主办单位:中国气象局沈阳大气环境研究所
国际刊号:ISSN 1673-503X
国内刊号:CN 21-1531/P

气象与环境学报 ›› 2024, Vol. 40 ›› Issue (4): 100-106.doi: 10.3969/j.issn.1673-503X.2024.04.012

• 论文 • 上一篇    下一篇

2001—2021年呼伦贝尔地区净生态系统生产力分布及其与气温和降水的关系

曲学斌1(),李丹2,*(),田野1,赵岳冀1,张岚彪2,董越1   

  1. 1. 呼伦贝尔市气象局,内蒙古呼伦贝尔 0210081
    2. 内蒙古自治区生态与农业气象中心,内蒙古呼和浩特 010051
  • 收稿日期:2023-02-09 出版日期:2024-08-28 发布日期:2024-10-11
  • 通讯作者: 李丹 E-mail:qxbtd@qq.com;40342051@qq.com
  • 作者简介:曲学斌,男,1988年生,高级工程师,主要从事应用气象研究,E-mail: qxbtd@qq.com
  • 基金资助:
    内蒙古自治区自然科学基金(2024LHMS04012);内蒙古自治区自然科学基金(2024MS04007);内蒙古自治区气象局创新项目(nmqxkjcx202319)

Distribution of net ecosystem productivity in the Hulunbuir region from 2001 to 2021 and its relationship with temperature and precipitation

Xuebin QU1(),Dan LI2,*(),Ye TIAN1,Yueji ZHAO1,Lanbiao ZHANG2,Yue DONG1   

  1. 1. Hulunbuir Municipal Meteorological Service, Hulunbuir 0210081, China
    2. Inner Mongolia Autonomous Region Center for Ecological and Agricultural Meteorology, Hohhot 010051, China
  • Received:2023-02-09 Online:2024-08-28 Published:2024-10-11
  • Contact: Dan LI E-mail:qxbtd@qq.com;40342051@qq.com

摘要:

选用2001—2021年呼伦贝尔地区MODIS NPP和气象站观测数据,计算该地区净生态系统生产力(Net Ecosystem Productivity,NEP),分析NEP时空分布及其与气温和降水的关系。结果表明:呼伦贝尔的年平均NEP为249.4 gC·m-2·a-1,从呼伦贝尔大兴安岭中南部森林向两麓递减,呼伦贝尔草原西部NEP最小,且变异系数最大,生态环境相对脆弱。呼伦贝尔地区NEP以平均4.5 gC·m-2·a-1的速度增加,大兴安岭以东的林农交错带NEP增加较快,大兴安岭北部和呼伦贝尔草原东南部增加较慢。Hurst指数分析表明,未来呼伦贝尔大部地区的NEP变化趋势呈反持续性,不利于未来该地区固碳能力的提升。呼伦贝尔的草原、耕地以及大兴安岭东南麓森林NEP与生长季降水呈显著或极显著的正相关;草原地区NEP与生长季气温呈显著或极显著的负相关,大兴安岭火灾的灾后区NEP与生长季气温呈显著或极显著的正相关。

关键词: 固碳, Hurst指数, 生长季降水, 生长季气温

Abstract:

Utilizing MODIS NPP and meteorological station data from 2001 to 2021, this study calculated the net ecosystem productivity (NEP) in the Hulunbuir region and analyzed the spatial and temporal distribution of NEP and its relationships with temperature and precipitation. The results show that the annual average NEP in the Hulunbuir is 249.4 gC·m-2·a-1, decreasing from the central and southern forests of the Greater Khingan Range to its flanks, with the western Hulunbuir grasslands having the lowest NEP and the highest coefficient of variation, indicating a relatively fragile ecological environment. The NEP in the Hulunbuir region has increased at an average rate of 4.5 gC·m-2·a-1, with rapid increases observed in the forest-agriculture transition zone east of the Greater Khingan Range and slower increases in the northern part of the Greater Khingan Range and southeastern Hulunbuir grasslands. The Hurst index analysis suggests that future trends in NEP across most of Hulunbuir will exhibit anti-persistence, which is not conducive to enhancing the region′s carbon sequestration capacity. The NEP in Hulunbuir′s grasslands, croplands, and forests at the southeastern foothills of the Greater Khingan Range shows a significant or highly significant positive correlation with precipitation during the growing season. The NEP in the grassland areas has a significant or highly significant negative correlation with temperatures during the growing season, while the post-fire areas in the Greater Khingan Range show a significant or highly significant positive correlation with temperatures during the growing season.

Key words: Carbon sequestration, Hurst index, Precipitation during the growing season, Temperature during the growing season

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