Articles | Volume 16, issue 7
Atmos. Chem. Phys., 16, 4743–4756, 2016
Atmos. Chem. Phys., 16, 4743–4756, 2016
Research article
15 Apr 2016
Research article | 15 Apr 2016

Microwave signatures of ice hydrometeors from ground-based observations above Summit, Greenland

Claire Pettersen et al.

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Cited articles

Ackerman, T. P. and Stokes, G. M.: The Atmospheric Radiation Measurement Program, Phys. Today, 55, 39–44, 2003.
Bennartz, R. and Bauer, P.: Sensitivity of microwave radiances at 85–183 GHz to precipitating ice particles, Radio Sci., 38, 8075,, 2003.
Castellani, B. B., Shupe, M. D., Hudak, D. R., and Sheppard, B. E.: The annual cycle of snowfall at Summit, Greenland, J. Geophys. Res., 120, 6654–6668,, 2015.
Church, J. A.: Changes in sea level, Climate Change 2001: The Scientific Basis, Cambridge University Press, 639–693, 2001.
Clough, S. A., Shephard, M. W., Mlawer, E. J., Delamere, J. S., Iacono, M. J., Cady-Pereira, K., Boukabara, S., and Brown, P. D.: Atmospheric radiative transfer modeling: a summary of the AER codes, J. Quant. Spectrosc. Ra., 91, 33–244, 2005.
Short summary
We examined four summers of data from a ground-based atmospheric science instrument suite at Summit Station, Greenland, to isolate the signature of the ice precipitation. By using a combination of instruments with different specialities, we identified a passive microwave signature of the ice precipitation. This ice signature compares well to models using synthetic data characteristic of the site.
Final-revised paper