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生态学杂志 ›› 2024, Vol. 43 ›› Issue (9): 2596-2606.doi: 10.13292/j.1000-4890.202409.021

• 森林与林业生态 • 上一篇    下一篇

气候变暖对长白山自然保护区森林碳库的影响

王丹1,2,王文娟2,武海涛2,姜明2,吕云峰1*,薛振山2*   

  1. 1长春师范大学地理科学学院, 长春 130032; 2中国科学院东北地理与农业生态研究所, 长春 130102)

  • 出版日期:2024-09-10 发布日期:2024-09-09

Effects of climate warming on forest carbon pools in the Changbai Mountain Nature Reserve.

WANG Dan1,2, WANG Wenjuan2, WU Haitao2, JIANG Ming2, LYU Yunfeng1*, XUE Zhenshan2*   

  1. (1School of Geographical Science, Changchun Normal University, Changchun 130032, China; 2Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, China).

  • Online:2024-09-10 Published:2024-09-09

摘要: 气候变化会影响森林生态系统结构和功能,进而给森林固碳潜力的估算带来许多不确定性。为明晰气候变暖下长白山森林碳库的动态特征,本研究利用空间直观景观模型LANDIS-Ⅱ,模拟了2000—2100年间长白山自然保护区在3种未来气候情景(SSP1-2.6、SSP3-7.0和SSP5-8.5)和现行气候情景(SSP0-1.0)下森林固碳潜力和碳储量的变化。结果表明:(1)未来森林净初级生产力(net primary productivity,NPP)会不断提高,到2100年,3种未来气候情景下的森林NPP均高于SSP0-1.0气候情景下的NPP值(1010 g C·m-2·a-1),但不同气候情景下森林NPP时空差异不显著。(2)4种气候情景下森林总碳储量均呈逐年增加趋势,但与SSP0-1.0情景相比,SSP1-2.6情景下植物碳库增加,土壤碳库和碎屑碳库减少,总碳储量降低了2.1%;SSP3-7.0和SSP5-8.5情景下植物碳库、碎屑碳库和土壤碳库均减少,总碳储量分别降低了3.4%和4.2%。(3)相较于中、高海拔地区,低海拔区域森林碳库对气候变暖更加敏感;森林植物碳库对气候变暖的响应存在海拔梯度规律,在3种未来气候情景下,植物碳库在低海拔处显著减少,在高海拔区域植物固碳增加。研究结果可为长白山长期森林管理和提高森林固碳潜力提供参考。


关键词: 气候变化, LANDIS-Ⅱ, 净初级生产力, 森林碳库

Abstract: Climate change will affect the structure and function of forest ecosystems, bringing uncertainty in the estimation of forest carbon sequestration potential. To clarify the dynamics of forest carbon pools in the Changbai Mountain under climate warming, we utilized the spatially explicit landscape model LANDIS-Ⅱ to simulate the changes in forest carbon sequestration potential and carbon stock in the Changbai Mountain Nature Reserve from 2000 to 2100 under three future climate scenarios (SSP1-2.6, SSP3-7.0, SSP5-8.5) and the current climate scenario (SSP0-1.0). The results showed that: (1) Net primary productivity (NPP) of forests would continue to increase in the future. By 2100, NPP under the three future climate scenarios is higher than that under the SSP0-1.0 scenario (NPP of 1010 g C·m-2·a-1). However, there are no significant spatial-temporal variations in NPP among the different climate scenarios. (2) The total carbon stock in forests shows an increasing trend under all climate scenarios. Compared to the SSP0-1.0 scenario, the SSP1-2.6 scenario leads to an increase in plant carbon pools but a decrease in soil carbon pools and detritus carbon pools, resulting in a 2.1% decrease in total carbon stock. Under the SSP3-7.0 and SSP5-8.5 scenarios, all carbon pools (plant, detritus, and soil) decrease, leading to reductions of 3.4% and 4.2% in total carbon stock, respectively. (3) The carbon pools of high-elevation forests are more sensitive to future climate warming than low-elevation and middle-elevation forests. The response of plant carbon pools to climate change shows an altitudinal gradient effect. Plant carbon pools significantly decrease at low-altitude regions and are promoted at high-altitude regions under all three future climate scenarios. This study could provide a reference for long-term forest management and the enhancement of forest carbon sequestration potential in the Changbai Mountain.


Key words: climate change, LANDIS-Ⅱ, net primary productivity, forest carbon pool