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The impact of water loading on postglacial decay times in Hudson Bay

机译:水荷载对哈德森湾后爆炸衰减时间的影响

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Ongoing glacial isostatic adjustment (GIA) due to surface loading (ice and water) variations during the last glacial cycle has been contributing to sea-level changes globally throughout the Holocene, especially in regions like Canada that were heavily glaciated during the Last Glacial Maximum (LGM). The spatial and temporal distribution of GIA, as manifested in relative sea-level (RSL) change, are sensitive to the ice history and the rheological structure of the solid Earth, both of which are uncertain. It has been shown that RSL curves near the center of previously glaciated regions with no ongoing surface loading follow an exponential-like form, with the postglacial decay times associated with that form having a weak sensitivity to the details of the ice loading history. Postglacial decay time estimates thus provide a powerful datum for constraining the Earth's viscous structure and improving GIA predictions. We explore spatial patterns of postglacial decay time predictions in Hudson Bay by decomposing numerically modeled RSL changes into contributions from water and ice loading effects, and computing their relative impact on the decay times. We demonstrate that ice loading can contribute a strong geographic trend on the decay time estimates if the time window used to compute decay times includes periods that are temporally close to (i.e. contemporaneous with, or soon after) periods of active loading. This variability can be avoided by choosing a suitable starting point for the decay time window. However, more surprisingly, we show that across any adopted time window, water loading effects associated with inundation into, and postglacial flux out of, Hudson Bay and James Bay will impart significant geographic variability onto decay time estimates. We emphasize this issue by considering both maps of predicted decay times across the region and site-specific estimates, and we conclude that variability in observed decay times (whether based on existing or future data
机译:由于表面负载(冰和水)在最后一次冰川周期中的表面装载(冰和水)变化导致的冰川等静态调整(GIA)在全新的全新世中,在全球范围内的海上变化,特别是在加拿大等地区,这些地区在最后冰川最大冰川最大值( LGM)。 GIA的空间和时间分布,如相对海平(RSL)变化,对固体地球的冰历史和流变结构敏感,这两者都不确定。已经表明,RSL曲线附近的先前冰川地区的中心,没有持续的表面装载,遵循指数相似的形式,与对冰负荷历史细节的细节具有较弱的敏感性的外阴衰减时间。冰后期衰减时间从而估计用于约束地球的粘性结构,提高GIA预测提供了有力的数据。我们通过将数值模型的RSL变为水和冰负荷效应的贡献来探讨哈德森海湾的后闪烁时间预测的空间模式,并计算它们对衰减时间的相对影响。我们证明冰负载可以在衰减时间估计的情况下,如果用于计算衰减次数的时间窗口包括在活动负载期间时间靠近的时间窗口的时间窗口包括时间窗口的时间窗口。通过为衰减时间窗口选择合适的起点,可以避免这种可变性。然而,更令人惊讶的是,我们表明,在任何采用的时间窗口中,与淹没的水量造成效应,哈德森湾和詹姆斯海湾的淹没和后闪烁通量将赋予衰减时间估计来赋予显着的地理变异性。我们通过考虑地区的预测衰减时间的地图和特定于地的估计,我们强调了这个问题,我们得出了观察到衰减时间的可变性(无论是基于现有或未来的数据

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