Lei Ying, Liu Yu, Sun Bo, Sun Changfeng
The State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, 710061, China.
Department of Environmental Science and Technology, School of Human Settlements and Civil Engineering, Xi'an Jiaotong University, Xi'an, 710049, China.
Int J Biometeorol. 2016 Oct;60(10):1519-1529. doi: 10.1007/s00484-016-1143-x. Epub 2016 Feb 21.
In this study, spruce tree rings from the southern slope of mid-Qinling Mountains were adopted to investigate the characteristics of average minimum temperatures during the past 138 years. Analysis showed that the interannual variability in radial growth of trees was positively correlated with the interannual variability of average minimum temperatures from previous December to current September (VTM ) in the study area during 1955-2010 AD. Based on the correlation analysis, the VTM were reconstructed for 1876-2013 AD with an explained variance of 42.5 % for the calibration period. Among the 22 dramatic changing years, extreme changes occurred more times when it was cooling, while the warming was comparatively gentle. Both the 10-year filtering of VTM series and the frequency of occurrences for those dramatic changing years showed a relatively stationary variation after the early 1950s. Over the last five decades, the accumulated VTM series showed an obvious warming trend, and the increase of the minimum temperature had contributed to the regional warming. The comparison of VTM and the dryness/wetness indices generally reflected cold-wet and warm-dry climate conditions in the study area. Significant positive correlations between the reconstructed VTM and the gridded minimum temperature indicated a regional representative of the temperature reconstruction, and positive correlations between VTM and sea surface temperature (SST) of the Indian Ocean and western Pacific regions suggested a possible linkage between the VTM variations and the Asian summer monsoon. Synchronous fluctuations in three tree-ring study series and connections of VTM with Arctic oscillation (AO) and El Niño-Southern Oscillation (ENSO) activities suggested that the minimum temperature variations in the TTH area responded sensitively to large-scale climate fluctuations and were the results of atmosphere-ocean interactions.
在本研究中,采用秦岭山脉中段南坡的云杉树轮来研究过去138年的平均最低气温特征。分析表明,公元1955 - 2010年期间,研究区域内树木径向生长的年际变化与前一年12月至当年9月的平均最低气温年际变化(VTM)呈正相关。基于相关性分析,重建了公元1876 - 2013年的VTM,校准期的解释方差为42.5%。在22个剧烈变化年份中,降温时极端变化出现的次数更多,而升温则相对平缓。VTM序列的10年滤波以及这些剧烈变化年份的出现频率在20世纪50年代初之后呈现出相对稳定的变化。在过去的五十年中,累积的VTM序列呈现出明显的变暖趋势,最低气温的升高促成了区域变暖。VTM与干湿指数的比较总体上反映了研究区域的冷湿和暖干气候条件。重建的VTM与网格化最低气温之间的显著正相关表明了温度重建的区域代表性,VTM与印度洋和西太平洋地区海表温度(SST)之间的正相关表明VTM变化与亚洲夏季风之间可能存在联系。三个树轮研究序列的同步波动以及VTM与北极涛动(AO)和厄尔尼诺 - 南方涛动(ENSO)活动的联系表明,TTH地区的最低气温变化对大规模气候波动敏感响应,是大气 - 海洋相互作用的结果。