Collaborative Research: Predicting Micro to Macro-scale Hot-spot and Hot-moment dynamics in Arctic Tundra Ecosystems

合作研究：预测北极苔原生态系统的微观到宏观热点和热点动态

• 批准号: 2311075
• 负责人: Christian Andresen
• 金额: $ 30.3万
• 依托单位: University of Wisconsin-Madison
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2023
• 资助国家: 美国
• 起止时间: 2023-07-01 至 2027-06-30
• 项目状态: 未结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2311075&HistoricalAwards=false
• 关键词: Collaborative; Research; Predicting; Micro; Macro

Rapid climate warming in the Arctic is thawing frozen soils, also known as permafrost, which is not only reshaping surface topography but also increasing the release of greenhouse gases to the atmosphere. Due to the speed in which Arctic landscapes are changing, and the massive carbon pools locked in permafrost, improving knowledge of the key interactions between plants and micro-organisms and their impacts on greenhouse gas release is essential for predicting how thawing Arctic soils will contribute to global climate change.The overarching objective of this project is to determine the micro-scale mechanisms driving hot-spot and hot-moment carbon dynamics, for improving predictions of macro-scale carbon balance. We hypothesize that the altered spatiotemporal distribution of degrading nutrient-rich permafrost has and will fundamentally alter the structure and function of northern tundra ecosystems, from microbes to landscapes. This multi-scale interdisciplinary project will transform our knowledge of fundamental plant-soil-microbial interactions that govern past and projected carbon cycle dynamics in permafrost ecosystems, while advancing knowledge of the key biogeochemical consequences of permafrost thaw over space (i.e., plot to landscape) and time (i.e., seasonal to decadal). The spatiotemporal mechanisms of hot-spots and hot-moment carbon dynamics will be characterized using a combination of low and high-precision ground and airborne flux observations to determine the location and assess the magnitude of carbon dioxide (CO2) and methane (CH4) hot-spots. Ground and remote sensing observations will determine the controls on the observed spatial distribution of hot-spots and fluxes, space-for-time analyses of plants, microbes, and landforms, coupled with the timing of permafrost degradation will infer the existence of hot-moments, while incubation experiments will illuminate the mechanisms driving hot-moments across sites across the Arctic Coastal Plain of northern Alaska. The proposed research will therefore provide the foundation for next-generation mechanistic and process-based models to represent novel disturbance regimes in the new Arctic. These research efforts will be complimented by a growing collaborative network of Alaskan native high-school student involvement in Arctic disturbance ecology. Students will use drones to measure their environment and share results across campuses and with the broader scientific community.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.

北极的快速气候变暖正在融化冻土，也称为永久冻土，这不仅重塑了地表地形，而且增加了温室气体向大气的释放。由于北极景观变化的速度，以及永久冻土中大量的碳库，提高对植物和微生物之间关键相互作用及其对温室气体释放影响的认识对于预测北极土壤融化将如何促进全球气候变化至关重要。本项目的总体目标是确定驱动热点和热点时刻碳动态的微观机制，改善宏观碳平衡的预测。我们假设，改变时空分布的降解营养丰富的永久冻土已经并将从根本上改变北方苔原生态系统的结构和功能，从微生物景观。这个多尺度的跨学科项目将改变我们对永久冻土生态系统中过去和预计的碳循环动态的基本植物-土壤-微生物相互作用的认识，同时推进对永久冻土解冻在空间上的关键地球化学后果的认识（即，绘图到风景）和时间（即，季节性到十年期）。热点和热点时刻碳动力学的时空机制将通过结合使用低精度和高精度地面和空中通量观测来确定二氧化碳（CO2）和甲烷（CH 4）热点的位置并评估其大小。地面和遥感观测将确定控制所观察到的热点和通量的空间分布，植物，微生物和地貌的时空分析，再加上永久冻土退化的时间将推断热时刻的存在，而孵化实验将照亮整个网站的驱动机制热时刻在整个北极沿海平原的北方阿拉斯加。因此，拟议的研究将为下一代机制和基于过程的模型提供基础，以代表新北极的新扰动机制。这些研究工作将得到阿拉斯加本地高中生参与北极干扰生态学的日益增长的合作网络的补充。学生将使用无人机测量他们的环境，并在校园内和更广泛的科学界分享结果。该奖项反映了NSF的法定使命，并通过使用基金会的知识价值和更广泛的影响审查标准进行评估，被认为值得支持。