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A first chronology for the North Greenland Eemian Ice Drilling (NEEM) ice core

机译:北格陵兰Eemian冰钻(NEEM)冰芯的第一个年代

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A stratigraphy-based chronology for the North Greenland Eemian Ice Drilling(NEEM) ice core has been derived by transferring the annual layer countedGreenland Ice Core Chronology 2005 (GICC05) and its model extension(GICC05modelext) from the NGRIP core to the NEEM core using 787 match pointsof mainly volcanic origin identified in the electrical conductivitymeasurement (ECM) and dielectrical profiling (DEP) records. Tephra horizonsfound in both the NEEM and NGRIP ice cores are used to test the matchingbased on ECM and DEP and provide five additional horizons used for the timescale transfer.A thinning function reflecting the accumulated strain along the core hasbeen determined using a Dansgaard–Johnsen flow model and anisotope-dependent accumulation rate parameterization. Flow parameters aredetermined from Monte Carlo analysis constrained by the observed depth-agehorizons.In order to construct a chronology for the gas phase, the ice age–gas agedifference (Δage) has been reconstructed using a coupled firndensification-heat diffusion model. Temperature and accumulation inputs tothe Δage model, initially derived from the water isotope proxies, havebeen adjusted to optimize the fit to timing constraints from δ15Nof nitrogen and high-resolution methane data during the abrupt onset ofGreenland interstadials.The ice and gas chronologies and the corresponding thinning functionrepresent the first chronology for the NEEM core, namedGICC05modelext-NEEM-1. Based on both the flow and firn modelling results,the accumulation history for the NEEM site has been reconstructed. Together,the timescale and accumulation reconstruction provide the necessary basisfor further analysis of the records from NEEM.
机译:通过将787年格陵兰冰芯年代年鉴(GICC05)及其模型扩展(GICC05modelext)从NGRIP核心转移到NEEM核心,得出了北格陵兰Eemian冰钻(NEEM)冰芯的基于地层的年代学。在电导率测量(ECM)和电介质分析(DEP)记录中识别出的主要火山成因的匹配点。在NEEM和NGRIP冰芯中发现的Tephra地层被用于测试基于ECM和DEP的匹配,并提供了用于时间尺度转移的另外五个地层。 Dansgaard-Johnsen流模型和与同位素有关的累积速率参数化。流动参数由蒙特卡洛分析法确定,并受观测到的深度-年龄的约束。 为了构造气相的年代学,我们使用了耦合的菲氏化-热来重建冰龄-气体的年龄差异(Δage)。扩散模型。最初从水同位素代理得出的Δage模型的温度和累积输入已进行调整,以优化格陵兰间质突然爆发期间氮的δ 15 和高分辨率甲烷数据对时序约束的拟合。 冰和天然气年代学以及相应的稀疏功能代表了NEEM岩心的第一个年代学,命名为GICC05modelext-NEEM-1。根据流场和模型模拟的结果,重建了NEEM站点的堆积历史。时间尺度和累积重建共同为进一步分析NEEM的记录提供了必要的基础。

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