GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstrasse 1-3, Kiel, 24148, Germany.
Ocean Networks Canada, University of Victoria's Ocean-Climate Building at the Queenswood Campus, 2474 Arbutus Rd, Victoria, BC, V8N 1V9, Canada.
Nat Commun. 2018 Aug 15;9(1):3264. doi: 10.1038/s41467-018-05736-x.
Widespread gas venting along the Cascadia margin is investigated from acoustic water column data and reveals a nonuniform regional distribution of over 1100 mapped acoustic flares. The highest number of flares occurs on the shelf, and the highest flare density is seen around the nutrition-rich outflow of the Juan de Fuca Strait. We determine ∼430 flow-rates at ∼340 individual flare locations along the margin with instantaneous in situ values ranging from ∼6 mL min to ∼18 L min. Applying a tidal-modulation model, a depth-dependent methane density, and extrapolating these results across the margin using two normalization techniques yields a combined average in situ flow-rate of ∼88 × 10 kg y. The average methane flux-rate for the Cascadia margin is thus estimated to ∼0.9 g ym. Combined uncertainties result in a range of these values between 4.5 and 1800% of the estimated mean values.
从声学水柱数据中研究了卡斯卡迪亚边缘的广泛气体逸出,并揭示了超过 1100 个映射声耀斑的非均匀区域分布。耀斑数量最多的发生在大陆架上,而富营养物质流出的胡安·德富卡海峡周围的耀斑密度最高。我们在边缘的大约 340 个耀斑位置确定了大约 430 个流量率,瞬时原位值范围从大约 6 毫升/分钟到大约 18 升/分钟。应用潮汐调制模型、深度相关的甲烷密度,并使用两种归一化技术将这些结果外推到整个边缘,得出的总平均原位流量率约为 88×10 千克/年。因此,卡斯卡迪亚边缘的甲烷通量速率估计约为 0.9 克/年。结合不确定性,这些值的范围在估计平均值的 4.5 到 1800%之间。