In this paper,we aim to design a practical low complexity low-density parity-check(LDPC)coded scheme to build a secure open channel and protect information from eavesdropping.To this end,we first propose a punctured L...In this paper,we aim to design a practical low complexity low-density parity-check(LDPC)coded scheme to build a secure open channel and protect information from eavesdropping.To this end,we first propose a punctured LDPC coded scheme,where the information bits in a codeword are punctured and only the parity check bits are transmitted to the receiver.We further propose a notion of check node type distribution and derive multi-edge type extrinsic information transfer functions to estimate the security performance,instead of the well-known weak metric bit error rate.We optimize the check node type distribution in terms of the signal-to-noise ratio(SNR)gap and modify the progressive edge growth algorithm to design finite-length codes.Numerical results show that our proposed scheme can achieve a lower computational complexity and a smaller security gap,compared to the existing scrambling and puncturing schemes.展开更多
To evaluate the downscaling ability with respect to tropical cyclones(TCs)near China and its sensitivity to the model physics representation,the authors performed a multi-physics ensemble simulation with the regional ...To evaluate the downscaling ability with respect to tropical cyclones(TCs)near China and its sensitivity to the model physics representation,the authors performed a multi-physics ensemble simulation with the regional Climate-Weather Research and Forecasting(CWRF)model at a 30 km resolution driven by ERA-Interim reanalysis data.The ensemble consisted of 28 integrations during 1979-2016 with varying CWRF physics configurations.Both CWRF and ERA-Interim can generally capture the seasonal cycle and interannual variation of the TC number near China,but evidently underestimate them.The CWRF downscaling and its multi-physics ensemble can notably reduce the underestimation and significantly improve the simulation of the TC occurrences.The skill enhancement is especially large in terms of the interannual variation,which is most sensitive to the cumulus scheme,followed by the boundary layer,surface and radiation schemes,but weakly sensitive to the cloud and microphysics schemes.Generally,the Noah surface scheme,CAML(CAM radiation scheme as implemented by Liang together with the diagnostic cloud cover scheme of Xu and Randall(1996))radiation scheme,prognostic cloud scheme,and Thompson microphysics scheme stand out for their better performance in simulating the interannual variation of TC number.However,the Emanuel cumulus and MYNN boundary layer schemes produce severe interannual biases.Our study provides a valuable reference for CWRF application to improve the understanding and prediction of TC activity.展开更多
This paper evaluates the skills of physical Parameterization schemes in simulating extreme rainfall events over Dar es Salaam Region, Tanzania using the Weather Research and Forecasting (WRF) model. The model skill is...This paper evaluates the skills of physical Parameterization schemes in simulating extreme rainfall events over Dar es Salaam Region, Tanzania using the Weather Research and Forecasting (WRF) model. The model skill is determined during the 21 December 2011 flooding event. Ten sensitivity experiments have been conducted using Cumulus, Convective and Planetary boundary layer schemes to find the best combination and optimize the WRF model for the study area for heavy rainfall events. Model simulation results were verified against observed data using standard statistical tests. The model simulations show encouraging and better statistical results with the combination of Kain-Fritsch cumulus parameterization scheme, Lin microphysics scheme and Asymmetric Convection Model 2 (ACM2) planetary boundary scheme than any other combinations of physical parameterization schemes over Dar es Salaam region.展开更多
使用激波捕捉法求解以数学间断作为初始条件的无黏可压缩流场时,间断结构会逐渐演变为包含多个网格节点的数值过渡区,在此过程中会产生两个平行于间断且规则分布的非物理波动。使用捕捉法计算激波流场时,流场参数应满足修正方程,但作为...使用激波捕捉法求解以数学间断作为初始条件的无黏可压缩流场时,间断结构会逐渐演变为包含多个网格节点的数值过渡区,在此过程中会产生两个平行于间断且规则分布的非物理波动。使用捕捉法计算激波流场时,流场参数应满足修正方程,但作为初始条件进行计算的初始激波满足Euler方程,两者之间的矛盾是产生初始激波诱导非物理波动的原因。鉴于激波等间断是由特征型Euler方程定义的,从该方程出发构造了一种基于特征值迎风特性的通量计算格式(upwind flux scheme based on characteristics,UFSC),并采用若干种常规守恒型通量分裂格式作为参考。数值计算结果表明,UFSC可以消除Steger-Warming、Van Leer等矢通量分裂格式的初始接触间断诱导非物理波动,还可以减小初始激波诱导扰动的幅值。在光滑流场区域,UFSC和矢通量分裂格式的计算结果相近,但是在强激波附近会出现较大的压力尖峰。为克服这一缺陷,进一步构造了在激波区域和其他区域分别采用Steger-Warming格式和UFSC格式计算的混合通量计算格式UFSC+S,可以有效抑制初始激波诱导误差,提高计算精度。展开更多
利用美国国家环境预测中心(National Centers for Environmental Prediction,NCEP)和国家大气研究中心(NCAR)联合研发的天气研究和预报模式(Weather Research and Forecasting Model,WRF),研究了不同积云对流参数化方案和微物理过程方案...利用美国国家环境预测中心(National Centers for Environmental Prediction,NCEP)和国家大气研究中心(NCAR)联合研发的天气研究和预报模式(Weather Research and Forecasting Model,WRF),研究了不同积云对流参数化方案和微物理过程方案对0514号台风"彩蝶"路径的影响。结果表明,积云对流参数化方案对台风路径影响较大,KF方案比BM方案能更好地模拟出台风路径;使用KF方案时,选择微物理方案比不选微物理方案对于台风路径有更好的模拟结果,其中,Ferrier、WSM6和Lin非常接近于实况;KF方案较好地模拟出副热带高压(简称副高)的西伸和东退的变化以及台风环流的风场分布和强度。展开更多
为了研究微物理参数化方案对珠江三角洲(简称珠三角)降水模拟的影响,利用WRF中尺度数值预报模式,在3 km模式分辨率下,在微物理方案为WSM6方案条件下,选用KF、BMJ、GD以及G3等四种积云参数化方案对2010年5月14日广东珠三角地区的一次暴...为了研究微物理参数化方案对珠江三角洲(简称珠三角)降水模拟的影响,利用WRF中尺度数值预报模式,在3 km模式分辨率下,在微物理方案为WSM6方案条件下,选用KF、BMJ、GD以及G3等四种积云参数化方案对2010年5月14日广东珠三角地区的一次暴雨过程进行了模拟试验。结果显示,KF方案对于降水带和降水量的模拟与实况较为一致。在积云参数化方案为KF条件下,分别选用Kessler、Lin et al、WSM 3、WSM5、Ferrier(New eta)和WSM6等6种微物理方案再次对这次暴雨过程进行模拟试验,模拟结果的对比分析表明:选用Lin et al微物理方案时,模式较好地模拟出了强降水雨带的位置和降水强度;而其他5种参数方案的模拟效果均不好,降水量明显偏小,雨带位置偏差较大;同时对低空急流、K指数和上升速度等物理量分析可知,Lin et al方案能较好地模拟出降水实况。展开更多
文摘In this paper,we aim to design a practical low complexity low-density parity-check(LDPC)coded scheme to build a secure open channel and protect information from eavesdropping.To this end,we first propose a punctured LDPC coded scheme,where the information bits in a codeword are punctured and only the parity check bits are transmitted to the receiver.We further propose a notion of check node type distribution and derive multi-edge type extrinsic information transfer functions to estimate the security performance,instead of the well-known weak metric bit error rate.We optimize the check node type distribution in terms of the signal-to-noise ratio(SNR)gap and modify the progressive edge growth algorithm to design finite-length codes.Numerical results show that our proposed scheme can achieve a lower computational complexity and a smaller security gap,compared to the existing scrambling and puncturing schemes.
基金supported by the National Climate Center of China under Grants 2211011816501。
文摘To evaluate the downscaling ability with respect to tropical cyclones(TCs)near China and its sensitivity to the model physics representation,the authors performed a multi-physics ensemble simulation with the regional Climate-Weather Research and Forecasting(CWRF)model at a 30 km resolution driven by ERA-Interim reanalysis data.The ensemble consisted of 28 integrations during 1979-2016 with varying CWRF physics configurations.Both CWRF and ERA-Interim can generally capture the seasonal cycle and interannual variation of the TC number near China,but evidently underestimate them.The CWRF downscaling and its multi-physics ensemble can notably reduce the underestimation and significantly improve the simulation of the TC occurrences.The skill enhancement is especially large in terms of the interannual variation,which is most sensitive to the cumulus scheme,followed by the boundary layer,surface and radiation schemes,but weakly sensitive to the cloud and microphysics schemes.Generally,the Noah surface scheme,CAML(CAM radiation scheme as implemented by Liang together with the diagnostic cloud cover scheme of Xu and Randall(1996))radiation scheme,prognostic cloud scheme,and Thompson microphysics scheme stand out for their better performance in simulating the interannual variation of TC number.However,the Emanuel cumulus and MYNN boundary layer schemes produce severe interannual biases.Our study provides a valuable reference for CWRF application to improve the understanding and prediction of TC activity.
文摘This paper evaluates the skills of physical Parameterization schemes in simulating extreme rainfall events over Dar es Salaam Region, Tanzania using the Weather Research and Forecasting (WRF) model. The model skill is determined during the 21 December 2011 flooding event. Ten sensitivity experiments have been conducted using Cumulus, Convective and Planetary boundary layer schemes to find the best combination and optimize the WRF model for the study area for heavy rainfall events. Model simulation results were verified against observed data using standard statistical tests. The model simulations show encouraging and better statistical results with the combination of Kain-Fritsch cumulus parameterization scheme, Lin microphysics scheme and Asymmetric Convection Model 2 (ACM2) planetary boundary scheme than any other combinations of physical parameterization schemes over Dar es Salaam region.
文摘使用激波捕捉法求解以数学间断作为初始条件的无黏可压缩流场时,间断结构会逐渐演变为包含多个网格节点的数值过渡区,在此过程中会产生两个平行于间断且规则分布的非物理波动。使用捕捉法计算激波流场时,流场参数应满足修正方程,但作为初始条件进行计算的初始激波满足Euler方程,两者之间的矛盾是产生初始激波诱导非物理波动的原因。鉴于激波等间断是由特征型Euler方程定义的,从该方程出发构造了一种基于特征值迎风特性的通量计算格式(upwind flux scheme based on characteristics,UFSC),并采用若干种常规守恒型通量分裂格式作为参考。数值计算结果表明,UFSC可以消除Steger-Warming、Van Leer等矢通量分裂格式的初始接触间断诱导非物理波动,还可以减小初始激波诱导扰动的幅值。在光滑流场区域,UFSC和矢通量分裂格式的计算结果相近,但是在强激波附近会出现较大的压力尖峰。为克服这一缺陷,进一步构造了在激波区域和其他区域分别采用Steger-Warming格式和UFSC格式计算的混合通量计算格式UFSC+S,可以有效抑制初始激波诱导误差,提高计算精度。
文摘利用美国国家环境预测中心(National Centers for Environmental Prediction,NCEP)和国家大气研究中心(NCAR)联合研发的天气研究和预报模式(Weather Research and Forecasting Model,WRF),研究了不同积云对流参数化方案和微物理过程方案对0514号台风"彩蝶"路径的影响。结果表明,积云对流参数化方案对台风路径影响较大,KF方案比BM方案能更好地模拟出台风路径;使用KF方案时,选择微物理方案比不选微物理方案对于台风路径有更好的模拟结果,其中,Ferrier、WSM6和Lin非常接近于实况;KF方案较好地模拟出副热带高压(简称副高)的西伸和东退的变化以及台风环流的风场分布和强度。
文摘为了研究微物理参数化方案对珠江三角洲(简称珠三角)降水模拟的影响,利用WRF中尺度数值预报模式,在3 km模式分辨率下,在微物理方案为WSM6方案条件下,选用KF、BMJ、GD以及G3等四种积云参数化方案对2010年5月14日广东珠三角地区的一次暴雨过程进行了模拟试验。结果显示,KF方案对于降水带和降水量的模拟与实况较为一致。在积云参数化方案为KF条件下,分别选用Kessler、Lin et al、WSM 3、WSM5、Ferrier(New eta)和WSM6等6种微物理方案再次对这次暴雨过程进行模拟试验,模拟结果的对比分析表明:选用Lin et al微物理方案时,模式较好地模拟出了强降水雨带的位置和降水强度;而其他5种参数方案的模拟效果均不好,降水量明显偏小,雨带位置偏差较大;同时对低空急流、K指数和上升速度等物理量分析可知,Lin et al方案能较好地模拟出降水实况。
