Blog Archives
- January 2012
- October 2011
- September 2011
- July 2011
- June 2011
- May 2011
- April 2011
- March 2011
- February 2011
- November 2010
- October 2010
- September 2010
- August 2010
- July 2010
- June 2010
- April 2010
- February 2010
- October 2009
- September 2009
- August 2009
- July 2009
- June 2009
- May 2009
- April 2009
- March 2009
- February 2009
- January 2009
- December 2008
- November 2008
- October 2008
- September 2008
- August 2008
- July 2008
- June 2008
- May 2008
- April 2008
- March 2008
- February 2008
- January 2008
- December 2007
- November 2007
- October 2007
- September 2007
- August 2007
- July 2007
- May 2007
- April 2007
- March 2007
- February 2007
- December 2006
- November 2006
- October 2006
- August 2006
- July 2006
- June 2006
Blogroll
- Ags in AK The Adventures of Andy and Lisa Brown
- CIMSS Satellite Blog A weblog of meteorological satellite imagery relevant to current weather events
- Discovery Channel’s Storm Chasers Follow the storm chasers of the popular TV show
- High Plains Drifter Under the Meso Blogs
- Stormeyes: Convectives Storms Observed this Year by the Edwards
- This Week in Photography This Week in Photography – A blog about photography with podcasts
- Warren Faidley’s Storm Chasing Blog America’s first, full-time professional storm chaser
Meta
Monthly Archives: February 2007
Clines Corners, NM drifting snow
These are a few pictures taken from Clines Corners, NM (about 60 miles east of Albuquerque on I-40). Clines Corners sits along a gentle sloping ridge just below 7,100 feet in elevation. The area frequently observes gusty winds due to topographical forcing and when you add copious amounts of snow, it can easily reach near “white-out” conditions due to blowing and drifting snow.
The Albuquerque National Weather Service office maintains an Automated Surface Observing Site (ASOS) in Clines Corners and unfortunately the precipitation data for the past 30+ days has been erroneous and unusable. 
The actual rain gauge includes an 8″ diameter cylindrical bucket with the rim of the bucket at a height of about 5 feet above the ground. Surrounding the bucket is a perimeter of metal flaps that act to shield the falling rain drops from the wind in order to maximize the rain measurement. The bucket has heaters in the bottom that melt snow and thus measure a water equivalent of snowfall.
With 5ft. of drifted snow on top of the gauge, the heaters were continuously melting the snow allowing a continuous stream of water to be measured while the winds kept drifting the snow back on top of the gauge. In other words, the heaters could not keep up with this newly blown snow covering the gauge. The data was contaminated and we were seeing erroneous readings of 20+ inches of precipitation due to this process. Needless to say, our technicians had to physically dig out the gauge to prevent this from happening.
Temperature readings were also reading several degrees cooler than they should have been. The nearby temperature sensor was also feeling the effects of the snowpack.


Posted in Uncategorized
Comments Off



