007413基金（睿远成长价值混合基金007119）
内容导航：
Q1：张绍东的论文著作
(1) Zhang, S. D., F. Yi, C. M. Huang, K. M. Huang, Q. Gan, Y. H. Zhang and Y. Gong (2013), Latitudinal and altitudinal variability of lower atmospheric inertial gravity waves revealed by U.S. radiosonde data, J. Geophys. Res. Atmos., 118, 2197-2206, doi:10.1002/jgrd.50623. （影响因子：3.441）
(2) Gong, Y., Q. Zhou, and S. D. Zhang (2013), Atmospheric tides in the low latitude E- and F- region and their response to a sudden stratospheric warming in January 2010, J. Geophys. Res. Space Physics, 118, doi:10.1002/2013JA019248.（影响因子：3.441）
(3) *Huang, K. M., A. Z. Liu, X. Lu, Z. Li, Q. Gan, Y. Gong, C. M. Huang, F. Yi and S. D. Zhang (2013), Nonlinear coupling between quasi two-day wave and tides based on meteor radar observations at Maui, Journal of Geophysical Research, 118, doi:10.1002/jgrd.50872. (影响因子：3.441）
(4) Gong, Y., Q. Zhou, S. D. Zhang, N. Aponte, M. Sulzer, and S. Gonzalez (2013), The F-region and topside ionosphere response to a strong geomagnetic storm at Arecibo, Journal of Geophysical Research, 118, doi:10.1002/jgra.50502. (影响因子：3.441）
(5) *Huang, K. M., S. D. Zhang, F. Yi, C. M. Huang, Q. Gan, Y. Gong, and Y. H. Zhang (2013), Third-order resonant interaction of atmospheric gravity waves, Journal of Geophysical Research, 118, 2197-2206, doi:10.1002/jgrd.50252. （影响因子：3.441）
(6) Zhang, S. D., F. Yi, C. M. Huang and K. M. Huang (2012), High vertical resolution analyses of gravity waves and turbulence at a mid-latitude station, Journal of Geophysical Research, 117, D02103, doi:10.1029/2011JD016587. （影响因子：3.441）
(7) *Gan, Q., S. D. Zhang and F. Yi (2012), TIMED/SABER observations of lower mesospheric inversion layers at low and middle latitudes, Journal of Geophysical Research, 117, D07109, doi:10.1029/2012JD017455. （影响因子：3.441）
(8) *Huang，C. M., S. D. Zhang, Q. Zhou, F. Yi and K. M. Huang (2012), Atmospheric waves and their interactions in the thermospheric neutral wind as observed by the Arecibo incoherent scatter radar, Journal of Geophysical Research, 113, D02102, doi:10.1029/2012JD018241. （影响因子：3.441）
(9) Gong, Y., Q. Zhou, S. D. Zhang, N. Aponte, M. Sulzer and S. Gonzalez (2012)，Midnight ionosphere collapse at Arecibo and its relationship to the neutral wind, electric field, and ambipolar diffusion，Journal of Geophysical Research, 117, A08332, doi:10.1029/2012JA017530. （影响因子：3.441）
(10) *Huang, K. M., S. D. Zhang and F. Yi (2010), Reflection and transmission of atmospheric gravity waves in a stably sheared horizontal wind field, Journal of Geophysical Research, 115, D16103, doi:10.1029/2009JD012687. （影响因子：3.441）
(11) Yi, F., C. M. Yu, S. D. Zhang et al. (2009), Seasonal variations of the nocturnal mesospheric Na and Fe layers at 30oN, Journal of Geophysical Research, 114, D01301, doi:10.1029/2008JD010344. （影响因子：3.441）
(12) S. D. Zhang and F. Yi (2008), A numerical study on the response of wave number spectra of atmospheric gravity waves to lower atmospheric forcing, Journal of Geophysical Research, 113, D02102, doi:10.1029/2007JD008957. （影响因子：3.441）
(13) *Huang, K. M., S. D. Zhang, and F. Yi (2008), Propagation and reflection of gravity waves in a meridionally sheared wind field, Journal of Geophysical Research, 113, D09106, doi:10.1029/2007JD008877. （影响因子：3.441）
(14) Yi, F., S. D. Zhang et al. (2008), Some ubiquitous features of the mesospheric Fe and Na layer borders from simultaneous and common-volume Fe and Na lidar observations, Journal of Geophysical Research, 113, A04S91, doi:10.1029/2007JA012632. （影响因子：3.441）
(15) Zhang, S. D. and F. Yi (2007), Latitudinal and seasonal variations of inertial gravity wave activity in the lower atmosphere over central China, Journal of Geophysical Research, 112, D05109, doi:10.1029/2006JD007487. （影响因子：3.441）
(16) *Huang, K. M., S. D. Zhang and F. Yi (2007), A numerical study on the nonresonant interaction of gravity waves in a compressible atmosphere, Journal of Geophysical Research, 112, D11115, doi:10.1029/2006JD007373. （影响因子：3.441）
(17) Yi, F., S. D. Zhang, et al. (2007), Simultaneous observations of sporadic Fe and Na layers by two closely-colocated resonance fluorescence lidars in Wuhan (30.5oN, 114.4oE), Journal of Geophysical Research, 112, D04303, doi:10.1029/2006JD007413. （影响因子：3.441）
(18) Zhang, S. D. and F. Yi (2004), A numerical study on global study on global propagations and amplitude growths of large scale gravity wave packets, Journal of Geophysical Research, 109, D07106, Doi:10.1029/2003JD004429. （影响因子：3.441）
(19) Zhang, S. D. and F. Yi (2004), A numerical study on the propagation and evolution of resonant interacting gravity waves, Journal of Geophysical Research, 109, D24107, Doi:10.1029/2004JD004822. （影响因子：3.441）
(20) Zhang, S. D. and F. Yi (2002), A numerical study of propagation characteristics of gravity-wave packets propagating in a dissipative atmosphere, Journal of Geophysical Research, 107(D14), 14-1-14-9. （影响因子：3.441）
(21) Zhang, S. D. and F. Yi (1999), A numerical study of nonlinear propagation of a gravity-wave-packet in compressible atmosphere, Journal of Geophysical Research, 104, D12, 14261-14270. （影响因子：3.441）
(22) *Huang, K. M., S. D. Zhang, and F. Yi (2009), Gravity wave excitation through resonant interaction in a compressible atmosphere, Geophysical Research Letters, 36, L01803, doi:10.1029/2008GL035575. （影响因子：3.792）
(23) Yi, F., S. D. Zhang et al. (2002) Zeng, Yujin He, Xianchang Yue, Jinbo Liu, Hongfang Lu, Donghui, Xiong, Lidar observations of sporadic Na layers over Wuhan (30.5oN, 114.4oE), Geophysical Research Letters, 29(9), 59-1-59-4.（影响因子：3.792）
(24) *Zhang, Y. H., S. D. Zhang, and D. J. Seidel (2013), Trends in Planetary Boundary Layer Height over Europe, Journal of Climate, 26, 10071-10076, DOI: 10.1175/JCLI-D-13-00108.1. （影响因子：4.362）
(25) *Huang, K. M., A. Z. Liu, S. D. Zhang, F. Yi, C. M. Huang, Q. Gan, Y. Gong, and Y. H. Zhang (2013), A strong nonlinear interaction event between 16-day wave and diurnal tide from meteor radar observations, Annales Geophysicae, 31, 2039-2048.（影响因子：1.757）
(26) *Huang, C. M., S. D. Zhang, F. Yi, K. M. Huang, Q. Gan, Y. H. Zhang and Y. Gong (2013), Frequency variations of gravity waves interacting with a time-varying tide, Annales Geophysicae, 31, 1731-1743. （影响因子：1.757）
(27) *Huang, Y. Y., S. D. Zhang, F. Yi, C. M. Huang, K. M. Huang, Q. Gan, Y. Gong (2013), Global climatological variability of quasi-two-day waves revealed by SABER/TIMED observations, Annales Geophysicae, 31, 1061-1075. （影响因子：1.757）
(28) *Huang, K. M., A. Z. Liu, S. D. Zhang, F. Yi and Z. H. Li (2012), Spectral energy transfer of atmospheric gravity waves through sum and difference nonlinear interactions, Annales Geophysicae, 30, 303-315. （影响因子：1.757）
(29) Wang, R., S. D. Zhang, H. G. Yang and K. M. Huang (2012), Characteristics of mid-latitude planetary waves in the lower atmosphere derived from radiosonde data, Annales Geophysicae, 30, 1463-1477. （影响因子：1.757）
(30) *Zhang, Y. H., S. D. Zhang, F. Yi and Z. Y. Chen (2011), Statistics of lower tropospheric inversions over the continental United States, Annales Geophysicae, 29, 401-410. （影响因子：1.757）
(31) Zhang, S. D., F. Yi, C. M. Huang and Q. Zhou (2010), Latitudinal and seasonal variations of lower atmospheric inertial gravity wave energy revealed by US radiosonde data, Annales Geophysicae, 28, 1065-1074. （影响因子：1.757）
(32) *Huang, C. M., S. D. Zhang and F. Yi (2009), Intensive radiosonde observations of the diurnal tide and planetary waves in the lower atmosphere over Yichang (111o18’E, 30o42’N), China, Annales Geophysicae, 27, 1079-1095. （影响因子：1.757）
(33) Zhang, S. D., F. Yi, C. M. Huang and Z. Y. Chen (2008), Intensive radiosonde observations of gravity waves in the lower atmosphere over Yichang (111o18’E, 30o42’N), China, Annales Geophysicae, 26, 2005-2018. （影响因子：1.757）
(34) Zhang, S. D., C. M. Huang and F. Yi (2006), Radiosonde observations of vertical wavenumber spectra for gravity waves in the lower atmosphere over central China. Annales Geophysicae, 24, 3257-3265. （影响因子：1.757）
(35) *Huang, C. M, S. D. Zhang and F. Yi (2006), A numerical study on the impact of nonlinear interactions on the amplitude of the migrating semidiurnal tide, Annales Geophysicae, 24, 3241-3256. （影响因子：1.757）
(36) Zhang, S. D. and F. Yi (2005), A statistical study of gravity waves from radiosonde observations at Wuhan (30oN, 114oE), China. Annales Geophysicae, 23, 665-673. （影响因子：1.757）
(37) Zhang, S. D., F. Yi and J. F. Wang (2000), The nonlinear effects on the characteristics of gravity-wave packets: dispersion and polarization relations，Annales Geophysicae，18(10), 1316-1324. （影响因子：1.757）
(38) Yi, F., S. D. Zhang, et al. (2013), Simultaneous and common-volume three-lidar observations of sporadic metal layers in the mesopause region, Journal of Atmospheric and Solar-Terrestrial Physics, 102, 172-184. （影响因子：1.671）
(39) Huang, K. M., S. D. Zhang, and F. Yi (2011), Atmospheric gravity wave excitation through sum nonresonant interaction, Journal of Atmospheric and Solar-Terrestrial Physics, 73, 2429-2436.（影响因子：1.671）
(40) *Zhang, Y. H., S. D. Zhang and F. Yi (2009), Intensive radiosonde observations of lower tropospheric inversion layers over Yichang (111o18’E, 30o42’N), China, Journal of Atmospheric and Solar-Terrestrial Physics, 71, 180-190.（影响因子：1.671）
(41) *Huang, C. M., S. D. Zhang and F. Yi (2007), A numerical study on the impact of nonlinearity on the amplitude of the migrating diurnal tide, Journal of Atmospheric and Solar-Terrestrial Physics, 69, 631-648. （影响因子：1.671）
(42) Zhang, S. D., F. Yi and X. Hu (2004), MF radar observation of mean wind and tides of winter mesopause (80–98 km) region over Wuhan (30oN，114oE), Journal of Atmospheric and Solar-Terrestrial Physics, 66(1), 15-25. （影响因子：1.671）
(43) *Huang, C. M., S. D. Zhang, and F. Yi (2007), A numerical study on amplitude characteristics of the terdiurnal excited by nonlinear interaction between the diurnal and semidiurnal tides. Earth Planet and Space, 59, 183-191. （影响因子：1.025）
(44) Huang, K. M., S. D. Zhang, F. Yi and Z. Y. Chen (2009), Simulation of the equatorial quasi-biennial oscillation based on the parameterizatoin with a continuous spectrum of gravity waves, Chinese Science Bulletin, 53(17), 1940-1948. （影响因子：1.243）
(45) *Huang, C. M., S. D. Zhang and F. Yi (2005), A numerical study on nonlinear propagation and short-term variability of the migrating diurnal and semidiurnal tides, Chinese Science Bulletin, 50(17), 1940-1948. （影响因子：1.243）
(46) Huang, C. M, S. D. Zhang and X. Chen X. A topographic parameter inversion method based on laser altimetry, Sci. China Ser E-Tech Sci., 55(5), 1273-1280. （影响因子：1.243）
(47) Huang, K. M., S. D. Zhang and F. Yi (2012), A numerical study on match relationships of gravity waves in nonlinear interactions, Sci. China. （影响因子：1.243）
(48) Liu, F. C., F. Yi, J. Y. Jia, Y. P. Zhang, S. D. Zhang, C. M. Yu and Y. Tan (2012), High resolution full-spectrum water Raman lidar, Sci. China Ser E-Tech Sci., 55(5), 1224-1229. （影响因子：1.243）
(49) *Wang, R., S. D. Zhang and F. Yi (2010), Fan, Radiosonde observations of high-latitude planetary waves in the lower atmosphere, Sci. China, (40), 5, 603-617.（影响因子：1.243）
(50) *Ma, L. M., S. D. Zhang, and F. Yi (2012), Radiosonde observations of lower atmospheric gravity wave momentum flux spectra at a single mid-latitude station, Chinese Journal of Geophysics, (in Chinese), 55(10). 3194-3202, DOI: 10.6038/j.issn.00001-5733.2012.10.002.（影响因子：0.749）
(51) *Cao, W. X., S. D. Zhang, F. Yi, C. M. Huang (2012), Variation of the mesopause observed by SABER/TIMED satellite, Chinese Journal of Geophysics, (in Chinese), 55(8). 2489-2497, DOI: 10.6038/j.issn.00001-5733.2012.08.001.（影响因子：0.749）
(52) Zhong, S., F. Yi, and S. D. Zhang (2012). A new method for inversion of atmospheric temperature and aerosol backscatter coefficient using pure rotational Raman spectrum. Chinese Journal of Geophysics, (in Chinese), 55(11): 3527-3533,doi: 10.6038/j.issn.0001-5733.2012.11.002. （影响因子：0.749）
(53) *Ding, X., S. D. Zhang and F. Yi (2011), A numerical simulation on gravity waves generated by thermal source and their influence on mean flow. Chinese Journal of Geophysics, (in Chinese), 54(7). 1701-1710, DOI: 10.3969/j.issn.00001-5733.2011.07.0002.（影响因子：0.749）
(54) Li, J. and S. D. Zhang (2010), Wave mode analyses of gravity waves propagating in the mesospheric thermal duct, Chinese Journal of Geophysics, 53 (2): 237-246.（影响因子：0.749）
(55) *Hang, K. M., S. D. Zhang, and F. Yi (2007), A numerical study on gravity wave excited through nonresonant interaction, Chinese Journal of Geophysics, 50(1), 24-33.（影响因子：0.749）
(56) *Li, J., S. D. Zhang and F. Yi (2007), A numerical simulation on gravity waves propagation in mesospheric thermal duct, Chinese Journal of Geophysics, 50(4), 1030-1039.（影响因子：0.749）
(57) Zhang, S. D., F. Yi, J. F. Wang and D. H. Xiong (2001), A numerical study on saturation mechanism of gravity wave in mesosphere, Chinese Journal of Geophysics, 44(4):454-460.（影响因子：0.749）
(58) Zhang, S. D. and F. Yi (1999), Breaking of a upward propagating gravity wave packet, Chinese Journal of Geophysics, 42(3), 289-295.（影响因子：0.749）
Q2：请问成都哪里有山？
四川盆地，成都平原。。。成都四周全是山。。。。。。。。青城山咯，很近，不是前山跟后山，还有一座小的，足够锻炼了，前些年经常去，爬到进山收费处了我们就返程了。。
Q3：中国黄金金店回收黄金价格
合约开盘价最高价最低价收盘价涨跌（元）涨跌幅加权平均价成交量成交金额持仓量交收量Au9995 313.50313.85313.00313.460.480.002313.353,156988,934,140.00Au9999 314.50314.50313.00313.62-0.33-0.001313.413,2571,020,808,790.00Au100g315.00315.00313.50314.060.960.003314.26105.233,060,262.00Au(T+D)313.50314.00312.60313.140.350.001313.2315,4664,844,564,160.00108,7364,566 Pt9995 363.00365.00361.00364.003.300.009363.59418151,983,000.00Ag(T+D)7361.007413.007309.007410.0047.000.0067365.00710,5405,233,219,208.002,158,3384,740 注:此表的数据由6月27日的21:00至2:30和6月28日的9:00至11:30、13:30至15:30的交易形成。黄金回收价格是以上今天的交易所价格，金店回收价是当天价减去5-10元手续费或差价
Q4：华夏行业基金买的什么股票
上网查一下
Q5：007119基金有没有C端？
你好，没有C端的。
Q6：001416基金净值查询今天
截止2019年12月11日，001416基金（嘉实事件驱动股票型证券投资基金）单位净值是0.7990 ( -0.25% )。
嘉实事件驱动股票型证券投资基金是嘉实基金发行的一个股票型的基金理财产品。
以下是最近半个月001416基金历史净值（供参考）：
扩展资料：
001416基金（嘉实事件驱动股票型证券投资基金）基本情况介绍：
一、投资范围
本基金投资于依法发行或上市的股票、债券等金融工具及法律法规或中国证监会允许基金投资的其他金融工具。
具体包括：股票（包含中小板、创业板及其他依法发行、上市的股票），股指期货、权证，债券（国债、金融债、企业（公司）债、次级债、可转换债券（含分离交易可转债）、可交换公司债券、央行票据、短期融资券、超短期融资券、中期票据、中小企业私募债等）、资产支持证券、债券回购、银行存款等固定收益类资产以及现金,以及法律法规或中国证监会允许基金投资的其他金融工具（但须符合中国证监会的相关规定）。
二、分红政策
在符合有关基金分红条件的前提下，本基金可以进行收益分配，本基金每年收益分配次数最多为12次，每份基金份额每次收益分配比例不得低于收益分配基准日每份基金份额可供分配利润的20%，若《基金合同》生效不满3个月可不进行收益分配；
本基金收益分配方式分两种：现金分红与红利再投资，投资者可选择现金红利或将现金红利自动转为基金份额进行再投资；若投资者不选择，本基金默认的收益分配方式是现金分红；
基金收益分配后基金份额净值不能低于面值，即基金收益分配基准日的基金份额净值减去每单位基金份额收益分配金额后不能低于面值；
每一基金份额享有同等分配权。
三、风险收益特征
本基金为股票型证券投资基金，属于较高预期风险和预期收益的证券投资基金品种，其预期风险和预期收益高于混合型基金、债券型基金和货币市场基金。
参考资料来源：
百度百科--嘉实事件驱动股票型证券投资基金
嘉实官网--旗下基金--嘉实事件驱动股票
Q7：007119基金今天为什么不能赎出？
顶顶7119基金今天为什么不能卖出？他可能是今天的交易停盘。但是公司有洞大的决定或者是，某事动大的事情所他的交易停盘。
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