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Relationships of climate change and tree ring of Betula ermanii tree line forest in Changbai Mountain 被引量:34
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作者 YU Da-pao GU Hui-yan +2 位作者 WANG Jian-dong WANG Qing-li DAI Li-min 《Journal of Forestry Research》 SCIE CAS CSCD 2005年第3期187-192,共6页
Based on the tree-ring growth characteristics of Erman's birch (Betula ermanii charm.) and the relationships between it and climatic )'actors at elevation of 1950m, the sensitivity of tree lines in Changbai Mount... Based on the tree-ring growth characteristics of Erman's birch (Betula ermanii charm.) and the relationships between it and climatic )'actors at elevation of 1950m, the sensitivity of tree lines in Changbai Mountain to climatic factors was assessed. The results indicated tree line forest in Changbai Mountain had an obvious sensitivity to climate factors. However, difference from other study sits is that the main climatic control factor on tree-ring growth was not current growth season temperatures, as might be expected, but previous winter and current March temperature. Although the precipitation in the region was quite abundant, the tree-ring growth was still significantly correlated with the precipitation during previous winter and current spring. Additionally, climatic factors which influenced the Erman's birch growth were not the yearly variables, but seasonal and monthly variables. Therefore, the reported increase in yearly mean temperature and total yearly precipitation since 1980s was not responded by sustained increase in ring widths in recent decades. 展开更多
关键词 Climatic change dendrochronology erman's birch Tree line in Changbai Mountain
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大兴安岭岳桦林的类型、结构特征和分布规律
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作者 周瑞昌 杨国亭 +1 位作者 马克平 孔刚 《地理科学》 CSSCI CSCD 北大核心 1991年第1期86-93,共8页
岳桦林在东北大兴安岭分布在海拔940—1650m 的山地。依据其组成、结构及分布特征划分三个类型。本区岳桦林在组成和结构上与长白山地岳桦林有明显的不同。岳桦林具有水土保持作用,应予以保护。
关键词 岳桦林 类型 结构 分布 大兴安岭
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长白山西坡风灾区森林恢复状况 被引量:12
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作者 郭利平 姬兰柱 +2 位作者 张伟东 张悦 薛俊刚 《应用生态学报》 CAS CSCD 北大核心 2010年第6期1381-1388,共8页
以长白山西坡风灾迹地(阔叶红松林、云冷杉林、岳桦林)的样地调查资料为基础,研究了各林型森林群落遇灾23年后的恢复特征.结果显示:3种林型的恢复速度为阔叶红松林>云冷杉林>岳桦林,并且它们与各自对照的群落共有度指数分别为0.49... 以长白山西坡风灾迹地(阔叶红松林、云冷杉林、岳桦林)的样地调查资料为基础,研究了各林型森林群落遇灾23年后的恢复特征.结果显示:3种林型的恢复速度为阔叶红松林>云冷杉林>岳桦林,并且它们与各自对照的群落共有度指数分别为0.49、0.44、0.33.风灾对各林型的乔木组成和多样性的影响不同:阔叶红松林中,风灾显著增加了乔木总数量,但对乔木种数和α多样性指数没有显著影响(P>0.05);云冷杉林中,风灾仅显著降低了Shan-non多样性指数和Simpson优势度指数;岳桦林中,除Pielou均匀度指数,其余多样性指数都因风灾而显著降低.各林型优势树种组成变化及更新情况对风灾的响应也与林型相关:阔叶红松林与对照区的优势树种组成显著不同,而云冷杉林及岳桦林受灾前后的优势树种组成差异均不大;阔叶红松林的幼树更新情况较好,云冷杉林有少量更新,岳桦林带几乎没有林木更新.表明风灾对森林群落的影响在23年后仍未消除,森林在风灾干扰后的恢复需要一个漫长的过程. 展开更多
关键词 风灾干扰 恢复状况 多样性指数 阔叶红松林 云冷杉林 岳桦林
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