NEWS:

January 30, 2008: This site is running the code developed by Tad Hurst.

Why not submit your favorite site? I need site name, lat, long, LZ and launch altitudes and the zipcode.

- Alan

Also check out the Santa Barbara Regional Atmospheric Soaring Prediction BLIPMAP Forecast - produced by Don Taber

Sounding

Station:

KVBG (alt)

Date/Time:

3 SEP 2010

Temp/Wind data from:

NOAA Digital Forecast
Fri Sat Sun Mon Tue Wed
Site
Name
Wind Above
Launch
Wind Above
Launch
Wind Above
Launch
Wind Above
Launch
Wind Above
Launch
Wind Above
Launch
Bates Beach W 9 0 W 9 278 W 9 0 SW 8 0 SW 7 278 SW 9 278
Pine Mountain S 8 7542 SW 8 7542 NW 8 8006 N 10 5835 W 3 4567 W 6 2853
Eliminator Skyport W 7 1077 W 8 1077 NW 15 1077 N 7 0 W 5 0 W 8 0
Ojai S 13 6984 N 13 6984 N 8 7604 N 7 5435 SW 5 2692 SW 7 0
Dunlap W 8 6815 W 8 7129 W 9 4448 SW 7 945 SW 9 63 SW 8 0
Calabasas SW 12 9293 SW 12 9598 SW 12 3030 S 7 1307 S 12 674 SW 8 368
Saddle Peak S 14 6317 S 15 6317 S 15 261 S 6 0 S 13 0 SW 7 0
Garlock S 8 8022 SW 16 8706 W 28 6796 NE 9 5167 SW 22 3201 W 24 0
Blackhawk NE 9 7934 W 13 8402 SW 20 6348 SW 12 5081 SW 16 4430 SW 18 923
Slick Rock SW 10 6211 SW 10 6525 NW 12 3759 SW 7 1189 W 12 0 W 12 0
Horseshoe SE 12 9767 W 12 11932 W 15 9244 N 7 4612 S 9 3812 SW 12 178
Malibu - Castro Peak S 14 6943 S 15 6943 S 15 383 S 6 0 S 13 0 W 7 0

DISCLAIMER: These estimates are intended to assist in daily site selection only.  No warranty is made concerning the accuracy of these estimates.  These estimates cannot be used to determine if conditions are safe for flying.  Conditions should be evaluated at the launch site by experienced pilots before launching.

Sounding: This is the site at which the weather balloon was released.  If the flying site predicted is far from the sounding site, the estimate is not valid.  Also, the sounding is done at 12Z (4AM PST).  If a front comes through, the sounding is no longer valid. The sounding becomes less valid later in the day.

Thermal Ceiling: the lower of the height at which the thermal stops rising and the cloud level.  We can't fly into the clouds, so it doesn't matter how much higher the thermal goes.  Remember that we can't get to the top of the thermal because of our sink rate.  Our upper limit will be lower than the reported ceiling.

Soaring Ceiling: We will stop going up when the thermal is rising just fast enough to offset our sink.  It is estimated that this happens when the temperature difference between the thermal and the surrounding air is about 2 degrees F. This number is an estimate of the maximum altitude we might reach if we start at launch height, and should be more reflective of our chances of soaring than the thermal top. Please let me know how this compares with actually flying, and I will adjust it as necessary.

Above Launch: The difference between how high we might get and how high we start. This estimate does not account for ridge lift.

High Temp: This estimate is taken from the National Weather Service website.  Puddle temperatures can exceed this temperature. 

Puddle Temp: This estimate is based on the High Temp and the National Weather Service estimate of cloudiness, and the angle of the sun.  When the sun is directly overhead on a sunny day, the puddle temp is esimated to be 25 degrees warmer than the high ambient temperature. This estimate now includes a rigorous calculation of the Sun Angle, and accounts for the seasonal differences in zenith and daylight hours.

Wind: This estimate is taken from the National Weather Service website.

Thermal Type: Blue (no cloud formation) or White (Cloud formation)

Thermal Index: This is the maximum difference in temperature between the rising packet of air (the thermal) and the surrounding air.  The difference in temperature is responsible for the buoyancy of the thermal, and larger temperature differences mean faster rising thermals.  A value of about 10 F or greater often means that the conditions are soarable.  Values above 20 could indicate rowdy thermals.

Validity of estimate: Many factors (including strong wind, fronts, cloud shadows, incorrectly predicted temperatures, etc) can affect the validity of the estimates. 

Author: Tad Hurst

Supported By: Alan Crouse ac_soaring@yahoo.com