澜沧江源区高山柏径向生长对气候变化的响应
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科技部第二次青藏高原综合科学考察研究项目(2019QZKK0608)


Response of radial growth of Sabina squamata to climatic change in the Source Region of Lancang River
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The Second Tibetan Plateau Scientific Exploration, Grant/Award Number: 2019QZKK0608

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    摘要:

    为探究澜沧江源区气候变化对高山柏(Sabina squamata)径向生长的影响,在该区巴青县、杂多县和囊谦县分别对高山柏进行采样。运用树木年轮学方法测定3个样地高山柏逐年树轮宽度和胸高断面积增量(BAI),建立高山柏树轮宽度标准年表并分析其对气候变化的响应。研究结果表明,1986-2019年,澜沧江源区年平均温度呈快速上升趋势(0.43℃/10a,P<0.01),年平均最低气温(0.57℃/10a,P<0.01)的上升速率明显高于年平均最高气温(0.33℃/10a,P<0.01),而年降水量呈不显著的上升趋势(2.39 mm/a,P>0.10)。气候变暖背景下,澜沧江源区高山柏树轮宽度呈上升趋势(P<0.01),2000-2019年生长速率((0.37±0.16) mm/a)较1986-1999年((0.20±0.09) mm/a)增加了85%;BAI亦上升显著,在1986-1999年一直呈上升趋势((12.16±5.16) mm2/a),2000-2019年处于平稳快速生长阶段((22.49±8.84) mm2/a),表现出稳定且持续的生长能力。高山柏树轮宽度标准年表与气候因素的相关性显示:澜沧江源区高山柏径向生长对温度的响应明显强于降水,与多数月份(上年6月-当年10月)的降水呈不显著正相关,而与多数月份的温度呈显著正相关。与月平均最高温度和平均温度相比,高山柏径向生长与月平均最低温度的相关性更为显著(P<0.01)。在气候暖湿化背景下,近30年澜沧江源区高山柏径向生长进入快速生长时期,树轮宽度和BAI均呈快速生长特征,表明该区域气候条件更加适宜高山柏生长。

    Abstract:

    In order to explore the influence of climate change on the radial growth of Sabina squamata in the Source Region of Lancang River, samples of Sabina squamata were taken from Baqing County, Zaduo County, and Nangqian County in the Source Region of Lancang River, respectively. Dendrochronological method was used to measure the year-by-year tree ring width and basal area increment (BAI) of Sabina squamata in the three sample plots, and the standard chronology of Sabina squamata tree ring width was established and its response to climatic change was analyzed. The results showed that the annual mean temperature presented a rapid increasing trend from 1986 to 2019 in the Source Region of Lancang River (0.43℃/10a, P<0.01), and the annual mean minimum temperature (0.57℃/10a, P<0.01) increased significantly higher than the annual mean maximum temperature (0.33℃/10a, P<0.01), while the annual precipitation presented a weak upward trend (2.39 mm/a, P>0.10). Under the background of climate warming, the tree ring width of Sabina squamata showed an upward trend in the Source Region of Lancang River (P<0.01), and the growth rate of Sabina squamata ((0.37±0.16) mm/a) from 2000 to 2019 increased by 85% compared with that in 1986 to 1999 ((0.20±0.09) mm/a). The BAI also increased significantly, showing an upward trend ((12.16±5.16) mm2/a) from 1986 to 1999, and it was in a stable and rapid growth stage ((22.49±8.84) mm2/a) from 2000 to 2019, showing a stable and sustained growth ability. The correlation between the standard chronology of Sabina squamata tree ring width and climatic factors showed that the response of radial growth of Sabina squamata to temperature was significantly stronger than that of precipitation in the Source Region of Lancang River, which was not significantly positively correlated with precipitation in most months (June of last year to October of that year). However, it was significantly positively correlated with the temperature in most months. Compared with the monthly mean maximum temperature and mean temperature, the correlation between the radial growth of Sabina squamata and the monthly mean minimum temperature was more significant (P<0.01). Under the background of climate warming and humidification, the radial growth of Sabina squamata has entered a rapid growth period in the Source Region of Lancang River in recent 30 years, and the tree ring width and BAI were characterized by rapid growth, indicating that the climatic conditions in this area were more suitable for the growth of Sabina squamata.

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赵国清,信忠保,柳金昊,刘亚玲,黄艳章,李宗善.澜沧江源区高山柏径向生长对气候变化的响应.生态学报,2024,44(1):235~245

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