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How do unmodeled systematic mean sea level variations affect long-term sea level trend estimates from tide gauge data?

机译:未建模的系统平均海平面变化如何影响潮汐计数据的长期海平面趋势估计?

摘要

Although there are over 1,800 globally distributed tide gauge stations, only a few hundred of them are suitable for monitoring and analyzing global mean sea level (MSL) changes. This is because several tide gauge records span short periods of time and therefore their trend estimates are adversely affected by unmodeled systematic sea level changes such as seasonal, interannual, decadal variations. This limitation can be improved by using more elaborate models that account for systematic fluctuations in MSL for shorter time-series. In this study, analytic expressions were derived to analyze and quantify the epoch-by-epoch and lump-sum effects of these systematic changes to the local MSL trend estimates as a function of the time-series‘ lengths. The numerical results reveal that systematic MSL variations, particularly transient/episodic ones, if they are not properly modeled or omitted from the models, will bias the trend estimates for the tide gauge data series around the world by up to 0.6 mm/year for the 50-year time-series that are needed for more reliable inferences about global MSL. Random effects, which are not a factor in estimating MSL trends for the long-term (>50 years) time-series, need to be scrutinized together with the systematic errors for time-series shorter than 50 years.
机译:尽管全球共有1800多个潮位计站,但其中只有几百个适合监测和分析全球平均海平面(MSL)变化。这是因为几个潮位计记录跨越了很短的时间,因此它们的趋势估计受到未建模的系统性海平面变化(例如季节性,年际,年代际变化)的不利影响。通过使用更精细的模型可以解决此限制,该模型考虑了较短时间序列中MSL的系统波动。在这项研究中,得出了分析表达式,以分析和量化这些系统变化对本地MSL趋势估计值的逐时和一次总和效应,该效应是时间序列长度的函数。数值结果表明,如果未正确建模或未从模型中忽略系统的MSL变化,尤其是瞬态/间歇性变化,将使全球潮汐仪数据序列的趋势估计值偏差达0.6 mm /年。需要50年的时间序列,才能更可靠地推断出全局MSL。随机效应不是评估长期(> 50年)时间序列MSL趋势的因素,需要与短于50年的时间序列的系统误差一起进行仔细研究。

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    Iz BH;

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  • 年度 2006
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  • 正文语种 eng
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