Abstract

Land surface temperature (LST) is used as a critical indicator for various environmental issues because it links land surface fluxes with the surface atmosphere. Moderate-resolution imaging spectroradiometers (MODIS) 1 km LSTs have been widely utilized but have the serious limitation of not being provided under cloudy weather conditions. In this study, we propose two schemes to estimate all-weather 1 km Aqua MODIS daytime (1:30 p.m.) and nighttime (1:30 a.m.) LSTs in South Korea for humid summer days. Scheme 1 (S1) is a two-step approach that first estimates 10 km LSTs and then conducts the spatial downscaling of LSTs from 10 km to 1 km. Scheme 2 (S2), a one-step algorithm, directly estimates the 1 km all-weather LSTs. Eight advanced microwave scanning radiometer 2 (AMSR2) brightness temperatures, three MODIS-based annual cycle parameters, and six auxiliary variables were used for the LST estimation based on random forest machine learning. To confirm the effectiveness of each scheme, we have performed different validation experiments using clear-sky MODIS LSTs. Moreover, we have validated all-weather LSTs using bias-corrected LSTs from 10 in situ stations. In clear-sky daytime, the performance of S2 was better than S1. However, in cloudy sky daytime, S1 simulated low LSTs better than S2, with an average root mean squared error (RMSE) of 2.6 °C compared to an average RMSE of 3.8 °C over 10 stations. At nighttime, S1 and S2 demonstrated no significant difference in performance both under clear and cloudy sky conditions. When the two schemes were combined, the proposed all-weather LSTs resulted in an average R2 of 0.82 and 0.74 and with RMSE of 2.5 °C and 1.4 °C for daytime and nighttime, respectively, compared to the in situ data. This paper demonstrates the ability of the two different schemes to produce all-weather dynamic LSTs. The strategy proposed in this study can improve the applicability of LSTs in a variety of research and practical fields, particularly for areas that are very frequently covered with clouds.

Highlights

  • Land surface temperature (LST) is the radiative temperature of the land surface, which plays a crucial role in understanding various environmental problems such as heatwaves, drought, wildfire, air quality, and urban heat islands [1,2,3,4,5,6,7]

  • We used eight advanced microwave scanning radiometer 2 (AMSR2) Brightness temperature (BT), three annual cycle parameters (ACPs) (i.e., mean annual surface temperature (MAST), Yast, and theta), and six auxiliary variables for the LST estimations based on Random Forest (RF) machine learning

  • Scheme 2 (S2) is a one-step algorithm that directly estimates the 1 km all-weather LSTs, which we have evaluated using a series of validations

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Summary

Introduction

Land surface temperature (LST) is the radiative temperature of the land surface, which plays a crucial role in understanding various environmental problems such as heatwaves, drought, wildfire, air quality, and urban heat islands [1,2,3,4,5,6,7]. It is important to obtain accurate LST over large areas on both high spatial and temporal domains. With the continued development of remote sensing technology, LST has been retrieved from satellite data for large areas with high temporal and spatial resolution. Thermal infrared (TIR) sensors are the most widely used in producing satellite-based LST. Several algorithms, such as single-channel, split-window, and temperature and emissivity separation (TES) techniques, have been developed to provide TIR-based LST [11]. LST products are provided by several other TIR sensors with different specifications in both low earth orbit and geostationary orbit satellites: The visible infrared imaging radiometer suite (VIIRS), spinning enhanced visible and infrared imager (SEVIRI), and advanced spaceborne thermal emission and reflection radiometer (ASTER). Some studies have been conducted to fill the gaps in LST data caused by clouds [12,13,14,15,16,17,18,19,20,21,22,23,24,25,26]

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