青藏高原高寒草甸生态系统碳通量特征及其控制因子
Carbon Flux and Controlling Process of Alpine Meadow on Qinghai-Tibetan Plateau
查看参考文献28篇
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文摘
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青藏高原特殊的气候变化特征,在区域生态系统碳动态平衡起着重要作用。本文就青藏高原不同生态系统CO_2通量的时空变化及其影响因子和控制途径进行综述,以明确青藏高原植草地生态系统的碳源汇状况及时空变化特征,为全球变化的研究提供依据。 |
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其他语种文摘
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The Qinghai-Tibetan plateau possesses the largest area of natural grasslands in China. The grassland ecosystem on the plateau is hypothesized to play an important role in the carbon balance in both regional and global ecosystems. It is therefore of great significance to study the carbon flux of alpine meadow vegetation. The paper mainly summarizes research advances about the characters of carbon source/sink and carbon spatio-temporal variation for alpine meadow ecosystem on Qinghai-Tibetan plateau as well as con ducts some analysis of related researches in the future. |
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来源
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西北植物学报
,2007,27(5):1054-1060 【核心库】
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关键词
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青藏高原
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碳汇/源
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环境因子
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控制过程
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地址
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中国科学院西北高原生物研究所, 西宁, 810001
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语种
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中文 |
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文献类型
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综述型 |
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ISSN
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1000-4025 |
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学科
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植物学 |
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基金
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中国科学院知识创新工程项目
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中国科学院“百人计划”项目
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国家973计划
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国家科技支撑计划项目
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国家自然科学基金
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文献收藏号
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CSCD:2949549
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参考文献 共
28
共2页
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