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The Canadian CloudSat/CALIPSO Validation Project (C3VP)
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Daily Summary for 7 November 2006


 

Quick links:

Weather SummaryFlight SummarySatellite ImagesSurface ObservationsModel AnalysesRadiosonde Soundings

 

Weather Summary

With a split flow scenario, the major weather systems in play over eastern North America were a deep low over the northernmost tip of Quebec and a weaker system over the Southeast US. The storm over the Southeast advanced northward during the day, providing precipitation for CARE and southwestern Ontario. Nearer to Ottawa and the CloudSat overpass, conditions were mixed. The system over Northern Quebec provided mid-level clouds, while the system to the south brought in clouds at multiple layers: cirrus, altostratus, and nimbostratus.

Pictures taken during the flight by Adam Kankiewicz:

 

Flight Summary

Today's C3VP flight turned out to be a mixed bag of clouds. We went north out of Ottawa and initially found a great looking mixed phase deck of clouds. After heading north along the CloudSat track and swinging back around to the south the deck of mid-level clouds started dissipating rapidly. By CloudSat overpass time (~13:30 LT) only a few scattered clouds at different layers were left. We had a thick layer of partially visible cirrus present over us the entire time. After C3VP ops were finished, we headed east out of the C3VP target region looking for some better mixed-phase clouds (as observed on the uploaded satellite images!). After heading east for about 25 minutes we found the best looking clouds around and were able to run a porpoising leg through the top followed by a spiral sounding through the cloud. Cloud top had peak lwc of ~0.15 g/m3. This cloud (like all the other clouds we observed today) dissipated right before our eyes. We then decided to call it a day and head home. We used about 1.5 hrs of flight time. It was a very frustrating midlevel cloud case.

Lessons learned:

This was the first time we have tried anything outside the C3VP ops region and we had excellent cooperation from Montreal ATC. Vertical blocks and sounding requests were quickly approved. The scattered nature of the clouds prevented any meaningful Lagrangian sampling attempts. If CLEX cloud conditions look favorable, we need to try to arrive early on a C3VP track to take advantage of the clouds before they disappear. Kevin's lidar proved to be very useful for identifying targetable liquid cloud layers.

Below is a MODIS IR image and CloudSat swath during the C3VP/CLEX flight.

Preliminary backscatter vs. time from the upward and downward looking airborne lidars at 1024 nm (top) and 532 nm. Images courtesy Kevin Strawbridge.



 

Satellite Images

Images are every 4 hours beginning at 0045 UTC.

GOES-12 IR courtesy of RAP @ UCAR

 

GOES-12 Visible (during daylight hours) and Near IR (night) albedo from CIRA.

 

GOES-12 IR (10.7 µm) brightness temperature from CIRA. The color scale begins at 0 °C with an increment of -10 °C between color changes.

 

GOES-12 experimental cloud phase from CIRA. Blue represents ice particles, red is liquid droplets above freezing and yellow represents supercooled liquid droplets. Gray areas are clear (no cloud) based on an IR cloud mask.

 

Surface Observations

20 UTC RUC surface analysis from RAP @ UCAR

Surface METARs every 4 hours beginning at 00 UTC courtesy RAP @ UCAR

 

Model Analyses

12 UTC Eta analysis of 500 mb heights and vorticity

 

Radiosonde Soundings

12 UTC Maniwaki, QC