Abstract

Surface longwave downward radiation (LWDR) plays a key role in determining the Arctic surface energy budget, especially in insolation-absent boreal winter. A reliable LWDR product is essential for understanding the intrinsic physical mechanisms of the rapid changes in the Arctic climate. The Medium-Resolution Spectral Imager (MERSI-2), a major payload of the Chinese second-generation polar-orbiting meteorological satellite, FengYun-3D (FY-3D), was designed similar to the NASA Moderate-Resolution Imaging Spectroradiometer (MODIS) in terms of the spectral bands. Although significant progress has been made in estimating clear-sky LWDR from MODIS observations using a variety of methods, few studies have focused on the retrieval of clear-sky LWDR from FY-3D MERSI-2 observations. In this study, we propose an advanced method to directly estimate the clear-sky LWDR in the Arctic from the FY-3D MERSI-2 thermal infrared (TIR) top-of-atmosphere (TOA) radiances and auxiliary information using the extremely randomized trees (ERT) machine learning algorithm. The retrieval accuracy of RMSE and bias, validated with the Baseline Surface Radiation Network (BSRN) in situ measurements, are 14.14 W/m2 and 4.36 W/m2, respectively, which is comparable and even better than previous studies. The scale effect in retrieval accuracy evaluation was further analyzed and showed that the validating window size could significantly influence the retrieval accuracy of the MERSI-2 clear-sky LWDR dataset. After aggregating to a spatial resolution of 9 km, the RMSE and bias of MERSI-2 retrievals can be reduced to 9.43 W/m2 and −0.14 W/m2, respectively. The retrieval accuracy of MERSI-2 clear-sky LWDR at the CERES SSF FOV spatial scale (approximately 20 km) can be further reduced to 8.64 W/m2, which is much higher than the reported accuracy of the CERES SSF products. This study demonstrates the feasibility of producing LWDR datasets from Chinese FY-3D MERSI-2 observations using machine learning methods.

Highlights

  • The surface longwave downward radiation (LWDR), which is closely related to the atmospheric greenhouse effect, is an important component for determining the Earth’s surface energy budget [1]

  • Satellite-based LWDR retrieval methods are usually grouped into three categories [8,11,12]: profile-based schemes that calculate LWDR with radiative transfer models (RTMs) and satellite-estimated atmospheric meteorological profiles [12,13,14], parameterization schemes that estimate LWDR with satellite-retrieved near-surface meteorological parameters [15], and hybrid schemes that calculate LWDR with a statistical model built with RTM-simulated LWDR and satellite-observed Top of Atmosphere (TOA)

  • It shows that the Clouds and the Earth’s Radiant Energy System (CERES) Single Scanner Footprint (SSF) FOV instantaneous clear-sky LWDR products are consistent with the ground measurements in the Arctic

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Summary

Introduction

The surface longwave downward radiation (LWDR), which is closely related to the atmospheric greenhouse effect, is an important component for determining the Earth’s surface energy budget [1]. In the insolation absent boreal winter, the LWDR emitted from the warmer and wetter atmosphere gases and clouds contributes most incoming energy to the Arctic surface [2]. Whether this results from either the enhanced greenhouse effect of increased water vapor and clouds [3,4] or the lapse-rate feedback of the Arctic boundary temperature inversion [5,6] is still under debate, increased LWDR was suggested to play a key role in driving Arctic wintertime warming and spring sea-ice initial melting [2,3,4,7] in recent decades. Satellite-based LWDR retrieval methods are usually grouped into three categories [8,11,12]: profile-based schemes that calculate LWDR with radiative transfer models (RTMs) and satellite-estimated atmospheric meteorological profiles [12,13,14], parameterization schemes that estimate LWDR with satellite-retrieved near-surface meteorological parameters [15], and hybrid schemes that calculate LWDR with a statistical model built with RTM-simulated LWDR and satellite-observed Top of Atmosphere (TOA)

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