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首页> 外文期刊>Climate of the past >The SP19 chronology for the South Pole Ice Core – Part 2: gas chronology, Δage, and smoothing of atmospheric records
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The SP19 chronology for the South Pole Ice Core – Part 2: gas chronology, Δage, and smoothing of atmospheric records

机译:南极冰芯的SP19年表 - 第2部分:气体年表,ΔAge和大气记录的平滑

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A new ice core drilled at the South Pole provides a 54?000-year paleoenvironmental record including the composition of the past atmosphere. This paper describes the SP19 chronology for the South Pole atmospheric gas record and complements a previous paper (Winski et al., 2019) describing the SP19 ice chronology. The gas chronology is based on a discrete methane (CH 4 ) record with 20- to 190-year resolution. To construct the gas timescale, abrupt changes in atmospheric CH 4 during the glacial period and centennial CH 4 variability during the Holocene were used to synchronize the South Pole gas record with analogous data from the West Antarctic Ice Sheet Divide ice core. Stratigraphic matching based on visual optimization was verified using an automated matching algorithm. The South Pole ice core recovers all expected changes in CH 4 based on previous records. Gas transport in the firn results in smoothing of the atmospheric gas record with a smoothing function spectral width that ranges from 30 to 78 years, equal to 3?% of the gas-age–ice-age difference, or Δ age. The new gas chronology, in combination with the existing ice age scale from Winski et al. (2019), allows a model-independent reconstruction of the gas-age–ice-age difference through the whole record, which will be useful for testing firn densification models.
机译:在南极钻的新冰芯提供了54 000年的古环境记录,包括过去大气的组成。本文介绍了南极大气气体记录的SP19年表,并补充了前一篇论文(Winski等,2019),描述了SP19冰时间。气体时间量基于分立甲烷(CH 4)记录,具有20至190年的分辨率。为了构建气体时间尺度,在冰川期间和全新世期间百年云期间和百年CH 4可变性的突然变化用于将南极气体记录与西南冰冰片分冰芯的类似数据同步。使用自动匹配算法验证了基于可视优化的基于视觉优化的地层匹配。南极冰芯根据以前的记录恢复了CH 4的所有预期变化。 FIRN中的气体运输导致大气的气体记录平滑,具有平滑的功能光谱宽度,范围为30至78岁,等于气体年龄差异的3?%或δ年龄。新的气体年表,与Winski等人的现有冰河年龄相结合。 (2019),允许通过整个记录进行模型 - 自然重建煤气时代冰差,这对于测试FiRN致密化模型将是有用的。

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