Articles | Volume 15, issue 11
https://doi.org/10.5194/essd-15-5207-2023
https://doi.org/10.5194/essd-15-5207-2023
Data description paper
 | 
28 Nov 2023
Data description paper |  | 28 Nov 2023

Quality-controlled meteorological datasets from SIGMA automatic weather stations in northwest Greenland, 2012–2020

Motoshi Nishimura, Teruo Aoki, Masashi Niwano, Sumito Matoba, Tomonori Tanikawa, Tetsuhide Yamasaki, Satoru Yamaguchi, and Koji Fujita

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Revised manuscript accepted for ESSD
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Cited articles

Aoki, T., Aoki, T., Fukabori, M., and Uchiyama, A.: Numerical simulation of the atmospheric effects on snow albedo with a multiple scattering radiative transfer model for the atmosphere-snow system, J. Meteorol. Soc. Jpn., 77, 595–614, https://doi.org/10.2151/jmsj1965.77.2_595, 1999. 
Aoki, T., Hachikubo, A., and Hori, M.: Effect of snow physical parameters on shortwave broadband albedos, J. Geophys. Res., 108, 4616, https://doi.org/10.1029/2003jd003506, 2003. 
Aoki, T., Kuchiki, K., Niwano, M., Kodama, Y., Hosaka, M., and Tanaka, T.: Physically based snow albedo model for calculating broadband albedos and the solar heating profile in snowpack for general circulation models, J. Geophys. Res.-Atmos., 116, 1–22, https://doi.org/10.1029/2010JD015507, 2011. 
Aoki, T., Matoba, S., Uetake, J., Takeuchi, N., and Motoyama, H.: Field activities of the “Snow Impurity and Glacial Microbe effects on abrupt warming in the Arctic” (SIGMA) Project in Greenland in 2011–2013, Bull. Glaciol. Res., 32, 3–20, https://doi.org/10.5331/bgr.32.3, 2014. 
Armstrong, R. L. and Brun, E. (Eds.): Physical processes within the snow cover and their parameterization, in: Snow and Climate: Physical Processes, Surface Energy Exchange and Modeling, Cambridge University Press, Cambridge, N. Y., p. 58, ISBN 9780521130653, 2008. 
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We presented the method of data quality checks and the dataset for two ground weather observations in northwest Greenland. We found that the warm and clear weather conditions in the 2015, 2019, and 2020 summers caused the snowmelt and the decline in surface reflectance of solar radiation at a low-elevated site (SIGMA-B; 944 m), but those were not seen at the high-elevated site (SIGMA-A; 1490 m). We hope that our data management method and findings will help climate scientists.
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