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    吉林省不同生态区碳源/汇能力及气候驱动因子分析

    Analysis of carbon source/sink capacity and climate driving factors in different ecological regions of Jilin Province

    • 摘要: 基于改进的CASA模型,利用2000—2022年MODIS、气象、土地利用分类多源数据,估算了吉林省不同生态区植被净生态系统生产力(NEP),探讨了NEP时空变化特征和气候驱动因子。结果表明:月际尺度上,研究区3—10月NEP为正值,呈现自然碳汇状态,其余月份呈碳源特征。年际尺度上,NEP多年均值为383.8 gC·m-2·a-1,呈波动上升趋势。空间尺度上,研究区NEP呈现自东向西逐渐减少的格局,研究时段内累积固碳量东部针阔叶混交林生态区>中部农田生态区>西部草甸草原生态区。植被NEP改善的面积占总面积90.38%,明显改善区域主要分布在西部生态区。研究区植被NEP与降水、太阳辐射主要呈正相关关系,与气温主要呈负相关。影响西部生态区NEP的主导气候因子是降水,影响中东部生态区NEP的主导气候因子是太阳辐射,且西部生态区NEP对降水和太阳辐射变化的敏感性更高。当降水量<700 mm时,植被NEP对降水的敏感性较高;当气温在5.7~6.9 ℃时,植被NEP敏感性随气温升高而增强。

       

      Abstract: This study is based on an improved CASA model and uses multi-source data from MODIS,meteorology,and land use classification from 2000 to 2022 to estimate the net ecosystem productivity (NEP) of vegetation in different ecological regions of Jilin Province.The spatiotemporal variation characteristics and climate driving factors of NEP are explored.The results indicate that on a monthly scale,the NEP in the study area is positive from March to October,showing a natural carbon sink state,while the remaining months exhibitcarbon source characteristics.On an interannual scale,the average annual NEP is 383.8 gC·m-2·a-1,exhibiting a fluctuating upward trend.On a spatial scale,the NEP in the study area shows a gradual decreasing trend from east to west.During the study period,the cumulative carbon sequestration was higherin the eastern coniferous and broad-leaved mixed forest ecological zone than in the central farmland ecological zone and the western grassland ecological zone.The area with improved vegetation NEP accounts for 90.38% of the total area,and the areas with significant improvement are mainly distributed in the western ecological zone.The vegetation NEP in the study area is mainly positively correlated with precipitation and solar radiation,and negatively correlated with temperature.The dominant climate factor affecting NEP in the western ecological zone is precipitation,while that in the central and eastern ecological zones is solar radiation,and NEP in the western ecological zone is more sensitive to changes in precipitation and solar radiation.When precipitation is less than 700 mm,vegetation NEP is more sensitive to precipitation;When the temperature is between 5.7 and 6.9 ℃,the sensitivity of vegetation NEP increases with rising temperature.

       

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