Analysis of Sea Surface Temperature due to Climate Change using Satellite Products and Spatial Gap-filling Approaches

Jihye Ahn, Yang-Jae Lee
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Abstract

Sea Surface Temperature(SST) is crucial for atmosphere-ocean interaction and one of the essential factor for the Earth system. The distribution and characteristics of SST have been used in various fields such as climate modeling, global heat balance, weather forecasting, atmospheric and ocean circulation, and ocean data assimilation. Global SST is on the rise due to climate change, and this change can be observed with satellites. Currently, Geostationary Korea Multi-Purpose Satellite-2A(GK2A) daily SST product is provided for East Asia. However, the SST value based on infrared sensors is missing in the case of sea areas where clouds or aerosols appear continuously. Since these missing data increase the uncertainty of the satellite product, it is necessary to improve it in order to expand the use of SST product. Therefore, this study aims to produce high-quality gap-free SST data for climate change monitoring in East Asian Seas. For this purpose, three steps of outlier removal, spatial gap-filling techniques, and validation with in-situ observations were applied. Outlier detection was performed using Deviation from Spatial Autocorrelation Trend(DSAT) [1]. DSAT detects extreme outliers with exceptional characteristics when compared to neighboring pixels. Our spatial gap-filling approaches were based on statistics such as Multiple Linear Regression(MLR) and Regression Kriging(RK). These regression techniques used the relation between SST with meteorological factors like temperature, humidity, and wind speeds, etc. Specifically, RK was performed through the following procedure [2].
基于卫星产品和空间缺口填补方法的气候变化海表温度分析
海温是大气-海洋相互作用的关键因素,也是地球系统的重要因子之一。海温的分布和特征已被用于气候模拟、全球热平衡、天气预报、大气和海洋环流以及海洋资料同化等多个领域。由于气候变化,全球海温呈上升趋势,这种变化可以通过卫星观测到。目前,地球同步韩国多用途卫星2a (GK2A)为东亚地区提供每日海温产品。然而,在云或气溶胶连续出现的海域,红外传感器的海温值缺失。由于这些缺失的数据增加了卫星产品的不确定性,为了扩大海表温度产品的使用,有必要对其进行改进。因此,本研究旨在为东亚海域气候变化监测提供高质量的无间隙海温数据。为此,应用了三个步骤:异常值去除、空间空白填充技术和原位观测验证。使用偏离空间自相关趋势(DSAT)进行离群值检测[1]。与相邻像素相比,DSAT检测到具有异常特征的极端异常值。我们的空间空白填充方法基于多元线性回归(MLR)和回归克里金(RK)等统计数据。这些回归技术利用海温与温度、湿度、风速等气象因子的关系。具体来说,RK是通过以下程序进行的[2]。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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