globalchange  > 气候变化事实与影响
CSCD记录号: CSCD:6040127
论文题名:
天山东西部雪岭云杉径向生长对气候变暖的响应差异
其他题名: Difference in response of radial growth of Picea schrenkiana to climate warming in the eastern and western Tianshan Mountains
作者: 张艳静; 于瑞德; 郑宏伟; 甘淼; 杨美琳; 石冰冰
刊名: 生态学杂志
ISSN: 1000-4890
出版年: 2017
卷: 36, 期:8, 页码:407-419
语种: 中文
中文关键词: 树木年轮 ; 雪岭云杉 ; 气候变暖 ; 敏感性 ; 天山
英文关键词: tree ring ; Picea schrenkiana ; climate warming ; sensitivity ; Tianshan Mountains
WOS学科分类: BIOLOGY
WOS研究方向: Life Sciences & Biomedicine - Other Topics
中文摘要: 运用树木年轮气候学方法,研究了天山东西部森林上下限雪岭云杉(Picea schrenkiana)树木生长与气候因子的关系,以期揭示不同地区雪岭云杉径向生长对气候因子响应的差异及气候变暖影响下雪岭云杉的敏感性。结果表明:(1)昭苏地区年轮年表的统计特征更显著,比哈密地区树木径向生长对气候因子的响应更敏感; (2) 2个地区树木生长受温度与降水的综合影响,从西部到东部,森林下限树木径向生长与温度的响应由显著正相关转为显著负相关;而森林上限树木生长与降水的关系由显著负相关转变为显著正相关; (3)进入快速升温阶段,气候条件对昭苏和哈密地区森林下限雪岭云杉生长的影响增强,而对哈密地区森林上限雪岭云杉生长的影响减弱; (4)随着温度升高,昭苏森林下限和哈密森林上下限的雪岭云杉径向生长与气候因子的关系均出现了显著变化。快速升温后,4月温度对哈密森林上限树木径向生长的促进作用显著增加,6月温度对昭苏和哈密森林下限树木生长的抑制作用显著增加,而对哈密森林上限树木生长的促进作用显著减弱; 5和6月份降水分别对昭苏森林下限和哈密森林上限雪岭云杉径向生长的促进作用显著增加; 4月温度和10月降水对哈密森林下限树木生长的抑制作用显著减弱。昭苏森林上限降水能够满足树木生长,气温升高对树木生长与气候因子关系的影响不显著。
英文摘要: The relationship between tree growth and meteorological factors of Picea schrenkiana in upper and lower forest of eastern and western Tianshan Mountains was studied by climatological method,to reveal the radial growth of P. schrenkiana in response to climatic factors in different regions and the sensitivity of P. schrenkiana under the influence of climate warming. Through a large number of data collection and analysis,the results showed several interesting points. First, the statistical characteristics of chronology were more significant and radial growth of trees was more sensitive to climatic factors in Zhaosu than in Hami. Second,the growth of trees in the two regions was affected by temperature and precipitation. From western to eastern Tianshan Mountains,the significantly positive correlation was reversed to be significantly negative between tree radial growth and temperature in the lower forest boundary,while the relationship between tree growth and precipitation in the upper forest boundary changed from significantly negative to significantly positive. Third,at the lower elevations of Zhaosu and Hami,climate had a stronger influence on the growth of P. schrenkiana during 1984 - 2015 with increasing temperature than during 1957-1983 with decreasing temperature,whereas the growth of trees displayed reversed patterns in response to climate between the two periods at higher elevations of Hami. Furthermore, as the temperature increased,the promoting effect of temperature on the radial growth of trees increased significantly in the lower forest boundary of Hami in April,while the inhibitory effect of temperature on the radial growth of trees increased significantly in the lower forest boundary of Zhaosu and Hami in June. However,the promoting effect of temperature in June on P. schrenkiana growth decreased significantly in the upper forest boundary in Hami. The promoting effects of precipitation increased significantly for the radial growth of P. schrenkiana in lower forest boundary in Zhaosu and in upper forest boundary in Hami in May and June,respectively. The inhibitory effect of temperature in April and precipitation in October on P. schrenkiana growth decreased significantly in the lower forest boundary in Hami. As the temperature increased,the relationship between tree growth and the local climate factors changed insignificantly,because the precipitation in the upper forest boundary in Zhaosu can meet the growth of trees.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/153074
Appears in Collections:气候变化事实与影响

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作者单位: 中国科学院新疆生态与地理研究所荒漠环境研究室, 乌鲁木齐, 新疆 830011, 中国

Recommended Citation:
张艳静,于瑞德,郑宏伟,等. 天山东西部雪岭云杉径向生长对气候变暖的响应差异[J]. 生态学杂志,2017-01-01,36(8):407-419
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