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首页> 外文期刊>Advances in Water Resources >A new approach to simulating stream isotope dynamics using Markov switching autoregressive models
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A new approach to simulating stream isotope dynamics using Markov switching autoregressive models

机译:使用马尔可夫切换自回归模型模拟流同位素动力学的新方法

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In this study we applied Markov switching autoregressive models (MSARMs) as a proof-of-concept to analyze the temporal dynamics and statistical characteristics of the time series of two conservative water isotopes, deuterium (δ~2H) and oxygen-18 (δ~(18)O), in daily stream water samples over two years in a small catchment in eastern Scotland. MSARMs enabled us to explicitly account for the identified non-linear, non-Normal and non-stationary isotope dynamics of both time series. The hidden states of the Markov chain could also be associated with meteorological and hydrological drivers identifying the short (event) and longer-term (inter-event) transport mechanisms for both isotopes. Inference was based on the Bayes-ian approach performed through Markov Chain Monte Carlo algorithms, which also allowed us to deal with a high rate of missing values (17%). Although it is usually assumed that both isotopes are conservative and exhibit similar dynamics, δ~(18)O showed somewhat different time series characteristics. Both isotopes were best modelled with two hidden states, but δ~(18)O demanded autoregressions of the first order, whereas δ~2H of the second. Moreover, both the dynamics of observations and the hidden states of the two isotopes were explained by two different sets of covariates. Consequently use of the two tracers for transit time modelling and hydrograph separation may result in different interpretations on the functioning of a catchment system.
机译:在这项研究中,我们使用马尔可夫切换自回归模型(MSARM)作为概念验证,以分析两种保守水同位素氘(δ〜2H)和氧18(δ〜 (18)O),在苏格兰东部的一个小流域中,在两年的日常水流样本中。 MSARM使我们能够明确考虑两个时间序列中已识别的非线性,非正态和非平稳同位素动力学。马尔可夫链的隐藏状态还可能与确定这两种同位素的短期(事件)和长期(事件间)传输机制的气象和水文驱动因素有关。推论基于通过马尔可夫链蒙特卡洛算法执行的贝叶斯方法,这也使我们能够处理较高的漏失率(17%)。尽管通常认为两种同位素都是保守的并且表现出相似的动力学,但δ〜(18)O的时间序列特性却有所不同。最好用两个隐藏状态对两种同位素建模,但是δ〜(18)O要求一阶自回归,而δ〜2H则要求二阶。此外,观测的动力学和两种同位素的隐藏状态都由两组不同的协变量来解释。因此,将两个示踪剂用于渡越时间建模和水文分离可能会导致对集水系统功能的不同解释。

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