones(TCs) from the Japan Meteorological Agency, the characteristics of suddenly reversed TCs(SRTCs), which have turning angles usually approaching 180°, are statistically analyzed from 1949 to 2011 over the western North Pacific Ocean. The typical large-scale circulation patterns of SRTCs are investigated using reanalysis data and dynamical composite analysis. Results show that turnings mainly occur in low latitudes between 10°N and 20°N,and mainly west of 135°E. The majority of SRTCs reach their peak intensity at, or slightly before, the turning time and subsequently decrease at some variable rate. Specifically, SRTCs are divided into four types, each containing two groups(i.e.eight groups in total) in terms of the moving-direction changes. The moving speed of all SRTC types except the south–north type decreases to its lowest during the 24 h, corresponding to a significant reduction in the primary steering components.According to the analysis of the 13 typical flow patterns found in this study, we suggest that sudden track changes are caused by the reversal steering flow. The original balance of the background flow patterns are broken up by new systems, e.g. binary TCs or dispersion-induced anticyclones. Additionally, sudden track changes are often due to double ridge variations of the subtropical high or weakened/strengthened high pressure in the east and west, respectively.
基金supported by the National Public Benefit(Meteorology)Research Foundation of China(Grant No.GYHY201106004)the National Natural Science Foundation of China(Grant No.41005029)
文摘天气研究并且(WAVEWATCH III ) 预报(WRF ) 模特儿,普林斯顿海洋模型(POM ) ,和波浪当模特儿被用来开发 a coupled atmosphere-wave-ocean 模型,它包括 air-forcing,海洋反馈,导致波浪的混合和波浪水流相互作用包含不同物理过程。在这篇论文,台风 KAEMI (2006 ) 被检验了基于联合 atmosphere-ocean-wave 模型在海洋反应上调查风水流相互作用的效果,即,就海表面而言,在风的计算的水流强调。结果证明风水流相互作用在 10 m 弯屈的模拟上有显著影响。包含风水流相互作用的效果的模型能戏剧性地改进台风预言。风水流相互作用阻止过多的动量流动被变成上面的海洋,它贡献小得多的骚乱动能(TKE ) ,垂直扩散性,和水平移流和散开。冷却在台风开发的起始的阶段期间由风水流相互作用导致了的海表面温度(SST ) 是那么次要的台风紧张不对它很敏感。当台风到达它的山峰时,它的风能扰乱 thermocline,并且在 thermocline 下面的冷水被打气。然而,这个冷却过程被风水流相互作用削弱,当海洋反馈推迟台风的腐烂。同时,在 30 m 的深度下面的温度与一个时期显示出惯性的摆动大约 40 个小时(17 瘠癩? 敲灳湯吗?
基金supported by the Special Funds of Public Welfare of China (Grant No. GYHY201306061)the National Natural Science Foundation of China (Grant Nos. 41230421, 41105065 & 41275128)
文摘A nuclear accident involving the leaking of radioactive pollutants occurred at the Fukushima Nuclear Power Plant in Japan,following an earthquake and subsequent tsunami on March 11,2011.Using official Japanese data on pollutant emissions during the accident,this study simulates the dispersion of nuclear pollutants.The source term of the nuclear leakage of radioactive material is designed using PM2.5as the tracer of radioactive pollutants,and the study considers dry and wet deposition processes.A coupled-model system is constructed from the air-quality model Models-3/CMAQ and the Weather Research and Forecasting atmospheric model.The transport path and distribution of radioactive pollutants over long and short distances are simulated with different model horizontal resolutions of 30 and 4 km respectively.The long-distance simulation shows that,following the Fukushima nuclear accident,under the effect of westerly winds,radioactive pollutants are transported generally towards the eastern Pacific and reach the American continent after 5 days,but their concentration is only about 10–7 times the concentration near the Fukushima Nuclear Power Plant.The time required for pollutants to reach the United States is basically consistent with measurements made in California on March 18.Because the upper westerly wind is faster than the lower westerly wind,the distribution of pollutants tilts eastward in terms of its vertical structure.The short-distance(local)highresolution simulation indicates that strong winds and precipitation associated with a cyclone can accelerate the deposition,diffusion and transport of pollutions,and local cyclonic circulation can change the transport path of pollutants,even resulting in repeated effects of pollution in some areas.Pollutants disperse to southeastern Honshu,Japan,on March 14,2011,agreeing well with the timing of local observations of increases in the absorbed dose rate.Results also show that radioactive pollutants from the Fukushima nuclear accident are mainly transported and diffuse eastward,resulting in a relatively short-term impact on the Japanese mainland even under the influence of the cyclone system.Therefore,in terms of atmospheric conditions,the location of the Fukushima Nuclear Power Plant is appropriate and could serve as a reference to site selection and protection of other nuclear facilities.
基金supported by National Natural Science Foundation of China(Grants Nos.41230421,41005029,41105012,41375106 and 41105065)National Public Benefit(Meteorology)Research Foundation of China(Grant No.GYHY 201106004)
文摘Traditional variational data assimilation(VDA) with only one regularization parameter constraint cannot produce optimal error tuning for all observations. In this paper, a new data assimilation method of "four dimensional variational data assimilation(4D-Var) with multiple regularization parameters as a weak constraint(Tikh-4D-Var)" is proposed by imposing different regularization parameters for different observations. Meanwhile, a new multiple regularization parameters selection method, which is suitable for actual high-dimensional data assimilation system, is proposed based on the posterior information of 4D-Var system. Compared with the traditional single regularization parameter selection method, computation of the proposed multiple regularization parameters selection method is smaller. Based on WRF3.3.1 4D-Var data assimilation system, initialization and simulation of typhoon Chaba(2010) with the new Tikh-4D-Var method are compared with its counterpart 4D-Var to demonstrate the effectiveness of the new method. Results show that the new Tikh-4D-Var method can accelerate the convergence with less iterations. Moreover, compared with 4D-Var method, the typhoon track, intensity(including center surface pressure and maximum wind speed) and structure prediction are obviously improved with Tikh-4D-Var method for 72-h prediction. In addition, the accuracy of the observation error variances can be reflected by the multiple regularization parameters.