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A new global gridded sea surface temperature data product based on multisource data

机译:基于多源数据的全球网格表面温度数据产品

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Sea surface temperature (SST) is an important geophysical parameter that is essential for studying global climate change. Although sea surface temperature can currently be obtained through a variety of sensors (MODIS, AVHRR, AMSR-E, AMSR2, WindSat, in situ sensors), the temperature values obtained by different sensors come from different ocean depths and different observation times, so different temperature products lack consistency. In addition, different thermal infrared temperature products have many invalid values due to the influence of clouds, and passive microwave temperature products have very low resolutions. These factors greatly limit the applications of ocean temperature products in practice. To overcome these shortcomings, this paper first took MODIS SST products as a reference benchmark and constructed a temperature depth and observation time correction model to correct the influences of the different sampling depths and observation times obtained by different sensors. Then, we built a reconstructed spatial model to overcome the effects of clouds, rainfall, and land interference that makes full use of the complementarities and advantages of SST data from different sensors. We applied these two models to generate a unique global 0.041 ° gridded monthly SST product covering the years 2002–2019. In this dataset, approximately 25?% of the invalid pixels in the original MODIS monthly images were effectively removed, and the accuracies of these reconstructed pixels were improved by more than 0.65? ° C compared to the accuracies of the original pixels. The accuracy assessments indicate that the reconstructed dataset exhibits significant improvements and can be used for mesoscale ocean phenomenon analyses. The product will be of great use in research related to global change, disaster prevention, and mitigation and is available at https://doi.org/10.5281/zenodo.4419804 (Cao et al., 2021a).
机译:海表面温度(SST)是一个重要的地球物理参数,对于研究全球气候变化至关重要。虽然目前可以通过各种传感器(MODIS,AVHRR,AMSR-E,AMSR2,Windsat,原位传感器)获得海表面温度,但不同传感器获得的温度值来自不同的海洋深度和不同的观察时间,如此不同温度产品缺乏一致性。此外,由于云的影响,不同的热红外温度产品具有许多无效值,并且被动微波温度产品具有非常低的分辨率。这些因素极大地限制了海洋温度产品在实践中的应用。为了克服这些缺点,本文首先将MODIS SST产品作为参考基准,并构建了温度深度和观察时间校正模型,以校正不同的采样深度和由不同传感器获得的观察时间的影响。然后,我们建立了一个重建的空间模型,以克服云,降雨和土地干扰的影响,从而充分利用来自不同传感器的SST数据的互补性和优点。我们应用这两款模型,以产生2002 - 2019年的独特全球0.04​​1°覆盖的月度SST产品。在该数据集中,有效地删除了原始MODIS每月图像中的无效像素的大约25?%,并且这些重建像素的精度提高了大于0.65? °C与原始像素的准确性相比。准确性评估表明,重建的数据集表现出显着的改进,可用于Mescale海洋现象分析。该产品在与全球变革,防灾和缓解相关的研究中,可以在HTTPS://doi.org/10.5281/zenodo.4419804(Cao等,2021a)中使用。

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