Remotely Sensed Clear-Sky Surface Longwave Downward Radiation by Using Multivariate Adaptive Regression Splines Method

Surface radiation balance plays a vital role in the earth surface system and affects many biogeophysical processes. As one of components of surface energy balance, longwave downward radiation (LWDR) is considered as the most poorly estimated radiation component, and its uncertainty is regarded as substantially larger than other terms of surface energy budget. In this paper, we applied the multivariate adaptive regression splines (MARS) method to derive LWDR based on MODIS thermal infrared bands top of atmosphere radiances and ground-based LWDR measurements. In model fitting process, the RMSE, bias and R-square value are 25.49 W/m2, −0.000 W/m2 and 0.88, respectively; and in model validation stage, the RMSE, bias and R-square value are 25.63 W/m2, 0.481 W/m2 and 0.87, respectively. The newly proposed model demonstrates comparable accuracy with other LWDR estimating methods and proves that MARS method is very useful in remote sensing based LWDR estimation.

[1]  Shunlin Liang,et al.  A Method for Estimating Clear-Sky Instantaneous Land-Surface Longwave Radiation With GOES Sounder and GOES-R ABI Data , 2010, IEEE Geoscience and Remote Sensing Letters.

[2]  Frank J. Murcray,et al.  Measurements of the downward longwave radiation spectrum over the Antarctic Plateau and comparisons with a line-by-line , 1998 .

[3]  Shunlin Liang,et al.  An efficient hybrid method for estimating clear‐sky surface downward longwave radiation from MODIS data , 2017 .

[4]  Richard G. Allen,et al.  Satellite-Based Energy Balance for Mapping Evapotranspiration with Internalized Calibration (METRIC)—Model , 2007 .

[5]  Pedro Viterbo,et al.  The land surface‐atmosphere interaction: A review based on observational and global modeling perspectives , 1996 .

[6]  W. Oechel,et al.  FLUXNET: A New Tool to Study the Temporal and Spatial Variability of Ecosystem-Scale Carbon Dioxide, Water Vapor, and Energy Flux Densities , 2001 .

[7]  A. Ångström,et al.  A study of the radiation of the atmosphere , 2011 .

[8]  Regine Hock,et al.  Glacier melt: a review of processes and their modelling , 2005 .

[9]  Guangjian Yan,et al.  Consistent retrieval methods to estimate land surface shortwave and longwave radiative flux components under clear-sky conditions , 2012 .

[10]  Xiaotong Zhang,et al.  Review on Estimation of Land Surface Radiation and Energy Budgets From Ground Measurement, Remote Sensing and Model Simulations , 2010, IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing.

[11]  C. Long,et al.  SURFRAD—A National Surface Radiation Budget Network for Atmospheric Research , 2000 .

[12]  S. Schwartz,et al.  The Atmospheric Radiation Measurement (ARM) Program: Programmatic Background and Design of the Cloud and Radiation Test Bed , 1994 .

[13]  B. McArthur,et al.  Baseline surface radiation network (BSRN/WCRP) New precision radiometry for climate research , 1998 .

[14]  W. Brutsaert On a derivable formula for long-wave radiation from clear skies , 1975 .

[15]  Bo-Hui Tang,et al.  Estimation of instantaneous net surface longwave radiation from MODIS cloud-free data , 2008 .

[16]  J. Freidman,et al.  Multivariate adaptive regression splines , 1991 .

[17]  Shunlin Liang,et al.  Estimation of high-spatial resolution clear-sky longwave downward and net radiation over land surfaces from MODIS data , 2009 .