CAREER: Experimental Warming, Permafrost Thawing, and the Loss of Old Carbon from Tundra: Radiocarbon Research and Education to Understand Ecosystem Feedbacks to Climate Change

职业：实验变暖、永久冻土融化和苔原旧碳的流失：放射性碳研究和教育，以了解生态系统对气候变化的反馈

• 批准号: 0747195
• 负责人: Edward Schuur
• 金额: $ 60万
• 依托单位: University of Florida
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2008
• 资助国家: 美国
• 起止时间: 2008-03-01 至 2014-02-28
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0747195&HistoricalAwards=false
• 关键词: CAREER; Experimental; Warming; Permafrost; Thawing

Enough carbon is contained in soils and permafrost of northern ecosystems to double current carbon dioxide in the atmosphere. Because of the size and nature of the permafrost carbon pool, decomposition of previously frozen, old organic carbon is one of the most likely positive feedbacks from terrestrial ecosystems to climate change in a warmer world. This project uses radiocarbon measurements as a unique fingerprint for detecting the loss of old soil carbon in combination with an ecosystem-scale field manipulation to determine controls over the release of permafrost carbon. This high-precision isotope research is paired with the continued development and teaching of an intensive short course designed to expose students to the emerging technology of accelerator mass spectrometry for measuring radiocarbon. Increased numbers of radiocarbon measurements combined with more researchers skilled in the interpretation of this data offers great promise towards detecting changes in ecosystem and global carbon cycling. Climate change is altering the world in which we live. At present, increasing greenhouse gases responsible for climate change are largely a result of human activities. However, climate change may alter the natural cycling of carbon in ecosystems far from direct human influence. The permafrost carbon pool is more than 100 times the current annual inputs of carbon dioxide into the atmosphere from human activity, and thresholds at the freezing point indicate that abrupt changes are possible. This research and education plan focusing on radiocarbon is aimed at understanding more broadly whether terrestrial ecosystems will accelerate or mitigate future climate change.

北方生态系统的土壤和永久冻土中含有足够的碳，使大气中目前的二氧化碳增加一倍。 由于永久冻土碳库的规模和性质，以前冻结的旧有机碳的分解是陆地生态系统对温暖世界中气候变化的最有可能的正反馈之一。 该项目使用放射性碳测量作为一种独特的指纹，结合生态系统规模的现场操作，以确定对永久冻土碳释放的控制，检测旧土壤碳的损失。 这种高精度的同位素研究与一个密集的短期课程的持续开发和教学相结合，旨在让学生接触到用于测量放射性碳的加速器质谱的新兴技术。 越来越多的放射性碳测量加上更多的研究人员熟练地解释这些数据，为检测生态系统和全球碳循环的变化提供了巨大的希望。气候变化正在改变我们生活的世界。目前，造成气候变化的温室气体不断增加，主要是人类活动造成的。 然而，气候变化可能会改变远离人类直接影响的生态系统中碳的自然循环。 永久冻土的碳库是目前人类活动每年向大气中输入的二氧化碳的100倍以上，冰点的阈值表明可能发生突然变化。 这项研究和教育计划侧重于放射性碳，旨在更广泛地了解陆地生态系统是否会加速或减缓未来的气候变化。