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Assessing trends and uncertainties in satellite-era ocean chlorophyll using space-time modeling

机译:使用时效模型评估卫星时代海洋叶绿素的趋势和不确定性

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The presence, magnitude, and even direction of long-term trends in phytoplankton abundance over the past few decades are still debated in the literature, primarily due to differences in the data sets and methodologies used. Recent work has suggested that the satellite chlorophyll record is not yet long enough to distinguish climate change trends from natural variability, despite the high density of coverage in both space and time. Previous work has typically focused on using linear models to determine the presence of trends, where each grid cell is considered independently from its neighbors. However, trends can be more thoroughly evaluated using a spatially resolved approach. Here a Bayesian hierarchical spatiotemporal model is fitted to quantify trends in ocean chlorophyll from September 1997 to December 2013. The approach used in this study explicitly accounts for the dependence between neighboring grid cells, which allows us to estimate trend by "borrowing strength" from the spatial correlation. By way of comparison, a model without spatial correlation is also fitted. This results in a notable loss of accuracy in model fit. Additionally, we find an order of magnitude smaller global trend, and larger uncertainty, when using the spatiotemporal model: -0.023 +/- 0.12% yr(-1) as opposed to -0.38 +/- 0.045% yr(-1) when the spatial correlation is not taken into account. The improvement in accuracy of trend estimates and the more complete account of their uncertainty emphasize the solution that space-time modeling offers for studying global long-term change.
机译:在过去几十年中,浮游植物丰富的长期趋势的存在,幅度和均匀的方向在文献中仍然争论,主要是由于数据集和使用方法的差异。最近的工作表明,尽管空间和时间的覆盖率高,但卫星叶绿素记录尚未足够长,以区分气候变化趋势。以前的工作通常集中在使用线性模型来确定存在趋势的存在,其中每个网格小区独立于其邻居考虑。但是,可以使用空间解决方法更彻底地评估趋势。在这里,贝叶斯等级时空模型适用于1997年9月至2013年12月的海洋叶绿素的趋势。本研究中使用的方法明确地占邻近网格细胞之间的依赖,这使我们能够通过“借用力量”来估算趋势空间相关性。通过比较,也装配了没有空间相关的模型。这导致模型适合中的值得注意的准确性损失。此外,我们发现数量级别较小的全球趋势,更大的不确定性,当使用时空模型时:-0.023 +/- 0.12%YR(-1),而不是-0.38 +/- 0.045%YR(-1)不考虑空间相关性。趋势估计准确性的提高和更完全陈述的不确定性强调了用于研究全球长期变化的时空建模优惠。

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