RAPID: Waiting to Exhale: Quantifying Tropical Storm-Induced Increased Flux of Coastal Wetland Carbon into the Atmosphere?

于二零二零年夏季及秋季，路易斯安那州的沿海海湾受到多场热带风暴╱飓风的影响。热带风暴马可、飓风劳拉、莎莉和贝塔最接近巴拉塔里亚湾，距离马可81公里，贝塔379公里。风暴侵蚀可导致沿海土壤中的碳以二氧化碳（CO2）的形式释放到大气中。科学家们很少有机会评估热带风暴对湿地土壤碳转化为二氧化碳释放到大气中的影响，因为他们没有风暴前的详细测量数据与风暴后的数据进行比较。该项目有机会受益于现有的NSF赠款，并进行了四年的广泛测量。快速响应资金将支持在2020年风暴后立即对巴拉塔里亚湾进行密集采样，并在一年后进行。尽管没有直接打击沿海盆地，沼泽边缘侵蚀率高达60倍以上的4年的长期平均水平。这已经是一个重要的发现，因为大多数测量集中在海岸线的直接打击，但显然，大量的湿地侵蚀发生在热带风暴赋予风场驱动波能量在相当长的距离。因此，一个特别活跃的热带风暴季节导致大量富含碳的湿地土壤在相对较短的时间内被倾倒到巴拉塔里亚湾的浅水有氧沃茨。该项目要解决的主要问题是，2020年风暴季节的加速侵蚀是否以及如何导致从海湾到大气的二氧化碳排放量显着增加，以及这种影响将持续多久。调查小组将在未来一年继续测量沼泽边缘侵蚀，每月两次对海湾表面沃茨进行水取样，以确定溶解的无机和有机碳以及溶解的二氧化碳。采样将沿着样带进行，从靠近开放海湾的湿地侵蚀站开始。海气CO2通量将使用一个模型进行估算，并与湿地侵蚀率相关联。该小组将把风暴事件引起的“海湾呼吸”率与明年的情况进行比较。这个快速项目将产生几个重要成果：1）确定一些重大风暴导致的湿地碳损失的增加和时间影响，类似于气候变化下未来的预期;（二）了解有机碳分解为二氧化碳是否会增加沿海海湾内的沿海酸化。该奖项反映了NSF的法定使命，并被认为是值得的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，

In the summer and fall of 2020, the coastal bays of Louisiana have experienced impacts from a number of tropical storms/hurricanes in close procession. Tropical storm Marco, Hurricanes Laura, Sally and Beta made their closest approaches to Barataria Bay from 81 km for Marco, up to 379 km for Beta. Storm erosion can lead to carbon from coastal soils being released to the atmosphere as carbon dioxide (CO2). Scientists rarely have the opportunity to assess the impact of tropical storms on the conversion of wetland soil carbon to CO2 release to the atmosphere, because they don’t have detailed measurements from before the storms to compare with post-storm data. This project has an opportunity to benefit from an existing NSF grant with four years of extensive measurements. RAPID-response funding will support intensive sampling of Barataria Bay in the immediate aftermath of the 2020 storms, and up to a year afterwards. Despite no direct strikes to the coastal basin, marsh edge erosion rates were up to 60 times higher than the 4-year long-term average. This is already an important finding since most measurements focus on coastlines with direct strikes but clearly, substantial wetland erosion occurs from tropical storms imparting wind fields driving wave energy at substantial distances. Consequently, a particularly active tropical storm season has led to significant carbon-rich wetland soil being dumped into the shallow, aerobic waters of the Barataria Bay in a relatively short period of time. The primary questions to be addressed by this project are whether and how accelerated erosion from the 2020 storm season will lead to a significant increase in CO2 outgassing from the bay to the atmosphere, and for how long the effects will persist. The team of investigators will continue to measure marsh edge erosion over the next year correlated to twice a month water sampling of bay surface waters for determination of dissolved inorganic and organic carbon, and dissolved CO2. Sampling will be conducted along transects running from close proximity to the wetland erosion stations out in the open bay. Air-sea CO2 flux will be estimated using a model and correlated to the wetland erosion rates. The team will compare the storm event-induced “bay respiration” rate with that of next year. This RAPID project will yield several important outcomes: 1) Determination of the increase and temporal impact of wetland carbon loss to the atmosphere from a number of significant storms, similar to what is expected for the future under a changing climate; 2) Understanding if the organic C breakdown to CO2 will increase coastal acidification within the coastal bay.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.