Articles | Volume 18, issue 7
https://doi.org/10.5194/acp-18-4715-2018
https://doi.org/10.5194/acp-18-4715-2018
Research article
 | 
09 Apr 2018
Research article |  | 09 Apr 2018

Precipitation regimes over central Greenland inferred from 5 years of ICECAPS observations

Claire Pettersen, Ralf Bennartz, Aronne J. Merrelli, Matthew D. Shupe, David D. Turner, and Von P. Walden

Data sets

Microwave radiometer snow categorization tool for Summit, Greenland, 2010–2015 C. Pettersen and A. Merrelli https://doi.org/10.18739/A2R28Q

Microwave Radiometer measurements of sky brightness temperature taken at Summit Station, Greenland, 2010 D. Turner and R. Bennartz https://doi.org/10.18739/A2R79T

Microwave Radiometer measurements of sky brightness temperature taken at Summit Station, Greenland, 2011 D. Turner and R. Bennartz https://doi.org/10.18739/A27795

Microwave Radiometer measurements of sky brightness temperature taken at Summit Station, Greenland, 2012 D. Turner and R. Bennartz https://doi.org/10.18739/A2ZR3K

Microwave Radiometer measurements of sky brightness temperature taken at Summit Station, Greenland, 2013 D. Turner and R. Bennartz https://doi.org/10.18739/A22J6K

Microwave Radiometer measurements of sky brightness temperature taken at Summit Station, Greenland, 2014 D. Turner and R. Bennartz https://doi.org/10.18739/A2HJ57

Microwave Radiometer measurements of sky brightness temperature taken at Summit Station, Greenland, 2015 D. Turner and R. Bennartz https://doi.org/10.18739/A24B8W

Millimeter Cloud Radar measurements taken at Summit Station, Greenland, 2010 M. Shupe https://doi.org/10.18739/A2G74F

Millimeter Cloud Radar measurements taken at Summit Station, Greenland, 2011 M. Shupe https://doi.org/10.18739/A2M17R

Millimeter Cloud Radar measurements taken at Summit Station, Greenland, 2012 M. Shupe https://doi.org/10.18739/A2BJ3X

Millimeter Cloud Radar measurements taken at Summit Station, Greenland, 2013 M. Shupe https://doi.org/10.18739/A2318G

Millimeter Cloud Radar measurements taken at Summit Station, Greenland, 2014 M. Shupe https://doi.org/10.18739/A2121J

Precipitation Occurrence Sensor System measurements taken at Summit Station, Greenland, 2011 M. Shupe https://doi.org/10.18739/A2H20H

Precipitation Occurrence Sensor System measurements taken at Summit Station, Greenland, 2012 M. Shupe https://doi.org/10.18739/A2CB7P

Precipitation Occurrence Sensor System measurements taken at Summit Station, Greenland, 2013 M. Shupe https://doi.org/10.18739/A27J64

Occurrence Sensor System measurements taken at Summit Station, Greenland, 2015 M. Shupe https://doi.org/10.18739/A2VB8D

Radiosonde temperature and humidity profiles taken at Summit Station, Greenland, 2010 V. P. Walden and M. Shupe https://doi.org/10.18739/A2F490

Radiosonde temperature and humidity profiles taken at Summit Station, Greenland, 2011 V. P. Walden and M. Shupe https://doi.org/10.18739/A25N4S

Radiosonde temperature and humidity profiles taken at Summit Station, Greenland, 2012 V. P. Walden and M. Shupe https://doi.org/10.18739/A2X508

Radiosonde temperature and humidity profiles taken at Summit Station, Greenland, 2013 V. P. Walden and M. Shupe https://doi.org/10.18739/A2NN44

Radiosonde temperature and humidity profiles taken at Summit Station, Greenland, 2014 V. P. Walden and M. Shupe https://doi.org/10.18739/A2WZ18

Radiosonde temperature and humidity profiles taken at Summit Station, Greenland, 2015 V. P. Walden and M. Shupe https://doi.org/10.18739/A2GZ1J

Precipitation Occurrence Sensor System measurements taken at Summit Station, Greenland, 2014 M. Shupe https://doi.org/10.18739/A2020V

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Short summary
A novel method for classifying Arctic precipitation using ground based remote sensors is presented. The classification reveals two distinct, primary regimes of precipitation over the central Greenland Ice Sheet: snowfall coupled to deep, fully glaciated ice clouds or to shallow, mixed-phase clouds. The ice clouds are associated with low-pressure storm systems from the southeast, while the mixed-phase clouds slowly propagate from the southwest along a quiescent flow.
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