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| 1 | The seasonal variations in the significant wave height and sea surface wind speed of the China's seas显示文摘Long-term variations in a sea surface wind speed(WS) and a significant wave height(SWH) are associated with the global climate change, the prevention and mitigation of natural disasters, and an ocean resource exploitation,and other activities. The seasonal characteristics of the long-term trends in China's seas WS and SWH are determined based on 24 a(1988–2011) cross-calibrated, multi-platform(CCMP) wind data and 24 a hindcast wave data obtained with the WAVEWATCH-III(WW3) wave model forced by CCMP wind data. The results show the following.(1) For the past 24 a, the China's WS and SWH exhibit a significant increasing trend as a whole, of3.38 cm/(s·a) in the WS, 1.3 cm/a in the SWH.(2) As a whole, the increasing trend of the China's seas WS and SWH is strongest in March-April-May(MAM) and December-January-February(DJF), followed by June-July-August(JJA), and smallest in September-October-November(SON).(3) The areal extent of significant increases in the WS was largest in MAM, while the area decreased in JJA and DJF; the smallest area was apparent in SON. In contrast to the WS, almost all of China's seas exhibited a significant increase in SWH in MAM and DJF; the range was slightly smaller in JJA and SON. The WS and SWH in the Bohai Sea, the Yellow Sea, East China Sea, the Tsushima Strait, the Taiwan Strait, the northern South China Sea, the Beibu Gulf, and the Gulf of Thailand exhibited a significant increase in all seasons.(4) The variations in China's seas SWH and WS depended on the season. The areas with a strong increase usually appeared in DJF. | ZHENG Chongwei PAN Jing TAN Yanke GAO Zhansheng RUI Zhenfeng CHEN Chaohui | 2015 | Acta Oceanologica Sinica2015，34，9： | 5 |
| 2 | The Interdecadal Changes of South Pacific Sea Surface Temperature in the Mid-1990s and Their Connections with ENSO显示文摘The characteristic changes of South Pacific sea surface temperature anomalies(SSTAs) for the period January 1979 to December 2011, during which the 1990s Pacific pan-decadal variability(PDV) interdecadal regime shifts occurred, were examined. Empirical Orthogonal Function(EOF) analysis was applied to the monthly mean SSTA for two sub-periods: January 1979 to December 1994(P1) and January 1996 to December 2011(P2). Both the spatial and temporal features of the leading EOF mode for P1 and P2 showed a remarkable difference. The spatial structure of the leading EOF changed from a tripolar pattern for P1(EOF-P1) to a dipole-like pattern for P2(EOF-P2). Besides, EOF-P1(EOF-P2) had significant spectral peaks at 4.6 yr(2.7 yr). EOF-P2 not only had a closer association with El Nin o-Southern Oscillation(ENSO), but also showed a faster response to ENSO than EOF-P1 based on their lead-lag relationships with ENSO. During the development of ENSO, the South Pacific SSTA associated with ENSO for both P1 and P2 showed a significant eastward propagation. However, after the peak of ENSO, EOF-P1 showed a stronger persistence than EOF-P2, which still showed eastward propagation. The variability of the SSTA associated with the whole process of ENSO evolution during P1 and the SSTA associated with the development of ENSO during P2 support the existence of ocean-to-atmosphere forcing, but the SSTA associated with the decay of ENSO shows the phenomenon of atmosphere-to-ocean forcing. | LI Gang LI Chongyin TAN Yanke BAI Tao | 2014 | Advances in Atmospheric Sciences2014，31，1： | 5 |
| 3 | The Influence of El Ni?o on MJO over the Equatorial Pacific显示文摘In this paper, the influence of El Ni?o event on the Madden-Julian Oscillation(MJO) over the equatorial Pacific is studied by using reanalysis data and relevant numerical simulation results. It is clearly shown that El Ni?o can reduce the intensity of MJO. The kinetic energy of MJO over the equatorial Pacific is stronger before the occurrence of the El Ni?o event, but it is reduced rapidly after El Ni?o event outbreak, and the weakened MJO even can continue to the next summer. The convection over the central-western Pacific is weakened in El Ni?o winter. The positive anomalous OLR over the central-western Pacific has opposite variation in El Ni?o winter comparing to the non-ENSO cases. The vertical structure of MJO also affected by El Ni?o event, so the opposite direction features of the geopotential height and the zonal wind in upper and lower level troposphere for the MJO are not remarkable in the El Ni?o winter and tend to be barotropic features. El Ni?o event also has an influence on the eastward propa- gation of the MJO too. During El Ni?o winter, the eastward propagation of the MJO is not so regular and unanimous and there exists some eastward propagation, which is faster than that in non-ENSO case. Dynamic analyses suggest that positive SSTA(El Ni?o case) affects the atmospheric thickness over the equatorial Pacific and then the excited atmospheric wave-CISK mode is weakened, so that the intensity of MJO is reduced; the combining of the barotropic unstable mode in the atmosphere excited by external forcing(SSTA) and the original MJO may be an important reason for the MJO vertical structure tending to be barotropic during the El Ni?o. | CHEN Xiong LI Chongyin TAN Yanke | 2015 | Journal of Ocean University of China2015，14，1： | 3 |
| 4 | Scoring the collective effects of SNPs: association of minor alleles with complex traits in model organisms显示文摘It has long been assumed that most parts of a genome and most genetic variations or SNPs are non-functional with regard to reproductive fitness.However,the collective effects of SNPs have yet to be examined by experimental science.We here developed a novel approach to examine the relationship between traits and the total amount of SNPs in panels of genetic reference populations.We identified the minor alleles(MAs)in each panel and the MA content(MAC)that each inbred strain carried for a set of SNPs with genotypes determined in these panels.MAC was nearly linearly linked to quantitative variations in numerous traits in model organisms,including life span,tumor susceptibility,learning and memory,sensitivity to alcohol and anti-psychotic drugs,and two correlated traits poor reproductive fitness and strong immunity.These results suggest that the collective effects of SNPs are functional and do affect reproductive fitness. | YUAN DeJian ZHU ZuoBin TAN XiaoHua LIANG Jie ZENG Chen ZHANG JieGen CHEN Jun MA Long DOGAN Ayca BROCKMANN Gudrun GOLDMANN Oliver MEDINA Eva RICE Amanda D. MOYER Richard W. MAN Xian YI Ke LI YanKe LU Qing HUANG YiMin HUANG Shi | 2014 | Science China(Life Sciences)2014，57，9： | 2 |
| 5 | Diagnosis of Moist Vorticity and Moist Divergence for a Heavy Precipitation Event in Southwestern China显示文摘A regional heavy precipitation event that occurred over Sichuan Province on 8–9 September 2015 is analyzed based on hourly observed precipitation data obtained from weather stations and NCEP FNL data.Two moist dynamic parameters,i.e.,moist vorticity(mζ)and moist divergence(mδ),are used to diagnose this heavy precipitation event.Results show that the topography over southwestern China has a significant impact on the ability of these two parameters to diagnose precipitation.When the impact of topography is weak(i.e.,low altitude),mζ cannot exactly depict the location of precipitation in the initial stage of the event.Then,as the precipitation develops,its ability to depict the location improves significantly.In particular,mζ coincides best with the location of precipitation during the peak stage of the event.Besides,the evolution of the mζcenter shows high consistency with the evolution of the precipitation center.For mδ,although some false-alarm regions are apparent,it reflects the location of precipitation almost entirely during the precipitation event.However,the mδ center shows inconsistency with the precipitation center.These results suggest that both mζ and mδ have a significant ability to predict the location of precipitation.Moreover,mζ has a stronger ability than mδ in terms of predicting the variability of the precipitation center.However,when the impact of topography is strong(i.e.,high altitude),both of these two moist dynamic parameters are unable to depict the location and center of precipitation during the entire precipitation event,suggesting their weak ability to predict precipitation over complex topography. | Gang LI Daoyong YANG Xiaohua JIANG Jing PAN Yanke TAN | 2017 | Advances in Atmospheric Sciences2017，34，1： | 1 |
| 6 | Study on time-spatial changes and sudden characteristic of Winter Mongolia High显示文摘Based on the 155 years global monthly mean sea surface pressure data (Jan. 1850-Dec. 2004) from Hadley Centre, the time spatial change and sudden characteristics of the Winter Mongolia High are studied. First, the winter SLP distribution in Asia and the North Pacific are analyzed by the EOF method. Second, main cycle sequences of the Winter Mongolia High are reconstructed by the Singular Spectrum Analysis method, with special emphasis on the interdecadal periodic changes. Finally, the abrupt climate change is examined by the Mann-Kendall method. Results show that the Winter Mongolia High has quasi-biennial oscillation and a 3-4-year cycle of interannual change, also has a decadal variation for the 13-14-year cycle and interdecadal cycles for 20-21 years and 35-36 years. The 20-21-year cycle of WMHI is of the opposite phase to Aleutian Low, while the 35-36-year cycle is of the same phase. Otherwise, a significant abrupt climate change point in 1927 has been detected. | LiQunWang ChongYin Li YanKe Tan WeiMin Ma | 2010 | Research in Cold and Arid Regions2010，2，5： | 0 |
| 7 | Error Inhomogeneity in the Computation of Spherical Mean Displacement显示文摘The traditional method for computing the mean displacement in latitude–longitude coordinates is a spherical meridional–zonal resultant displacement method(MRDM), which regards the displacement as the resultant vector of the meridional and zonal displacement components. However, there are inhomogeneity and singularity in the computation error of the MRDM, especially at high latitudes. Using the NCEP/NCAR long-term monthly mean wind and idealized wind fields, the inhomogeneity in the MRDM was accessed by using a great circle displacement computing method(GCDM) for non-iterative cases. The MRDM and GCDM were also compared for iteration cases by taking the trajectories from a three-time level reference method as the real trajectories. In the horizontal direction, the GCDM assumes that an air particle moves along its locating great circle and that the magnitude of the displacement equals the arc length of the great circle. The inhomogeneity of the MRDM is evaluated in terms of the horizontal distance error from the products of wind speed, lapse time, and angle difference from the GCDM displacement orient.The non-iterative results show that the mean horizontal displacement computed through the MRDM has both computational and analytical errors. The displacement error of the MRDM depends on the wind speed, wind direction, and the departure latitude of the air particle. It increases with the wind speed and the departure latitude. The displacement magnitude error has a four-wave pattern and the displacement direction error has a two-wave feature in the definition range of the wind direction. The iterative result shows that the displacement magnitude error and angle error of the MRDM and GCDM with respect to the reference method increase with the lapse time and have similar distribution patterns. The mean magnitude error and the angle error of the MRDM are nearly twice as large as those of the GCDM. | Xuezhong WANG Banghui HU Hong HUANG Ju WANG Gang ZENG Yanke TAN Li ZOU | 2017 | Journal of Meteorological Research2017，31，6： | 0 |
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