The spring persistent rains（SPR）over southeastern China（SEC）are a unique synoptic and climatic phenomenon in East Asia.A former study has found that the southwesterly flow which lies on the southeastern flank of t...The spring persistent rains（SPR）over southeastern China（SEC）are a unique synoptic and climatic phenomenon in East Asia.A former study has found that the southwesterly flow which lies on the southeastern flank of the Tibetan Plateau（TP）is one of the deflected westerly flows of the TP,and it is suggested to be the direct climatic cause of SPR.This study found that the southwesterly flow is also highly correlated with the sensible heating of the southeastern TP in interannual variability,in addition to having a high correlation in seasonal variability.These facts suggest that the thermal forcing of the TP is another important climatic cause of SPR.Numerical sensitivity experiments further prove that the mechanical and thermal forcings of the TP are the climatic causes of the formation of the SPR.On the other hand,the Nanling Mountains and Wuyi Mountains（NWM）over southeastern China not only increase the SPR precipitation amount evidently,but also make the SPR rain belt move to the south by blocking the strong southwesterly flow.展开更多
Sensitivity analysis of composite laminated plates with bonding imperfection is carried out based on the radial point interpolation method （RPIM） in a Hamilton system. A set of hybrid governing equations of response...Sensitivity analysis of composite laminated plates with bonding imperfection is carried out based on the radial point interpolation method （RPIM） in a Hamilton system. A set of hybrid governing equations of response and sensitivity quantities is reduced using the spring-layer model and the modified Hellinger-Reissner （H-R） variational principle. The analytical method （AM）, the semi-analytical method （SAM）, and the finite difference method （FDM） are used for sensitivity analysis based on the reduced set of hybrid governing equations. A major advantage of the hybrid governing equations is that the convolution algorithm is avoided in sensitivity analysis. In addition, sensitivity analysis using this set of hybrid governing equations can obtain response values and sensitivity coefficients simultaneously, and accounts for bonding imperfection of composite laminated plates.展开更多
为有效识别基于APSIM模型籽粒生长参数中春小麦产量敏感性参数,快速并准确的估算当地模型参数。使用甘肃省定西市安定区凤翔镇安家沟村1971—2018年的气象数据和2000—2018年旱地春小麦大田试验数据,并利用EFAST方法对进行了5个增温梯...为有效识别基于APSIM模型籽粒生长参数中春小麦产量敏感性参数,快速并准确的估算当地模型参数。使用甘肃省定西市安定区凤翔镇安家沟村1971—2018年的气象数据和2000—2018年旱地春小麦大田试验数据,并利用EFAST方法对进行了5个增温梯度(0℃、0.5℃、1.0℃、1.5℃和2.0℃)下32个模型参数进行敏感性分析。粒子群算法对各个增温条件下均敏感的参数进行优化验证。结果表明:不同温度变化梯度下,对旱地春小麦产量影响最大的籽粒生长模型参数有9个,分别为消光系数、每克茎籽粒数量、穗粒数、单株最大籽粒质量、灌浆到成熟积温、出苗到拔节积温、株高、最大比叶面积和光合叶片老化的水分胁迫斜率。并且对产量敏感性强度有着显著的差异,其中消光系数和每克茎籽粒数量是对春小麦产量影响最大的参数,其他参数在不同温度下对春小麦产量的敏感性顺序存在差异。利用粒子群算法针对这9个参数进行优化,相较于优化前,优化后的春小麦产量、开花期和灌浆期籽粒干物质的均方根误差、归一化均方根误差和模型有效性指数均得到了显著改善,参数优化后开花期、灌浆期、成熟期产量的均方根误差平均值分别由13.50 kg hm-2减小到5.99 kg hm-2、183.17 kg hm-2减小到69.44 kg hm-2、141.69 kg hm-2减小到48.51 kg hm-2,归一化均方根误差平均值分别由4.94%减小到2.19%、10.92%减小到4.65%、8.39%减小到2.87%,模型有效性指数平均值分别由0.894提高到0.979、0.893提高到0.981、0.898提高到0.988。优化后的参数有效地提高了模型的预测精度。此研究为APSIM模型在当地应用和模型参数校准提供了科学依据。展开更多
The spring persistent rains （SPR） over southeastern China （SEC） is a synoptic and climatic phenomenon that is unique in East Asia. Sufficient evidence proves that it results from the mechanical and thermal effects...The spring persistent rains （SPR） over southeastern China （SEC） is a synoptic and climatic phenomenon that is unique in East Asia. Sufficient evidence proves that it results from the mechanical and thermal effects of the giant Tibetan Plateau （TP）, but its temporal span and spatial distribution are not clear at present. A climatological analysis of the NCEP/NCAR circulation and sensible heat data shows that at the 13th pentad of the solar year （lst pentad of March） there are remarkable increases in the sensible heating over the main and southeastern part of the TP, the southwesterly velocity over the southeastern flank of the TP and SEC, and rainfall over SEC, indicating the onset of the SPR. However, after the 27th pentad of the solar year （3rd pentad of May）, these variables, except for the sensible heating over the main part of the TP, decrease rapidly. The ridge line of the subtropical high in the mid-low troposphere over the South China Sea （SCS） slopes northward to the SCS and the SCS monsoon instead of southward as before breaks out, indicating the end The rain belt center over SEC shifts of the SPR. Hence, it is reasonable to define the SPR temporal span from the 13th to 27th pentad of the solar year. Data analysis and numerical sensitivity experiments show that, although the warm and cold airs converge at about 30°N in the SPR period, the distribution and intensity of the SPR rain belt are obviously influenced by the topography of the Nanling and Wuyi Mountains （NWM）. The mountains can block and lift cold and warm airs, strengthening frontogenesis and rainfall. As a result, the axis of the SPR rain belt is superposed over that of the mountain range. Accordingly, the spatial distribution of the SPR extends over most of the SEC, more specifically, to the south of the middle and lower reaches of the Yangtze River （30°N）, and to the east of 110°E.展开更多
基金support of the Chinese National 973 Program(Grant No.2006CB403600)the National Natural Science Foundation of China(NSFC)Project Nos.40875034,40810059005,40821092,and 40523001
文摘The spring persistent rains（SPR）over southeastern China（SEC）are a unique synoptic and climatic phenomenon in East Asia.A former study has found that the southwesterly flow which lies on the southeastern flank of the Tibetan Plateau（TP）is one of the deflected westerly flows of the TP,and it is suggested to be the direct climatic cause of SPR.This study found that the southwesterly flow is also highly correlated with the sensible heating of the southeastern TP in interannual variability,in addition to having a high correlation in seasonal variability.These facts suggest that the thermal forcing of the TP is another important climatic cause of SPR.Numerical sensitivity experiments further prove that the mechanical and thermal forcings of the TP are the climatic causes of the formation of the SPR.On the other hand,the Nanling Mountains and Wuyi Mountains（NWM）over southeastern China not only increase the SPR precipitation amount evidently,but also make the SPR rain belt move to the south by blocking the strong southwesterly flow.
基金Project supported by the National Natural Science Foundation of China (No. 60979001)the Major Project of Civil Aviation University of China (No. CAUC2009ZD0101)
文摘Sensitivity analysis of composite laminated plates with bonding imperfection is carried out based on the radial point interpolation method （RPIM） in a Hamilton system. A set of hybrid governing equations of response and sensitivity quantities is reduced using the spring-layer model and the modified Hellinger-Reissner （H-R） variational principle. The analytical method （AM）, the semi-analytical method （SAM）, and the finite difference method （FDM） are used for sensitivity analysis based on the reduced set of hybrid governing equations. A major advantage of the hybrid governing equations is that the convolution algorithm is avoided in sensitivity analysis. In addition, sensitivity analysis using this set of hybrid governing equations can obtain response values and sensitivity coefficients simultaneously, and accounts for bonding imperfection of composite laminated plates.
文摘为有效识别基于APSIM模型籽粒生长参数中春小麦产量敏感性参数,快速并准确的估算当地模型参数。使用甘肃省定西市安定区凤翔镇安家沟村1971—2018年的气象数据和2000—2018年旱地春小麦大田试验数据,并利用EFAST方法对进行了5个增温梯度(0℃、0.5℃、1.0℃、1.5℃和2.0℃)下32个模型参数进行敏感性分析。粒子群算法对各个增温条件下均敏感的参数进行优化验证。结果表明:不同温度变化梯度下,对旱地春小麦产量影响最大的籽粒生长模型参数有9个,分别为消光系数、每克茎籽粒数量、穗粒数、单株最大籽粒质量、灌浆到成熟积温、出苗到拔节积温、株高、最大比叶面积和光合叶片老化的水分胁迫斜率。并且对产量敏感性强度有着显著的差异,其中消光系数和每克茎籽粒数量是对春小麦产量影响最大的参数,其他参数在不同温度下对春小麦产量的敏感性顺序存在差异。利用粒子群算法针对这9个参数进行优化,相较于优化前,优化后的春小麦产量、开花期和灌浆期籽粒干物质的均方根误差、归一化均方根误差和模型有效性指数均得到了显著改善,参数优化后开花期、灌浆期、成熟期产量的均方根误差平均值分别由13.50 kg hm-2减小到5.99 kg hm-2、183.17 kg hm-2减小到69.44 kg hm-2、141.69 kg hm-2减小到48.51 kg hm-2,归一化均方根误差平均值分别由4.94%减小到2.19%、10.92%减小到4.65%、8.39%减小到2.87%,模型有效性指数平均值分别由0.894提高到0.979、0.893提高到0.981、0.898提高到0.988。优化后的参数有效地提高了模型的预测精度。此研究为APSIM模型在当地应用和模型参数校准提供了科学依据。
基金Supported by the National "973" program under Grant No.2006CB403600the National Natural Science Foundation of China under Grant Nos.40475027,40220503,and 40523001
文摘The spring persistent rains （SPR） over southeastern China （SEC） is a synoptic and climatic phenomenon that is unique in East Asia. Sufficient evidence proves that it results from the mechanical and thermal effects of the giant Tibetan Plateau （TP）, but its temporal span and spatial distribution are not clear at present. A climatological analysis of the NCEP/NCAR circulation and sensible heat data shows that at the 13th pentad of the solar year （lst pentad of March） there are remarkable increases in the sensible heating over the main and southeastern part of the TP, the southwesterly velocity over the southeastern flank of the TP and SEC, and rainfall over SEC, indicating the onset of the SPR. However, after the 27th pentad of the solar year （3rd pentad of May）, these variables, except for the sensible heating over the main part of the TP, decrease rapidly. The ridge line of the subtropical high in the mid-low troposphere over the South China Sea （SCS） slopes northward to the SCS and the SCS monsoon instead of southward as before breaks out, indicating the end The rain belt center over SEC shifts of the SPR. Hence, it is reasonable to define the SPR temporal span from the 13th to 27th pentad of the solar year. Data analysis and numerical sensitivity experiments show that, although the warm and cold airs converge at about 30°N in the SPR period, the distribution and intensity of the SPR rain belt are obviously influenced by the topography of the Nanling and Wuyi Mountains （NWM）. The mountains can block and lift cold and warm airs, strengthening frontogenesis and rainfall. As a result, the axis of the SPR rain belt is superposed over that of the mountain range. Accordingly, the spatial distribution of the SPR extends over most of the SEC, more specifically, to the south of the middle and lower reaches of the Yangtze River （30°N）, and to the east of 110°E.
