cloud occurrence at arctic atmospheric observatories

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Cloud Occurrence at Arctic Atmospheric Observatories Matthew Shupe, Taneil Uttal, Daniel Wolfe, David Welsh AMS Polar Meteorology and Oceanography 2007 Special Thanks for Ny’Alesund MPL Data: Masataka Shiobara, James Campbell

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Cloud Occurrence at Arctic Atmospheric Observatories. Matthew Shupe, Taneil Uttal, Daniel Wolfe, David Welsh. Special Thanks for Ny’Alesund MPL Data : Masataka Shiobara, James Campbell. AMS Polar Meteorology and Oceanography 2007. Arctic Cloud Stations. Barrow. SHEBA. Tiksi. Radar. - PowerPoint PPT Presentation

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Page 1: Cloud Occurrence at Arctic Atmospheric Observatories

Cloud Occurrence at Arctic Atmospheric Observatories

Matthew Shupe, Taneil Uttal, Daniel Wolfe, David Welsh

AMS Polar Meteorology and Oceanography 2007

Special Thanks for Ny’Alesund MPL Data:Masataka Shiobara, James Campbell

Page 2: Cloud Occurrence at Arctic Atmospheric Observatories

Arctic Cloud StationsBarrow

SHEBA

Eureka

Alert

Ny’Alesund

Tiksi

Radar Lidar

An Example Station

Summit

Page 3: Cloud Occurrence at Arctic Atmospheric Observatories

Site Instruments DatesSHEBA, Arctic Ocean Radar, lidar,

ceilometer1997-1998

Barrow, USA Radar, lidar, ceilometer

1998 – Present

Ny’Alesund, Norway Lidar 2002 – Present

Eureka, Canada Radar, lidar 2005 – Present

Alert, Canada Ceilometer ?

Tiksi, Russia None yet Not yet

Summit, Greenland None yet Not yet

Observatories

Page 4: Cloud Occurrence at Arctic Atmospheric Observatories

Data Processing Considerations

• Use a combination of cloud radar and lidar, depending on station

• “Cloud fraction” is from the perspective of vertically-pointing, surface-based instruments

• All but SHEBA must be considered preliminary in nature, more detailed multi-instrument analyses will follow

Page 5: Cloud Occurrence at Arctic Atmospheric Observatories

• Very cloudy in general at all stations (~75% total)• Summer/Fall maximum?

Total Cloud Fraction

Radar

Lidar

Surface observations

Page 6: Cloud Occurrence at Arctic Atmospheric Observatories

Vertical Distribution

Bimodal Dist’n in Vertical

Lots of Low-level Clouds

Radar

Lidar

Page 7: Cloud Occurrence at Arctic Atmospheric Observatories

Annual and Vertical Distribution

Page 8: Cloud Occurrence at Arctic Atmospheric Observatories

• Instruments: radar, lidar, microwave radiometer, radiosonde.

• Manually classified. Automated system has been developed but not yet applied to all observations at all sites.

• 1 year of data at SHEBA and 7 years at Barrow.

Cloud Type Classification

Page 9: Cloud Occurrence at Arctic Atmospheric Observatories

Annual Cycles of Cloud Type

• Mixed-phase clouds: Maxima in transition seasons.• Similar trends and magnitudes between SHEBA and Barrow

Page 10: Cloud Occurrence at Arctic Atmospheric Observatories

Liquid is present throughout the year more than half of the time!

Occurrence of Cloud Liquid

Page 11: Cloud Occurrence at Arctic Atmospheric Observatories

• Remarkable similarities• Slightly different balance at surface.

Vertical Distributions of Cloud Type

Page 12: Cloud Occurrence at Arctic Atmospheric Observatories

Annual & Vertical Dist’n of Type

Page 13: Cloud Occurrence at Arctic Atmospheric Observatories

• High annual fraction: ~75%• Remarkable similarities in vertical.• Similar dist’n of phase for W. Arctic sites. • Liquid is frequent (and important!)

• Radar-lidar combination at all sites.• Classification work at all sites using new algorithm.• More detailed analysis of boundaries

Conclusions

Future Work

Thank You.