Wave fields of the South China Sea （SCS） from 1976 to 2005 were simulated using WAVEWATCH III by inputting high-resolution reanalysis wind field datasets assimilated from several meteorological data sources. Compari...Wave fields of the South China Sea （SCS） from 1976 to 2005 were simulated using WAVEWATCH III by inputting high-resolution reanalysis wind field datasets assimilated from several meteorological data sources. Comparisons of wave heights between WAVEWATCH III and TOPEX/Poseidon altimeter and buoy data show a good agreement. Our results show seasonal variation of wave direction as follows： 1. During the summer monsoon （April-September）, waves from south occur from April through September in the southern SCS region, which prevail taking about 40% of the time; 2. During the winter monsoon （December-March）, waves from northeast prevail throughout the SCS for 56% of the period; 3. The dominant wave direction in SCS is NE. The seasonal variation of wave height Hs in SCS shows that in spring, Hs〉l m in the central SCS region and is less than 1 m in other areas. In summer, Hs is higher than in spring. During September- November, influenced by tropical cyclones, Hs is mostly higher than 1 m. East of Hainan Island, Hs〉2 m. In winter, Hs reaches its maximum value influenced by the north-east monsoon, and heights over 2 m are found over a large part of SCS. Finally, we calculated the extreme wave parameters in SCS and found that the extreme wind speed and wave height for the 100-year return period for SCS peaked at 45 m/s and 19 m, respectively, SE of Hainan Island and decreased from north to south.展开更多
The complex [Fe(C14H14NO2)3]2H2O has been prepared by reaction of N-p-methylphenyl-3-hydroxy-2-ethyl-4-pyridinone with FeCl36H2O. A single-crystal X-ray study shows that the iron atoms lie in a trigonally distorted oc...The complex [Fe(C14H14NO2)3]2H2O has been prepared by reaction of N-p-methylphenyl-3-hydroxy-2-ethyl-4-pyridinone with FeCl36H2O. A single-crystal X-ray study shows that the iron atoms lie in a trigonally distorted octahedral environment coordinated to the hydroxy and ketone oxygen atoms of three ligands in the mer configuration Mr=773.57(C42H46N3O8Fe). The crystal is hexagonal with space group P31c; a=15.943(2), c=17.612(4)? V=3877.0(12)?, Z=4, Dc=1.325g/cm3, m=0.445mm-1, F(000)=1634, R=0.0446, wR= 0.1154 for 3085 reflections with I >2s(I). The bond lengths from iron to oxygens are 1.980(1)?for the ketone oxygens and 2.071(1)?for the hydroxy oxygens. The molecule exhibits the expected propeller shape, and the angle of the trigonal twist is 48.37. The dihedral angles are 0.5(2)?between chelate ring plane and pyridine ring plane and 71.31(7)?between pyridine ring plane and benzene ring plane. The solvent H2O(O(3) and O(4)) molecules are linked with O(2) and O(1) by hydrogen bonds with bond lengths 2.900(1) and 2.999(1)? respectively.展开更多
将基于最优插值（OI）的同化并行模块植入全谱空间的第三代海浪模式 WAVEWATCH III ver-sion3.14,建立数据同化的海浪模式预报系统,并通过实际的预报个例对同化系统进行检验。个例实验是以5°S以北的印度洋海域为目标计算区域,海面...将基于最优插值（OI）的同化并行模块植入全谱空间的第三代海浪模式 WAVEWATCH III ver-sion3.14,建立数据同化的海浪模式预报系统,并通过实际的预报个例对同化系统进行检验。个例实验是以5°S以北的印度洋海域为目标计算区域,海面风场强迫采用业务单位的中尺度天气预报模式WRF （weather research and forecast）提供的逐时海面风场预报产品。模式积分过程中连续同化2010年12月15日、16日和17日过境北印度洋的Jason-2卫星高度计沿轨有效波高（SWH）数据（需要指出的是,每次同化得到新的SWH分析场后需重构相应的二维海浪谱用于谱模式）。SWH同化分析值和无同化的对照组分别与高度计沿轨观测数据比较发现,就日平均统计来看,同化较无同化使SWH分析值的均方根误差减小约25%-50%。以 SWH同化分析场作为初始场的预报表明,同化对预报影响的时效性可延长至48-60 h。本研究目的是通过将高度计测量的SWH数据同化到海浪模式进一步提升海浪数值预报的准确度。展开更多
目的:研究龙麻金宁方对热哮大鼠气道重塑及其肺组织中蛋白激酶B(PKBm RNA)、成纤维细胞α-平滑肌肌动蛋白(α-SMA m RNA)、血小板衍生因子(PDGF)、I、III胶原蛋白表达水平的影响。方法:雄性SD大鼠,70只,随机分成以下7组:正常组、模型组...目的:研究龙麻金宁方对热哮大鼠气道重塑及其肺组织中蛋白激酶B(PKBm RNA)、成纤维细胞α-平滑肌肌动蛋白(α-SMA m RNA)、血小板衍生因子(PDGF)、I、III胶原蛋白表达水平的影响。方法:雄性SD大鼠,70只,随机分成以下7组:正常组、模型组、地塞米松组、麻杏石甘汤组以及龙麻金宁高、中、低剂量组,每组10只。在第1天和第8天,以10%卵蛋白腹腔注射致敏及细菌脂多糖(LPS)滴鼻制热(终浓度400μg·m L-1)复制大鼠热哮模型。第15天开始1%卵蛋白雾化激发,连续7 d,第21天模型复制成功,开始治疗。正常组、模型组每天给予等量蒸馏水灌服,地塞米松组、麻杏石甘汤组、龙麻金宁高、中、低剂量组按人体与大鼠体表面积换算比折算剂量灌胃,灌胃4周后解剖大鼠并取出肺组织。采用HE染色法观察肺组织的病理形态学改变;采用免疫组化法观察肺组织的中、小气道I、III胶原蛋白的阳性表达;采用酶联免疫吸附反应定量肺组织的PDGF含量;采用逆转录-聚合酶链反应以半定量测定PKBm RNA、α-SMA m RNA的表达丰度。结果:与正常组比较,模型组发生明显肺组织炎症反应和气道重塑现象,α-SMAm RNA、PKBm RNA、PDGF、I、III胶原表达水平显著升高(P<0.01);龙麻金宁高、中、低剂量治疗组与模型组比较,α-SMAm RNA、PKBm RNA、PDGF、I、III胶原表达水平显著降低(P<0.01)。结论:龙麻金宁明显减轻热哮大鼠气道炎症反应,抑制热哮大鼠肺组织中α-SMA m RNA、PKBm RNA、PDGF、I、III胶原的表达,延缓气道重塑而治疗哮喘。展开更多
Wave climate analysis and other applications for the Pacific Ocean require a reliable wave hindcast. Five source and sink term packages in the Wavewatch III model （v3.14 and v4.18） are compared and assessed in this ...Wave climate analysis and other applications for the Pacific Ocean require a reliable wave hindcast. Five source and sink term packages in the Wavewatch III model （v3.14 and v4.18） are compared and assessed in this study through comprehensive observations, including altimeter significant wave height, advanced synthetic aperture radar swell, and buoy wave parameters and spectrum. In addition to the evaluation of typically used integral parameters, the spectra partitioning method contributes to the detailed wave system and wave maturity validation. The modified performance evaluation method （PS） effectively reduces attribute numbers and facilitates the overall assessment. To avoid possible misleading results in the root mean square error-based validations, another indicator called HH （indicating the two authors） is also calculated to guarantee the consistency of the results. The widely used Tolman and Chalikov （TC） package is still generally efficient in determining the integral properties of wave spectra but is physically deficient in explaining the dissipation processes. The ST4 package performs well in overall wave parameters and significantly improves the accuracy of wave systems in the open ocean. Meanwhile, the newly published ST6 package is slightly better in determining swell energy variations. The two packages （ACC350 and BIA） obtained from Wavewatch III v3.14 exhibit large scatters at different sea states. The three most ideal packages are further examined in terms of reproducing wave- induced momentum flux from the perspective of transport. Stokes transport analysis indicates that ST4 is the closest to the NDBC-buoy-spectrum-based transport values, and TC and ST6 tend to overestimate and underestimate the transport magnitude, respectively, in swell mixed areas. This difference must be considered, particularly in air-wave-current coupling research and upper ocean analysis. The assessment results provide guidance for the selection of ST4 for use in a background Pacific Ocean hindcast for high wave climate research and China Sea swell type analysis.展开更多
In this study, we simulated typhoon waves in the shallow waters around the Zhoushan Islands using the WaveWatch-Ⅲ(WW3) model version 5.16, the latest version released by the National Oceanic and Atmospheric Administr...In this study, we simulated typhoon waves in the shallow waters around the Zhoushan Islands using the WaveWatch-Ⅲ(WW3) model version 5.16, the latest version released by the National Oceanic and Atmospheric Administration. Specifically, we used in-situ measurements to evaluate the performance of seven packages of input/dissipation source terms in the WW3 model. We forced the WW3 model by wind fields derived from a combination of the parametric Holland model and high-resolution European Center for Medium-Range Weather Forecasts(ECMWF) wind data in a 0.125? grid, herein called H-E winds. We trained the H-E winds by fitting a shape parameter B to buoy-measured observations, which resulted in a smallest root mean square error(RMSE) of 3 m s^(-1) for B, when treated as a constant 0.4. Then, we applied the seven input/dissipation terms of WW3, labelled ST1, ST2, ST2+STAB2, ST3, ST3+STAB3, ST4, and ST6, to simulate the significant wave height(SWH) up to 5 m during typhoons Fungwong and Chan-hom around the Zhoushan Islands. We then compared the SWHs of the simulated waves with those measured by the in-situ buoys. The results indicate that the simulation using ST2 performs best with an RMSE of 0.79 m for typhoon Fung-wong and an RMSE of 1.12 m for typhoon Chan-hom. Interestingly, we found the simulated SWH results to be relatively higher than those of the observations in the area between Hangzhou Bay and the Zhoushan Islands. This behavior is worthy of further investigation in the future.展开更多
We use the WAVEWATCH-III model to quantify the effect of oceanic current on typhoon-wave modeling in the East-China-Sea（ECS）.Typhoons Jelawat and Saomai in the autumn of 2000 are hindcasted.The oceanic currents in t...We use the WAVEWATCH-III model to quantify the effect of oceanic current on typhoon-wave modeling in the East-China-Sea（ECS）.Typhoons Jelawat and Saomai in the autumn of 2000 are hindcasted.The oceanic currents in the ECS are mainly constituted of Kuroshio and typhoon-generated currents.The results show distinguishable differences in wave height and wave period under the typhoon conditions.The oceanic current causes the maximum differences,of up to a 0.5 m significant wave height and a 1 s mean wave period.Comparisons between typhoons Jelawat and Saomai show the dependence of the current effect on the typhoon characteristics.展开更多
基金Supported by the South China Sea Institute of Oceanology,Chinese Academy of Sciences
文摘Wave fields of the South China Sea （SCS） from 1976 to 2005 were simulated using WAVEWATCH III by inputting high-resolution reanalysis wind field datasets assimilated from several meteorological data sources. Comparisons of wave heights between WAVEWATCH III and TOPEX/Poseidon altimeter and buoy data show a good agreement. Our results show seasonal variation of wave direction as follows： 1. During the summer monsoon （April-September）, waves from south occur from April through September in the southern SCS region, which prevail taking about 40% of the time; 2. During the winter monsoon （December-March）, waves from northeast prevail throughout the SCS for 56% of the period; 3. The dominant wave direction in SCS is NE. The seasonal variation of wave height Hs in SCS shows that in spring, Hs〉l m in the central SCS region and is less than 1 m in other areas. In summer, Hs is higher than in spring. During September- November, influenced by tropical cyclones, Hs is mostly higher than 1 m. East of Hainan Island, Hs〉2 m. In winter, Hs reaches its maximum value influenced by the north-east monsoon, and heights over 2 m are found over a large part of SCS. Finally, we calculated the extreme wave parameters in SCS and found that the extreme wind speed and wave height for the 100-year return period for SCS peaked at 45 m/s and 19 m, respectively, SE of Hainan Island and decreased from north to south.
基金the Foundation of Returning Personal from Overseas Study of Jiangsu Education Department.
文摘The complex [Fe(C14H14NO2)3]2H2O has been prepared by reaction of N-p-methylphenyl-3-hydroxy-2-ethyl-4-pyridinone with FeCl36H2O. A single-crystal X-ray study shows that the iron atoms lie in a trigonally distorted octahedral environment coordinated to the hydroxy and ketone oxygen atoms of three ligands in the mer configuration Mr=773.57(C42H46N3O8Fe). The crystal is hexagonal with space group P31c; a=15.943(2), c=17.612(4)? V=3877.0(12)?, Z=4, Dc=1.325g/cm3, m=0.445mm-1, F(000)=1634, R=0.0446, wR= 0.1154 for 3085 reflections with I >2s(I). The bond lengths from iron to oxygens are 1.980(1)?for the ketone oxygens and 2.071(1)?for the hydroxy oxygens. The molecule exhibits the expected propeller shape, and the angle of the trigonal twist is 48.37. The dihedral angles are 0.5(2)?between chelate ring plane and pyridine ring plane and 71.31(7)?between pyridine ring plane and benzene ring plane. The solvent H2O(O(3) and O(4)) molecules are linked with O(2) and O(1) by hydrogen bonds with bond lengths 2.900(1) and 2.999(1)? respectively.
文摘将基于最优插值（OI）的同化并行模块植入全谱空间的第三代海浪模式 WAVEWATCH III ver-sion3.14,建立数据同化的海浪模式预报系统,并通过实际的预报个例对同化系统进行检验。个例实验是以5°S以北的印度洋海域为目标计算区域,海面风场强迫采用业务单位的中尺度天气预报模式WRF （weather research and forecast）提供的逐时海面风场预报产品。模式积分过程中连续同化2010年12月15日、16日和17日过境北印度洋的Jason-2卫星高度计沿轨有效波高（SWH）数据（需要指出的是,每次同化得到新的SWH分析场后需重构相应的二维海浪谱用于谱模式）。SWH同化分析值和无同化的对照组分别与高度计沿轨观测数据比较发现,就日平均统计来看,同化较无同化使SWH分析值的均方根误差减小约25%-50%。以 SWH同化分析场作为初始场的预报表明,同化对预报影响的时效性可延长至48-60 h。本研究目的是通过将高度计测量的SWH数据同化到海浪模式进一步提升海浪数值预报的准确度。
基金The National High Technology Research and Development Program(863 Program) of China under contract No.2013AA122803the Strategic Priority Research Program of the Chinese Academy of Sciences under contract No.XDA11010104
文摘Wave climate analysis and other applications for the Pacific Ocean require a reliable wave hindcast. Five source and sink term packages in the Wavewatch III model （v3.14 and v4.18） are compared and assessed in this study through comprehensive observations, including altimeter significant wave height, advanced synthetic aperture radar swell, and buoy wave parameters and spectrum. In addition to the evaluation of typically used integral parameters, the spectra partitioning method contributes to the detailed wave system and wave maturity validation. The modified performance evaluation method （PS） effectively reduces attribute numbers and facilitates the overall assessment. To avoid possible misleading results in the root mean square error-based validations, another indicator called HH （indicating the two authors） is also calculated to guarantee the consistency of the results. The widely used Tolman and Chalikov （TC） package is still generally efficient in determining the integral properties of wave spectra but is physically deficient in explaining the dissipation processes. The ST4 package performs well in overall wave parameters and significantly improves the accuracy of wave systems in the open ocean. Meanwhile, the newly published ST6 package is slightly better in determining swell energy variations. The two packages （ACC350 and BIA） obtained from Wavewatch III v3.14 exhibit large scatters at different sea states. The three most ideal packages are further examined in terms of reproducing wave- induced momentum flux from the perspective of transport. Stokes transport analysis indicates that ST4 is the closest to the NDBC-buoy-spectrum-based transport values, and TC and ST6 tend to overestimate and underestimate the transport magnitude, respectively, in swell mixed areas. This difference must be considered, particularly in air-wave-current coupling research and upper ocean analysis. The assessment results provide guidance for the selection of ST4 for use in a background Pacific Ocean hindcast for high wave climate research and China Sea swell type analysis.
基金partly supported by the National Key Research and Development Program of China under contract (Nos. 2017YFA0604901, 2016YFC 1401002 and 2016YFC1402000)the National Natural Science Foundation of China under contract (Nos. 41776 183, 41606024 and 41506033)
文摘In this study, we simulated typhoon waves in the shallow waters around the Zhoushan Islands using the WaveWatch-Ⅲ(WW3) model version 5.16, the latest version released by the National Oceanic and Atmospheric Administration. Specifically, we used in-situ measurements to evaluate the performance of seven packages of input/dissipation source terms in the WW3 model. We forced the WW3 model by wind fields derived from a combination of the parametric Holland model and high-resolution European Center for Medium-Range Weather Forecasts(ECMWF) wind data in a 0.125? grid, herein called H-E winds. We trained the H-E winds by fitting a shape parameter B to buoy-measured observations, which resulted in a smallest root mean square error(RMSE) of 3 m s^(-1) for B, when treated as a constant 0.4. Then, we applied the seven input/dissipation terms of WW3, labelled ST1, ST2, ST2+STAB2, ST3, ST3+STAB3, ST4, and ST6, to simulate the significant wave height(SWH) up to 5 m during typhoons Fungwong and Chan-hom around the Zhoushan Islands. We then compared the SWHs of the simulated waves with those measured by the in-situ buoys. The results indicate that the simulation using ST2 performs best with an RMSE of 0.79 m for typhoon Fung-wong and an RMSE of 1.12 m for typhoon Chan-hom. Interestingly, we found the simulated SWH results to be relatively higher than those of the observations in the area between Hangzhou Bay and the Zhoushan Islands. This behavior is worthy of further investigation in the future.
基金Project supported by the Public Science and Technology Research Funds of Ocean (Grant No. 201105018)the Young Scientist Fund of the National Natural Science Foundation of China (Grant No. 41106019)+1 种基金the Natural Science Foundation of Jiangsu Province of China (Grant No. BK2012315)the Young Scientist Fund of State Oceanic Administration,China (Grant No. 2011258)
文摘We use the WAVEWATCH-III model to quantify the effect of oceanic current on typhoon-wave modeling in the East-China-Sea（ECS）.Typhoons Jelawat and Saomai in the autumn of 2000 are hindcasted.The oceanic currents in the ECS are mainly constituted of Kuroshio and typhoon-generated currents.The results show distinguishable differences in wave height and wave period under the typhoon conditions.The oceanic current causes the maximum differences,of up to a 0.5 m significant wave height and a 1 s mean wave period.Comparisons between typhoons Jelawat and Saomai show the dependence of the current effect on the typhoon characteristics.
