青藏高原三江并流区近地表氧含量影响因素研究

Factors influencing near-surface oxygen in the Three Parallel Rivers Region of the Qinghai-Xizang Plateau

  • 摘要: 缺氧威胁着高海拔(海拔≥2 500 m)地区人群的身体健康.最近的研究表明,海拔不是影响青藏高原近地表大气氧含量(体积分数)的唯一因子,还受到气温和植被因素的综合影响,这种影响在青藏高原典型地区由于氧含量的观测点比较零散而未能深入探究。本研究于2019—2022年夏季沿川藏线和滇藏线对三江并流区开展野外路线考察测量,获得90个采样点数据以探索三江并流区干旱河谷近地表氧含量与海拔、植被(净初级生产力(NPP)、叶面积指数(LAI)、植被覆盖率(FVC)、生长季节长度(LOS))、气候变量(气温、月平均降水量)之间的关系.结果表明:1)气温、海拔、LAI、降水量、NPP和FVC是预测三江并流区近地表氧含量的重要变量;2)海拔是影响三江并流区近地表氧含量空间变异的主要因素;3)相较于整个青藏高原,植被因素对本研究区近地表氧含量的标准化直接影响显著下降.未来应将近地表氧含量的不同驱动因素纳入地球系统模型,以减少预测氧动态及其对全球变暖的潜在反馈的不确定性.

     

    Abstract: Low oxygen levels at high altitudes (≥ 2500 meters above sea level) threaten the health of human populations. Altitude is not the only factor affecting near-surface atmospheric oxygen content on the Qinghai-Xizang Plateau. Combined temperature and vegetation factors may also influence oxygen content but this has not been documented for the Qinghai-Xizang Plateau. In this study, field route survey measurements were made along the Sichuan-Xizang and Yunnan-Xizang routes in the summer of 2019-2022, data were obtained at 90 sampling points. Relationships were examined between near-surface oxygen content and elevation, vegetation (net primary productivity, leaf area index, vegetation cover, length of the growing season), climatic variables (air temperature, mean monthly precipitation) in the dry valleys of the Three Parallel Rivers Region. Temperature, elevation, LAI, precipitation, NPP and FVC were found to be important variables in predicting near-surface oxygen content in the Three Parallel Rivers Region. Elevation was the main factor influencing spatial variability of near-surface oxygen content. The standardized direct effect of vegetations on near-surface oxygen content in the present study area was significantly reduced compared with that of the entire Qinghai-Xizang Plateau. Different drivers of near-surface oxygen content should be incorporated into Earth system models to reduce uncertainty in predicting oxygen dynamics and its potential feedback to global warming.

     

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