Algorithm for estimating sea surface temperatures based on Aqua/MODIS global ocean data. 2. Automated quality check process for eliminating cloud contamination

Kohtaro Hosoda

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Algorithm for estimating sea surface temperatures based on Aqua/MODIS global ocean data. 2. Automated quality check process for eliminating cloud contamination

机译：基于Aqua / MODIS全球海洋数据的海面温度估算算法。 2.自动化的质量检查流程，消除了云污染

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This study developed a post-processing quality check (QC) process to eliminate cloud contamination in infrared sea surface temperature (SST) without manual handling. Cloudiness of a pixel was evaluated quantitatively, in which the graduated verifications and a comprehensive decision from a combination of several tests were conducted. Additionally, the quality of SST data at the pixel was measured by acceptable limits from reference SST, which were obtained from historical data. The QC processed data showed good accuracy below 0.8°C, even in the near-cloud area. Before the QC, their accuracies including near-cloud areas were as poor as 2–5°C.

机译：这项研究开发了一种后处理质量检查（QC）工艺，无需人工操作即可消除红外海面温度（SST）中的云污染。对像素的白浊度进行了定量评估，其中进行了分级验证，并结合了多种测试进行了综合决策。另外，像素的SST数据质量是通过从历史数据获得的参考SST可接受的限值来测量的。经过QC处理的数据显示，即使在近云区域，在0.8°C以下仍具有良好的精度。在质量控制之前，他们的精度（包括近云区域）低至2–5°C。

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《Journal of oceanography》 |2011年第6期|共15页
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Kohtaro Hosoda;
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中图分类海洋学;
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1. Algorithm for estimating sea surface temperatures based on Aqua/MODIS global ocean data. 2. Automated quality check process for eliminating cloud contamination [J] . Kohtaro Hosoda Journal of oceanography . 2011,第6期

机译：基于Aqua / MODIS全球海洋数据的海面温度估算算法。 2.自动化的质量检查流程，消除了云污染
2. Algorithm for estimating sea surface temperatures based on Aqua/MODIS global ocean data. 1. Development and validation of the algorithm [J] . Kohtaro Hosoda, Huiling Qin Journal of oceanography . 2011,第1期

机译：基于Aqua / MODIS全球海洋数据的海面温度估算算法。 1.算法的开发与验证
3. Algorithm for estimating sea surface temperatures based on Aqua/MODIS global ocean data. 1. Development and validation of the algorithm [J] . Kohtaro Hosoda, Huiling Qin Journal of oceanography . 2011,第1期

机译：基于Aqua / MODIS全球海洋数据的海面温度估算算法。 1.算法的开发与验证
4. Sea surface temperature and ocean colour (MODIS/AQUA) space and time variability in Indonesian Sea coral reef systems from 2002 to 2011 [C] . A. R. Polonia, M. Figueiredo, D. F. R. Cleary, Conference on remote sensing of the ocean, sea ice, coastal waters, and large water regions . 2012

机译：2002年至2011年印度尼西亚海珊瑚礁系统的海面温度和海洋颜色（MODIS / AQUA）时空变化
5. An Algorithm for Automated Satellite-Based River Ice Identification Using a Local Cloud Mask: Application over the Lower Susquehanna River Using VIIRS and MODIS [D] . Kraatz, Simon G. 2017

机译：一种使用局部云掩码的基于卫星的河冰自动识别算法：使用VIIRS和MODIS在萨斯奎哈纳河下游应用
6. Differences in liquid cloud droplet effective radius and number concentration estimates between MODIS Collections 5.1 and 6 over global oceans [O] . John Rausch, Kerry Meyer, Ralf Bennartz, -1

机译：MODIS Collections 5.1和6在全球海洋中液态云滴有效半径和数量浓度估计值的差异
7. The oceans mediate the response of global climate to natural and anthropogenic forcings. Yet for the past 2,000 years — a key interval for understanding the present and future climate response to these forcings — global sea surface temperature changes and the underlying driving mechanisms are poorly constrained. Here we present a global synthesis of sea surface temperatures for the Common Era (ce) derived from 57 individual marine reconstructions that meet strict quality control criteria. We observe a cooling trend from 1 to 1800 ce that is robust against explicit tests for potential biases in the reconstructions. Between 801 and 1800 ce, the surface cooling trend is qualitatively consistent with an independent synthesis of terrestrial temperature reconstructions, and with a sea surface temperature composite derived from an ensemble of climate model simulations using best estimates of past external radiative forcings. Climate simulations using single and cumulative forcings suggest that the ocean surface cooling trend from 801 to 1800 ce is not primarily a response to orbital forcing but arises from a high frequency of explosive volcanism. Our results show that repeated clusters of volcanic eruptions can induce a net negative radiative forcing that results in a centennial and global scale cooling trend via a decline in mixed-layer oceanic heat content. [O] . McGregor, Helen V., Evans, Michael N., Goosse, Hugues, 2015

机译：海洋调节了全球气候对自然和人为强迫的响应。然而，在过去的2,000年中（这是了解当前和未来气候对这些强迫的响应的关键间隔），全球海表温度变化及其潜在的驱动机制受到的约束很有限。在这里，我们提出了一个共同的时期（ce）的全球海面温度的全球综合，该综合来自57个符合严格质量控制标准的海洋重建项目。我们观察到从1到1800 ce的冷却趋势，对于显式测试重建中潜在的偏倚而言，该趋势很稳健。在801至1800 ce之间，表面降温趋势在质量上与地面温度重建的独立合成以及从使用过去外部辐射强迫的最佳估计的气候模型模拟集合推导出的海面温度合成在质量上是一致的。使用单一和累积强迫的气候模拟表明，从801到1800 ce的海洋表面冷却趋势主要不是对轨道强迫的反应，而是爆炸性火山爆发的频繁发生。我们的结果表明，火山喷发的反复簇可引起净的负辐射强迫，这会导致混合层海洋热量降低而导致百年和全球规模的降温趋势。
8. Comparison of Observed Data and GDEM (Generalized Digital Environmental Model)/Standard Ocean Data. Part 2. Monthly Sea Surface Temperature (SST) Plots and Temperature/Salinity Vertical Cross-Sections Along Great Circle Tracks in the Mediterranean Sea. [R] . Hashimoto, E., Daubin, S. C. 1983

机译：观测数据与GDEm（广义数字环境模型）/标准海洋数据的比较。第2部分。地中海沿大圆轨道的月海表温度（ssT）图和温度/盐度垂直横截面。

Algorithm for estimating sea surface temperatures based on Aqua/MODIS global ocean data. 2. Automated quality check process for eliminating cloud contamination

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