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Factors contributing to the oxygen concentration over the Qinghai-Tibetan Plateau and its contribution rate calculation
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作者 Peijun SHI Ying ZHANG +6 位作者 Yanqiang CHEN Wenquan ZHU Xiaokang HU Heyi YANG Lu JIANG Yonggui MA haiping tang 《Science China Earth Sciences》 SCIE EI CAS CSCD 2024年第2期497-509,共13页
A decline in atmospheric oxygen concentration is projected in the 21st century given the background of global warming.The Qinghai-Tibetan Plateau is located at a high altitude,and thus,it faces a hypoxia challenge;how... A decline in atmospheric oxygen concentration is projected in the 21st century given the background of global warming.The Qinghai-Tibetan Plateau is located at a high altitude,and thus,it faces a hypoxia challenge;however,knowledge of the factors contributing to its atmospheric oxygen concentration is still lacking.Here,we conducted joint observations of ecosystem oxygen production and carbon sinks and near-surface atmospheric oxygen concentrations on the Qinghai-Tibetan Plateau and meteorological elements at Beijing Fangshan Station.Using seasonal differences and statistical methods,we calculated the relative contribution rates of vegetation to changes in atmospheric oxygen concentration.Our results indicate that solar radiation,atmospheric humidity,and ecosystem oxygen consumption and production have a significant impact on the atmospheric oxygen concentration,and the impact shows temporal and spatial differences.Vegetation significantly impacts the oxygen concentration,with a contribution rate of 16.7%–24.5%,which is underestimated in existing research.Our findings provide important insights into the factors that influence atmospheric oxygen concentration and highlight the contribution of vegetation.To better understand the oxygen dynamics of the Qinghai-Tibetan Plateau,we recommend further field observations of soil respiration and vegetation photosynthesis to clarify the contributions of carbon storage,carbon sinks and other factors to the near-surface atmospheric oxygen concentration. 展开更多
关键词 Qinghai-Tibetan Plateau Oxygen concentration Relative contribution rate Air temperature VEGETATION
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再论青藏高原近地表大气相对氧含量影响因素的贡献率 被引量:12
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作者 史培军 陈彦强 +3 位作者 马恒 叶涛 唐海萍 王静爱 《科学通报》 EI CAS CSCD 北大核心 2021年第31期4028-4035,共8页
在2017年夏季对青藏高原青藏线沿线近地表大气相对氧含量测量的基础上,于2018~2020年夏季对青藏高原新藏线、环青海湖、环祁连山(含冬季)、川藏线、西宁-玉树-昌都-昆明线、玉树-那曲-阿里线、西宁-合作-成都线等不同区域作了野外路线... 在2017年夏季对青藏高原青藏线沿线近地表大气相对氧含量测量的基础上,于2018~2020年夏季对青藏高原新藏线、环青海湖、环祁连山(含冬季)、川藏线、西宁-玉树-昌都-昆明线、玉树-那曲-阿里线、西宁-合作-成都线等不同区域作了野外路线考察测量,共计得到487个采样点的近地表大气相对氧含量等数据.研究结果表明,海拔、气温、植被覆盖度三者对近地表大气相对氧含量的贡献存在明显的时空差异.海拔的相对贡献为47%,气温的相对贡献为32%,植被覆盖度的相对贡献为3%,海拔不是绝对控制因素.海拔、气温、植被覆盖度只解释了近地表大气相对氧含量的82%,其余未解释部分很可能与植被净第一性生产力(net primary productivity, NPP)、土壤异养呼吸等其他因素有关.青藏高原近地表大气相对氧含量的时空差异很可能主要由不同类型植被光合作用的释氧与土壤异养呼吸的耗氧之间的差异,以及地势和近地表温度改变大气密度所致. 展开更多
关键词 青藏高原 大气相对氧含量 时空差异 地理环境 贡献率
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Overexpression of SIRT3 disrupts mitochondrial proteostasis and cell cycle progression 被引量:3
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作者 Xiaofei Wang haiping tang +6 位作者 Yuling Chen Binghuan Chi Shiyu Wang Yang Lv Di WU Renshan Ge Haiteng Deng 《Protein & Cell》 SCIE CAS CSCD 2016年第4期295-299,共5页
关键词 线粒体蛋白 细胞周期 过表达 人胚肾细胞 进程 肿瘤发生 肿瘤抑制基因 TCA循环
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气候变暖很可能缓减青藏高原人口缺氧健康风险 被引量:2
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作者 陈彦强 张钢锋 +12 位作者 陈宗颜 杨显明 陈波 马永贵 谢惠春 罗巧玉 杨静 叶涛 于德永 王静爱 唐海萍 陈志 史培军 《Science Bulletin》 SCIE EI CSCD 2022年第4期341-344,M0003,共5页
Every year,millions of people travel to high-elevation regions(≥2500 m above sea level)for sightseeing,mountaineering,trekking,skiing or commercial and scientific research activities.As the largest and highest platea... Every year,millions of people travel to high-elevation regions(≥2500 m above sea level)for sightseeing,mountaineering,trekking,skiing or commercial and scientific research activities.As the largest and highest plateau of the world,the Qinghai-Tibet Plateau(QTP)is one of the most attractive tourist destinations because of its multiple splendid sceneries.High-altitude illnesses occur when the rate of ascent to a high altitude overcomes the ability of the individual to acclimatize.Chronic mountain sickness(CMS)is one of the most important high-altitude pathologies in most high-altitude regions over the world. 展开更多
关键词 ALTITUDE ATTRACTIVE OVERCOME
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Driving mechanisms of desertification process in the Horqin Sandy Land—a case study in Zhalute Banner,Inner Mongolia of China 被引量:1
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作者 haiping tang Yufu CHEN Xinyu LI 《Frontiers of Environmental Science & Engineering》 SCIE EI CSCD 2008年第4期487-493,共7页
Both natural and human factors contributing to desertification were examined to understand the driving mechanisms of the desertification process in Zhalute Banner,Inner Mongolia of China.The coefficient of variation(C... Both natural and human factors contributing to desertification were examined to understand the driving mechanisms of the desertification process in Zhalute Banner,Inner Mongolia of China.The coefficient of variation(CV)and climate departure index(Z)were calculated to examine the fluctuations and trends of interannual variations of temperature and precipitation;TM remote sensing data was extracted to obtain the sandy land area;linear regression analysis was used to analyze climate changes and the socio-economic evolution over the years,and it was also used to standardize the variables,which included annual temperature,annual precipitation,human population,and livestock number,in order to measure the difference in the rate of change between climate and anthropogenic factors.The results showed that there was a rise of about 1.6uC in temperature but no significant change in precipitation from 1961 to 2000,which indicated a short-term climatic trend toward aridity in this area,a condition necessary for desertification.The fraction of precipitation in spring tended to increase whilst the fraction in autumn and winter decreased.Both the human population and livestock population had tripled and the cultivated area had doubled from 1961 to 2000,suggesting that socio-economic factors might have contributed more significantly to the desertification.Between 1988 and 1997,the sandy land area increased by 12.5%,nearly 2.4 times in the farming section.It could be concluded that the driving mechanisms of the desertification processes in Zhalute banner are mainly the policy of cropland expansion and the rising populations of humans and their livestock,which has affected the land use pattern in the past decades. 展开更多
关键词 climatic change potential evapo-transpiration(PE) human activities land use change
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