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生态学杂志 ›› 2022, Vol. 41 ›› Issue (9): 1674-1682.doi: 10.13292/j.1000-4890.202206.012

• 研究报告 • 上一篇    下一篇

长白山区域森林主要树种迁移动态对气候变化的滞后响应

张鹏翼1,2,梁宇1,3*,马天啸1,刘波1,吴苗苗1


  

  1. (1中国科学院森林生态与管理重点实验室(中国科学院沈阳应用生态研究所), 沈阳 110016; 2中国科学院大学, 北京 100049; 3辽宁省陆地生态系统碳中和重点实验室, 沈阳 110016)

  • 出版日期:2022-09-10 发布日期:2022-09-02

The migration of main tree species lags behind climate change in Changbai Mountains.

ZHANG Peng-yi1,2, LIANG Yu1,3*, MA Tian-xiao1, LIU Bo1, WU Miao-miao1   

  1. (1CAS Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Shenyang 110016, China; 2University of Chinese Academy of Sciences, Beijing 100049, China; 3Key Laboratory of Terrestrial Ecosystem Carbon Neutrality, Liaoning Province, Shenyang 110016, China).

  • Online:2022-09-10 Published:2022-09-02

摘要: 在未来气候变化情景下,树种为了适应新的温度和降水格局,其分布边界可能会不断改变。本文通过耦合森林景观模型和生态系统过程模型模拟了树种迁移过程,并量化了未来100年长白山森林主要树种的迁移速度。为了探讨树种迁移动态对气候变化的滞后效应,本研究将未来100年的气候变化变量(温度、降水)的动态变化具象化为在空间上的迁移速度,通过比较气候变化速度与气候变化驱动下的树种迁移速度,从而量化了长白山区域主要树种对气候变化的滞后性。结果表明:未来100年长白山区域的温度在纬向上向北的平均迁移速度为0.57 km·a-1,降水在纬向上向北的平均迁移速度为1.17 km·a-1。长白山区域臭冷杉(Abies nephrolepis)、色木槭(Acer mono)、枫桦(Betula costata)、胡桃楸(Juglans mandshurica)、长白落叶松(Larix olgensis)、黄檗(Phellodendron amurense)、春榆(Ulmus davidiana var. japonica)的分布北界在未来100年以1.17~9.05 m·a-1的速度向北扩张,枫桦、黑桦(Betula dahurica)、长白鱼鳞云杉(Picea jezoensis var. komarovii)、红松(Pinus koraiensis)、紫椴(Tilia amurensis)、春榆的分布南界以0.97~10.03 m·a-1的速度向南扩张。臭冷杉、色木槭、枫桦、胡桃楸、长白落叶松、黄檗和春榆的分布北界向北迁移的速度滞后于气候向北迁移的速度,枫桦、黑桦、长白鱼鳞云杉、红松、紫椴和春榆的分布南界向南扩张同样显示了对气候变化的滞后响应。


关键词: 森林景观模型, 生态系统过程模型, 气候变化, 树种迁移滞后

Abstract: The range boundaries of tree species will continually shift in the future for adapting to the changing climate. We developed a model coupling framework which integrates a forest ecosystem model LINKAGES and a forest landscape model LANDIS PRO to simulate the migration process of main tree species in the Changbai Mountains. We calculated the migration velocity of those species in the next 100 years. To explore the migration lag of tree species in response to climate change, we calculated the latitudinal velocity of temperature and precipitation changes across Changbai Mountains in the next 100 years. We then compared the velocity of the shifts in tree species’ ranges with that of climate change to quantify the tree species migration lag. The results showed that the geometric mean velocity of annual mean temperature in latitude was 0.57 km·a-1 across all of the Changbai Mountains, and that the geometric mean velocity of total annual precipitation in latitude was 1.17 km·a-1. The northern boundary of Abies nephrolepis, Acer mono, Betula costata, Juglans mandshurica, Larix olgensis, Phellodendron amurense, and Ulmus davidiana var. japonica would migrate northward at a rate of 1.17-9.05 m·a-1 in the next 100 years. The southern boundary of Betula costata, Betula dahurica, Picea jezoensis var. komarovii, Pinus koraiensis, Tilia amurensis, and Ulmus davidiana var. japonica would migrate southward by 0.97-10.03 m·a-1. These results suggest that the migration of the examined tree species may lag behind climate change in Changbai Mountains.


Key words: forest landscape model, ecosystem process model, climate change, tree species migration lag.