NNA: Collaborative Research: MSB-FRA: Peat Expansion in Arctic Tundra - Pattern, Process, and the Implication for the Carbon Cycle (TundraPEAT)
NNA: Collaborative Research: MSB-FRA: Peat Expansion in Arctic Tundra - Pattern, Process, and the Implication for the Carbon Cycle (TundraPEAT)
批准号:
1802832
负责人:
Qianlai Zhuang
金额:
$30.45万
依托单位:
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2018
资助国家:
美国
项目状态:
已结题
起止时间:
2018-08-01 至 2024-07-31
中文摘要
近几十年来,北极变暖加剧,导致陆地生态系统发生了许多变化,有可能向全球系统提供强有力的反馈。由于复杂和不确定的土壤过程,北极植被绿化不一定会增加北极冻土带的碳固存。北极冻土带往往比大多数其他地带性生物群拥有更厚的有机土层(泥炭);研究表明,泥炭地构成了一个持续的碳汇。如果浅层泥炭地在整个北极普遍存在,那么全球范围内冻土带的整体净碳储存能力可能被低估了。然而,控制这些横跨北极的泥炭地的形成、分布和动态的因素还不是很清楚。该项目的总体目标是了解冻土带生物群中有机土壤(泥炭)的积累过程,并在十年和百年时间尺度上评估泥炭在区域和泛北极碳收支中的作用。该项目将研究变暖的北极地区潜在的泥炭迁移/扩张边界及其在区域和泛北极碳循环中的意义。该项目将对来自不同社会经济和文化背景的本科生、研究生和博士后进行数据分析和建模方面的培训。公众教育和推广计划包括面向初中生和高中生的STEM活动和一个关于北极环境的研讨会。了解控制绿色泥炭边界形成和向北迁移的环境条件和过程将为北极利益攸关方提供利用自然资源的信息。这个多学科研究小组将整合(1)北美北极最北部泥炭形成边界沿线多个冻土带地点的新数据收集,以及(2)实验室孵化实验,(3)综合冻土带和北方生物群的现有数据,以及(4)生态系统规模过程模型模拟。最重要的问题是:变暖的北极会像现在的北方地带那样,转变为泥炭丰富的地貌吗?或者,变暖的北极是否缺乏阻止这一转变的必要条件?为了解决这个广泛的问题,这项研究集中在北极泥炭形成生态系统的两个关键元素:泥炭地,以及泥炭在这些潜在的泥炭地形成、持续和快速固碳中的作用。使用观测、实验和模拟结果,以及来自协调的国际研究网络的合成产品,研究团队将测试以下假设:(1)这些快速形成和迁移的泥炭地的年龄、碳积累速率和大陆模式;(2)生产和分解过程对温度和湿度变化的不同响应;以及(3)泥炭在改变小气候和改变其生产力和腐解性之间的平衡方面的作用。这一奖项反映了NSF的法定使命,并通过使用基金会的智力优势和更广泛的影响审查标准进行评估,被认为值得支持。
英文摘要
Amplified Arctic warming in recent decades has caused a multitude of changes in terrestrial ecosystems that have potential for strong feedbacks to the global system. Arctic vegetation greening may not necessarily result in increases in carbon sequestration in Arctic tundra due to complex and uncertain soil processes. Arctic tundra tends to have a thicker organic soil horizon (peat) than most other zonal biomes; research shows that peatlands comprise a sustained carbon sink. If shallow peatlands are widespread throughout the Arctic, the overall net carbon storage capacity of tundra might be underestimated globally. However, the factors controlling the formation, distribution, and dynamics of these peat patches across the Arctic are not well understood. The overall goal of the project is to understand organic soil (peat) accumulation processes in the tundra biome and to assess the role of peat in regional and pan-Arctic carbon budgets at decadal and centennial timescales. The project will examine potential peat migration/expansion frontiers in a warming Arctic and their significance in the regional and pan-Arctic carbon cycle. The project will train undergraduates, graduate students, and postdocs from diverse socio-economic and cultural backgrounds in both data analysis and modeling. The public education and outreach program includes STEM activities involving middle and high school students and a symposium on Arctic environments. The understanding of environmental conditions and processes that control the formation and northward migrations of the green peat frontier will inform Arctic stakeholders in their use of natural resources.This multidisciplinary research team of researchers will integrate (1) new data collection from multiple tundra sites along the northernmost peat-forming frontiers of the North American Arctic, together with (2) laboratory incubation experiments, (3) a synthesis of existing data from the tundra and boreal biomes, and (4) ecosystem-scale process model simulations. The overarching question is: will the warming Arctic transform into a peat-rich landscape, as the boreal zone is now, or are there essential conditions lacking in a warming Arctic that will prevent this? To address this broad question, the research focuses on two key elements of the Arctic peat-forming ecosystems: peat patches, and the role of Sphagnum in the formation, persistence, and rapid rates of carbon sequestration of these potentially incipient peatlands. Using observational, experimental, and modeling results, along with synthesis products from a coordinated international research network, the research team will test hypotheses on (1) the ages, carbon accumulation rates, and continental pattern of these rapidly forming and migrating peat patches; (2) the various responses of production and decomposition processes to temperature and moisture change; and (3) the role of Sphagnum in modifying microclimate and shifting balance between their productivity and decomposability.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.
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DOI:
10.1038/s43247-022-00488-5
发表时间:
2022-07
期刊:
Communications Earth & Environment
影响因子:
7.9
作者:
[Y. Oh;Q. Zhuang;L. Welp;Licheng Liu;X. Lan;S. Basu;E. Dlugokencky;L. Bruhwiler;John B. Miller;S. Michel;S. Schwietzke;P. Tans;P. Ciais;J. Chanton]
通讯作者:
Y. Oh;Q. Zhuang;L. Welp;Licheng Liu;X. Lan;S. Basu;E. Dlugokencky;L. Bruhwiler;John B. Miller;S. Michel;S. Schwietzke;P. Tans;P. Ciais;J. Chanton
DOI:
10.1029/2022jg007009
发表时间:
2022-11
期刊:
Journal of Geophysical Research: Biogeosciences
影响因子:
--
作者:
[Bailu Zhao;Q. Zhuang;S. Frolking]
通讯作者:
Bailu Zhao;Q. Zhuang;S. Frolking
DOI:
10.5194/bg-20-251-2023
发表时间:
2023-01
期刊:
Biogeosciences
影响因子:
4.9
作者:
[Bailu Zhao;Q. Zhuang]
通讯作者:
Bailu Zhao;Q. Zhuang
DOI:
10.1029/2019jg005230
发表时间:
2020
期刊:
Journal of Geophysical Research: Biogeosciences
影响因子:
--
作者:
[Zhuang, Qianlai, Wang, Sirui, Zhao, Bailu, Aires, Filipe, Prigent, Catherine, Yu, Zicheng, Keller, Jason K., Bridgham, Scott]
通讯作者:
Bridgham, Scott
DOI:
10.1029/2021jg006774
发表时间:
2022-09
期刊:
Journal of Geophysical Research: Biogeosciences
影响因子:
--
作者:
[D. Kou;T. Virtanen;C. Treat;J. Tuovinen;Aleksi Räsänen;S. Juutinen;J. Mikola;M. Aurela;L. Heiskanen]
通讯作者:
D. Kou;T. Virtanen;C. Treat;J. Tuovinen;Aleksi Räsänen;S. Juutinen;J. Mikola;M. Aurela;L. Heiskanen
共 8 条
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Collaborative Research: Synthesis of Arctic System Carbon Cycle Research Through Model-Data Fusion Studies Using Atmospheric Inversion and Process-Based Approaches
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依托单位:
Collaborative Research: Synthesis of Arctic System Carbon Cycle Research Through Model-Data Fusion Studies Using Atmospheric Inversion and Process-Based Approaches
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资助金额:$24.59万
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财政年份:2005
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依托单位:
海外基金