Global observation gaps of peatland greenhouse gas balances: needs and obstacles

IF 3.9 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Biogeochemistry Pub Date : 2023-10-15 DOI:10.1007/s10533-023-01091-2
Junbin Zhao, Simon Weldon, Alexandra Barthelmes, Erin Swails, Kristell Hergoualc’h, Ülo Mander, Chunjing Qiu, John Connolly, Whendee L. Silver, David I. Campbell
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Abstract

Greenhouse gas (GHGs) emissions from peatlands contribute significantly to ongoing climate change because of human land use. To develop reliable and comprehensive estimates and predictions of GHG emissions from peatlands, it is necessary to have GHG observations, including carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O), that cover different peatland types globally. We synthesize published peatland studies with field GHG flux measurements to identify gaps in observations and suggest directions for future research. Although GHG flux measurements have been conducted at numerous sites globally, substantial gaps remain in current observations, encompassing various peatland types, regions and GHGs. Generally, there is a pressing need for additional GHG observations in Africa, Latin America and the Caribbean regions. Despite widespread measurements of CO2 and CH4, studies quantifying N2O emissions from peatlands are scarce, particularly in natural ecosystems. To expand the global coverage of peatland data, it is crucial to conduct more eddy covariance observations for long-term monitoring. Automated chambers are preferable for plot-scale observations to produce high temporal resolution data; however, traditional field campaigns with manual chamber measurements remain necessary, particularly in remote areas. To ensure that the data can be further used for modeling purposes, we suggest that chamber campaigns should be conducted at least monthly for a minimum duration of one year with no fewer than three replicates and measure key environmental variables. In addition, further studies are needed in restored peatlands, focusing on identifying the most effective restoration approaches for different ecosystem types, conditions, climates, and land use histories.

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泥炭地温室气体平衡的全球观测差距:需要和障碍
由于人类土地利用,泥炭地的温室气体排放对持续的气候变化有很大影响。为了对泥炭地的温室气体排放进行可靠和全面的估计和预测,有必要对全球不同泥炭地类型的温室气体进行观测,包括二氧化碳(CO2)、甲烷(CH4)和一氧化二氮(N2O)。我们将已发表的泥炭地研究与现场温室气体通量测量相结合,以确定观测中的差距,并为未来的研究提出方向。尽管已经在全球许多地点进行了温室气体通量测量,但目前的观测仍存在很大差距,包括各种泥炭地类型、区域和温室气体。总的来说,迫切需要在非洲、拉丁美洲和加勒比区域进行更多的温室气体观测。尽管对二氧化碳和甲烷进行了广泛的测量,但量化泥炭地N2O排放的研究很少,尤其是在自然生态系统中。为了扩大泥炭地数据的全球覆盖范围,进行更多的涡度协方差观测以进行长期监测至关重要。自动室对于绘图规模的观测是优选的,以产生高时间分辨率的数据;然而,采用手动测量室的传统实地活动仍然是必要的,特别是在偏远地区。为了确保数据可以进一步用于建模目的,我们建议至少每月进行一次室内活动,至少持续一年,不少于三次重复,并测量关键的环境变量。此外,还需要对恢复后的泥炭地进行进一步研究,重点是确定不同生态系统类型、条件、气候和土地利用历史的最有效恢复方法。
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来源期刊
Biogeochemistry
Biogeochemistry 环境科学-地球科学综合
CiteScore
7.10
自引率
5.00%
发文量
112
审稿时长
3.2 months
期刊介绍: Biogeochemistry publishes original and synthetic papers dealing with biotic controls on the chemistry of the environment, or with the geochemical control of the structure and function of ecosystems. Cycles are considered, either of individual elements or of specific classes of natural or anthropogenic compounds in ecosystems. Particular emphasis is given to coupled interactions of element cycles. The journal spans from the molecular to global scales to elucidate the mechanisms driving patterns in biogeochemical cycles through space and time. Studies on both natural and artificial ecosystems are published when they contribute to a general understanding of biogeochemistry.
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