当前位置: X-MOL 学术J. Volcanol. Geotherm. Res. › 论文详情
Our official English website, www.x-mol.net, welcomes your feedback! (Note: you will need to create a separate account there.)
Long-term year-round observations of magmatic CO2 emissions on Mammoth Mountain, California, USA
Journal of Volcanology and Geothermal Research ( IF 2.4 ) Pub Date : 2021-07-14 , DOI: 10.1016/j.jvolgeores.2021.107347
J.L. Lewicki 1
Affiliation  

Diffuse emission of magmatic CO2 is one of the main indicators of volcanic unrest at Mammoth Mountain, but the presence of deep seasonal snowpack at the site has hindered year-round CO2 flux observations. A permanent eddy covariance station was established at the largest area of diffuse CO2 degassing on Mammoth Mountain (Horseshoe Lake tree kill) that measured CO2 fluxes (Fc) and meteorological parameters on a half-hourly basis. From July 22, 2014 to May 24, 2020, Fc ranged from −35 to 10,546 g m−2 d−1. Fc decreased on average by 53% over the study period, tracking the long-term decline in CO2 emissions following the last major increase that occurred at the Horseshoe Lake tree kill area from 2009 to 2011. Statistical and spectral analyses were applied to the Fc and ancillary meteorological parameter time series to understand (1) relationships between these parameters, (2) their dominant periodicities, and (3) changes in Fc that may be unexplained by meteorological forcing. Variations in detrended Fc (Fcdt) were most strongly correlated with wind direction and atmospheric temperature, followed by atmospheric pressure on diurnal to annual time scales, but wind direction likely exerted the most direct control on Fcdt. Comparison of the smoothed (180-d span) Fcdt time series to the time series of average-daily snow water equivalent measured ~1 km away suggested that snowpack may have suppressed CO2 emissions. No evidence of a change in CO2 emissions related to the last major seismic swarm beneath Mammoth Mountain on February 2–18, 2014 was observed.



中文翻译:

美国加利福尼亚州猛犸山岩浆二氧化碳排放的长期全年观测

岩浆CO 2 的扩散排放是猛犸山火山动荡的主要指标之一,但该地点存在较深的季节性积雪,阻碍了全年的CO 2通量观测。在猛犸山(马蹄湖砍树)上最大的扩散 CO 2脱气区域建立了一个永久性涡流协方差站,每半小时测量一次 CO 2通量(F c)和气象参数。从2014年7月22日到2020年5月24日,F c范围从-35到10,546 gm -2 d -1˚F ç在研究期间平均下降了 53%,跟踪了2009 年至 2011 年马蹄湖树木杀戮区上一次大幅增加后 CO 2排放量的长期下降。对F c应用了统计和光谱分析和辅助气象参数时间序列,以了解 (1) 这些参数之间的关系,(2) 它们的主要周期性,以及 (3)可能无法用气象强迫解释的F c变化。去趋势F c ( F cdt) 与风向和大气温度的相关性最强,其次是昼夜到年时间尺度上的大气压力,但风向可能对F cdt施加了最直接的控制。将平滑的(180 天跨度)F cdt时间序列与约 1 公里外测量的平均每日雪水当量的时间序列进行比较,表明积雪可能抑制了 CO 2排放。没有观察到与 2014 年 2 月 2 日至 18 日猛犸山下最后一个主要地震群相关的CO 2排放量变化的证据。

更新日期:2021-07-29
down
wechat
bug