Abstract

Surface-upwelling longwave radiation (LWUP) is an important component of the surface radiation budget. Under the general framework of the hybrid method, the linear models and the multivariate adaptive regression spline (MARS) models are developed to estimate the 750 m instantaneous clear-sky LWUP from the top-of-atmosphere (TOA) radiance of the Visible Infrared Imaging Radiometer Suite (VIIRS) channels M14, M15, and M16. Comprehensive radiative transfer simulations are conducted to generate a huge amount of representative samples, from which the linear model and the MARS model are derived. The two models developed are validated by the field measurements collected from seven sites in the Surface Radiation Budget Network (SURFRAD). The bias and root-mean-square error (RMSE) of the linear models are −4.59 W/m2 and 16.15 W/m2, whereas those of the MARS models are −5.23 W/m2 and 16.38 W/m2, respectively. The linear models are preferable for the production of the operational LWUP product due to its higher computational efficiency and acceptable accuracy. The LWUP estimated by the linear models developed from VIIRS is compared to that retrieved from the Moderate Resolution Imaging Spectroradiometer (MODIS). They agree well with each other with bias and RMSE of −0.15 W/m2 and 25.24 W/m2 respectively. This is the first time that the hybrid method has been applied to globally estimate clear-sky LWUP from VIIRS data. The good performance of the developed hybrid method and consistency between VIIRS LWUP and MODIS LWUP indicate that the hybrid method is promising for producing the long-term high spatial resolution environmental data record (EDR) of LWUP.

Highlights

  • The surface radiation budget (SRB) is an important indicator in the study of climate formation and change and environmental prediction, which plays a key role in the global matter, energy cycles and interactions between the surface and the atmosphere system [1,2,3]

  • We have developed a hybrid method for retrieving clear-sky longwave upwelling radiation (LWUP) from Moderate Resolution Imaging Spectroradiometer (MODIS) data and produced two years’ global LWUP product recently [12]

  • A huge amount of representative samples are generated by extensive radiative transfer modeling; the linear model and Multivariate Adaptive Regression Spline (MARS) model are established to predict LWUP using TOA radiance of channels M14, M15 and M16

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Summary

Introduction

The surface radiation budget (SRB) is an important indicator in the study of climate formation and change and environmental prediction, which plays a key role in the global matter, energy cycles and interactions between the surface and the atmosphere system [1,2,3]. Surface-upwelling longwave radiation (LWUP, 4.0–100 μm), the sum of thermal radiation emitted by the surface and reflected atmospheric downward longwave radiation, is the main cause of surface cooling in the clear night sky and is an indirect indicator of surface temperature [5]. An accurate estimate of LWUP is Remote Sens. 2 of 17 2 of 16 ocnoeoloinf gthienptrheerecqleuairsinteigshfotrskoybtaanindinisgaalcscouarnatienwdieraetchteirnfdoirceactaosrtso,fcsluimrfaatceestiemmuplaetriaotnusr,ea[n5d].lAannda-scucurfraactee persoticmesastesimofulLaWtioUnPs. is one of the prerequisites for obtaining accurate weather forecasts, climate simuGlaetnioenrasl,layn, wd elacnadn-soubrtfaaicnetpheroLcWesUs sPimusuilnagtitohnrse.e approaches: field measurement, satellite remote sensinGgenaenrdalmlyo, dweel cparnedoibcttaioinn.thLeWLUWPUcPanubsienagctchurreaetealpypmroeaacshuerse:dfiweldithmfieealsdurinemstreunmt, esanttesl.liHteorwemevoetre, fiseenldsinnegtwanodrkms oadreelspparersdeilcytidonis.trLiWbuUtePdcgalnobbaellayc.cFuurrattheelyrmmoeraes,ufireelddwmiethasfuierledmiennsttrcuamneonntlsy. The hybrid method has been successfully used to produce high spatial-resolution regional [7,11,21] and global [12] LWUP recently

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