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An improved methodology for deriving high‐resolution surface shortwave radiative fluxes from MODIS in the Arctic region
Author(s) -
Niu Xiaolei,
Pinker Rachel T.
Publication year - 2015
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
eISSN - 2169-8996
pISSN - 2169-897X
DOI - 10.1002/2014jd022151
Subject(s) - shortwave , environmental science , arctic , standard deviation , irradiance , albedo (alchemy) , moderate resolution imaging spectroradiometer , atmospheric sciences , climatology , latitude , shortwave radiation , radiative flux , radiative transfer , mean radiant temperature , climate change , geology , statistics , mathematics , satellite , geodesy , physics , oceanography , art , quantum mechanics , astronomy , performance art , radiation , art history
The Arctic is experiencing an unprecedented increase in surface air temperature and decrease in sea ice extent. The causes of these changes are still being debated; radiative fluxes are believed to play an important role in this warming. The primary motivation for this study is to advance the quality and resolution of currently available information on surface shortwave (solar) irradiance (SWR) for the Arctic. Such information is needed to meet the challenge for accurate estimates of heat input into the open waters. An inference scheme that utilizes the Moderate Resolution Imaging Spectroradiometer (MODIS) observations is optimized for high latitudes and implemented at 5 km for 2007 at an hourly time scale. Evaluation of the 5 km based SWR estimates against hourly ground observations at Barrow site shows a mean bias of 7.9 W m −2 (3% of mean values), a standard deviation of 58.2 W m −2 (23% of mean value), and a high correlation of 0.95. Evaluation of the SWR estimates against daily ground measurements at these latitudes shows good agreement with surface observations at three sites, with a mean bias of 1.9 W m −2 (1.1% of mean values), a standard deviation of 31.5 W m −2 (17.8% of mean value), and a high correlation of 0.96. Information at this high resolution and good quality can lead to improved estimates of heat input into the complex Arctic domain. For the Beaufort Sea domain (70°N–80°N, 120°E–50°E), the differences can amount to 116 MJ m −2 (~7%) of the total solar input of this region.