哈萨克斯坦阿尔泰山树木径向生长及其对气候要素的响应

干旱区研究 ›› 2019, Vol. 36 ›› Issue (3): 723-733.

• 天气与气候 • 上一篇

哈萨克斯坦阿尔泰山树木径向生长及其对气候要素的响应

刘蕊^1,2,3，王勇辉¹，姜盛夏^2,3，张瑞波^2,3，秦莉^2,3，Bulkajyr T.Mambetov⁴，Nurzhan Kelgenbayev⁴，Daniyar Dosmanbetov⁴，Bagila Maisupova⁴，张同文^2,3

1. 新疆师范大学地理科学与旅游学院，新疆乌鲁木齐 830054；2. 中国气象局乌鲁木齐沙漠气象研究所，新疆乌鲁木齐 830002；3. 中国气象局树木年轮理化研究重点实验室，新疆乌鲁木齐 830002；4. 哈萨克斯坦农业部阿拉木图森林研究所，哈萨克斯坦阿拉木图 050050

收稿日期:2018-07-26 修回日期:2019-01-03 出版日期:2019-05-15 发布日期:2019-05-15
通讯作者: 王勇辉
作者简介:刘蕊（1995-），女，硕士研究生，自然地理学专业.Email: 1049830541@qq.com
基金资助:
国家自然科学基金（41605047）；上海合作组织科技伙伴计划（2017E01032）；自治区科技人才培养项目（qn2015bs025）和新疆维吾尔自治区重点实验室开放课题(2016D03005)共同资助

Radial Growth of Trees in Response to Climatic Factors in the Altay Mountains, South of Kazakhstan

LIU Rui^{1, 2, 3}, WANG Yong-hui¹, JIANG Sheng-xia^{2, 3}, ZHANG Rui-bo^{2, 3}, QIN Li^{2, 3}, Bulkajyr T. Mambetov⁴, Nurzhan Kelgenbayev⁴, Daniyar Dosmanbetov⁴, Bagila Maisupova⁴, ZHANG Tong-wen^{2, 3}

1. College of Geographical Science and Tourism,Xinjiang Normal University,Urumqi 830054,Xinjiang,China; 2. Institute of Desert Meteorology,China Meteorological Administration,Urumqi 830002,Xinjiang,China; 3. Key Laboratory of Tree-ring Physicochemical Research of China Meteorological Administration,Urumqi 830002,Xinjiang,China; 4. Almaty Institute of Forestry,Kazakhstan Ministry of Agriculture,Alma-Ata 050050,Kazakhstan

Received:2018-07-26 Revised:2019-01-03 Online:2019-05-15 Published:2019-05-15

摘要/Abstract

摘要： 针对哈萨克斯坦阿尔泰山南坡西伯利亚云杉（Picea obovata）和西伯利亚落叶松（Larix sibirica）开展树轮研究，建立树轮年表，计算年平均树轮宽度值和年平均断面积生长量（BAI），并分析在1988年发生升温突变前后，这2个树种树轮宽度指数变化趋势，及其树木径向生长对气候因子的响应。结果表明：在升温突变前后，2个树种树轮宽度指数变化趋势一致。但是，在升温突变后，其变化趋势均由不显著增加转为显著下降。即树木径向生长减缓；升温突变后，2个树种树木径向生长对降水的响应有所减弱，而对气温的响应有所增强，并且发生了树轮指数和气候因子间相关性“正负转换”的情况。

关键词: 阿尔泰山, 西伯利亚云杉, 西伯利亚落叶松, 树轮宽度, 径向生长, 响应分异, 哈萨克斯坦

Abstract:

The response of the radial growth of two tree species to climatic factors before and after a sudden rise of regional temperature in 1988 was analyzed based on the research of Picea obovata and Larix sibirica on the southern slope of the Altay Mountains in Kazakhstan. The results showed that there was a good correlation between the two standardized chronologies of the two tree species, and also a high consistency with the stage of low-frequency change and a high reliability of chronological series change. The GLK values of the two chronologies were high, which indicated that their radial growth was consistent. The radial growth of P. obovata and L. sibirica was faster at their young forest age but slower from the middle forest age to the mature forest age in the study area. The variation trend of tree-ring width index of these two tree species was consistent before and after the sudden rise of temperature. Before the sudden rise of temperature, the tree-ring width index of these two tree species increased unsignificantly with a slow decrease of precipitation and a slow increase of temperature. However, after the sudden rise of temperature, the tree-ring width index of P. obovata and L. sibirica was in a significant decline trend with the slow increase of annual precipitation and annual average temperature. This showed that there was a negative impact of climate change on the growth of trees, and the growth of these two tree species might be slowed down after the sudden rise of temperature. Under global warming, the radial growth of P. obovata and L. sibirica was mainly restricted by temperature, and the influence of precipitation was relatively low. The response of L. sibirica to temperature was slightly stronger than that of P. obovata. Holistically, there was a unsignificant difference in response of the radial growth of these two tree species to climate change. The response of the growth of these two tree species to climatic factors before and after the sudden rise of regional temperature in 1988 was analyzed. The results showed that, during the period from 1960 and 1988, there was a significant negative response of tree-ring width of L. sibirica to the precipitation in May that year, and to the temperature in August last year. There was a significant positive correlation between the radial growth of P. obovata and the precipitation in July of that year, but a significant negative correlation between it and the temperature in August last year. During the period from 1989 to 2016, the response of L. sibirica to the precipitation in May was no longer significant. Instead, there was a significant negative correlation between the growth of L. sibirica and the temperature in May of that year and in August last year. There was a weaker positive correlation and a higher negative correlation between the growth of this tree species and the temperature in growth season, or a change from positive correlation to negative correlation. The significant correlation between the radial growth of P. obovata and the precipitation disappeared. Instead, a negative correlation with temperature strengened, especially in August and October last year. The results showed that the positive response of the tree-ring width of P. obovata and L. sibirica to precipitation decreased but the negative response to temperature increased after the sudden rise of temperature. The response of the radial growth of P. obovata and L. sibirica to climatic factors might different after the sudden rise of temperature.

Key words: Altay Mountains, Picea obovata, Larix sibirica, tree-ring width, radial growth, response, Kazakhstan

刘蕊, 王勇辉, 姜盛夏, 张瑞波, 秦莉, Bulkajyr T.Mambetov, Nurzhan Kelgenbayev, Daniyar Dosmanbetov, Bagila Maisupova, 张同文.

哈萨克斯坦阿尔泰山树木径向生长及其对气候要素的响应 [J]. 干旱区研究, 2019, 36(3): 723-733.

LIU Rui, WANG Yong-hui, JIANG Sheng-xia, ZHANG Rui-bo, QIN Li, Bulkajyr T. Mambetov, Nurzhan Kelgenbayev, Daniyar Dosmanbetov, Bagila Maisupova, ZHANG Tong-wen.

Radial Growth of Trees in Response to Climatic Factors in the Altay Mountains, South of Kazakhstan [J]. Arid Zone Research, 2019, 36(3): 723-733.

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哈萨克斯坦阿尔泰山树木径向生长及其对气候要素的响应

Radial Growth of Trees in Response to Climatic Factors in the Altay Mountains, South of Kazakhstan

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