Abstract

The MODIS land surface temperature (LST) products contain large areas of missing data due to cloud contamination. Interpolating clear-sky equivalent LSTs on those areas is a first step in a stepwise approach toward fully recovering missing data. A previous study (viz. the Yu method) has implemented an effective clear-sky interpolation method, especially targeting large-area missing data. The Yu method postulates several global reference LST images that contain over 90% of valid pixels and that are assumed to have a close statistical relationship to the interpolated images. However, in practice, such reference images are rarely available throughout a one-year cycle, and the time gaps between the available reference images and the interpolated images are often huge, resulting in compromised interpolation accuracy. In this study, we intended to address those weaknesses and propose a novel clear-sky interpolation approach. The proposed approach uses multiple temporally proximate images as reference images, with which multiple initial estimates are made by an empirically orthogonal function method and then fused by a Bayesian approach to achieve a best estimate. The proposed approach was compared through two experiments to the Yu method and two other widely used methods, i.e., harmonic analysis of time series and co-kriging. Both experiments demonstrate the superiority of the proposed approach over those established methods, as evidenced by higher spatial correlation coefficients (0.90-0.94) and lower root-mean-square errors (1.19-3.64 °C) it achieved when measured against the original data that were intentionally removed.

Highlights

  • IntroductionManuscript received August 26, 2020; revised October 11, 2020; accepted November 11, 2020

  • L AND surface temperature (LST) is a key variable for monitoring surface energy budget, determined by the landManuscript received August 26, 2020; revised October 11, 2020; accepted November 11, 2020

  • CoK results [see Figs. 3(e) and 4(e)] exhibit many strange patterns, especially in the northwest and southern Qinghai-Tibet Plateau (QTP) on the nighttime image and in the central zone of QTP on the daytime image. Those artifacts expose a critical weakness in CoK, as shown with the QTP examples, for interpolating extensive missing data even if the digital elevation model (DEM) is used as a covariant

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Summary

Introduction

Manuscript received August 26, 2020; revised October 11, 2020; accepted November 11, 2020. Date of publication November 16, 2020; date of current version January 6, 2021. It is widely used in a variety of studies including climate change, hydrological cycle, vegetation monitoring, and ecosystem assessment [1]–[3]. The MODIS LST products contain a large portion of missing data as a result of cloud contamination, high aerosol content, sensor failure, and quality control. The average cloud coverage amounts to more than 50% on the Qinghai-Tibet Plateau (QTP) [7], [8]

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