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Blanchard: If the prevailing wind is more North than 212° (SSW), launch and LZ likely NW (see a map).   For South wind, terrain often adds some SE at launch. This page has parts updated at varying intervals. The parts refresh only when the page reloads. The page reloads automatically every 10 minutes. Last reload  .    Use the refresh button to force a refresh.
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Current RUC2 Soundings   |   




Click for Burlington Airport, Washington Forecast Current RUC Sounding

Bellingham Cold Storage camera may not always point South!
When it does, Blanchard Mt is about 6mi SSE of the peak on the left.
Blanchard launch is   ↓  above and just to the left of the church steeple.  ↓
Source Cam → Baker,Blanchard from Anacortes. | Cam location. | clear air shot | snow shows launch

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Low elevation sounding analysis for 48.74N, 122.38W Near Lake Whatcom
♦Reverse Rows

 is the lapse rate from the lowest to highest elevations listed.
 Point to point lapse rates are listed in the table.
Use the calculator below to determine lapse rates for other altitude ranges.
For the full RUC2 Sounding and Chart Click here

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The atmosphere is
Absolutely Unstable
The atmosphere is
Conditionally Unstable
The Atmosphere is
Absolutely Stable
The Atmosphere
is Inverted
When the lapse is more negative than
the near constant dry adiabatic lapse rate
-9.8 C°/km.
that is
-3 C°/1000ft)
or
-5.5 F°/1000ft
When the lapse rate is between
-4 C°/km   and   -9.8 C/km
that is
-1.2 C°/1000ft   and   -3 C°/1000ft
or
-2.16 F°/1000ft   and   -5.5 F°/1000ft
When the lapse rate
is smaller negative than
-4 C°/km
that is
-1.2 C°/1000ft
or
-2.16 F°/1000ft
When the lapse rate
is positive, that is
when the higher level
air is warmer than the
lower air.
 Overall stability will depend on moisture content.   More moisture → less cooling as the air rises → increasing instability.
To think about thermal soaring, remember that the higher the lapse rate the smaller the heating or mechanical trigger required to get air to start rising. Once rising, it will rise until it reaches the level where the temperature has dropped to the dew point and clouds form. Layers of air where the lapse rate becomes stable are called caps. It is possible for strong thermals to "break through" a cap and soaring can continue to much higher altitudes. There is often considerable turbulence associated with breaking through a cap. see JEFF HABY Thermodynamics Q&A
See also the skew-t soundings and text data with indicies at Unisys.
These are for KUIL Quiallute where they actually launch a real balloon.
TJ Olney
A fantastic glossary to help interpret the forecast discussions.

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Temps are C°  -5C° → 23F° 0C° → 32F°   5C° → 41F°   10C° → 50F°   15C° → 59F°     20C° → 68F°   25C° → 77F°   30C° → 86F°   35C° → 95F°

Meter to Feet and back converter.


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Forecast for Straight of Juan de Fuca and Admiralty Inlet.

Metars: Top of Page   |   
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Mesowest and aprs observations updated here every 10 minutes. These 4 tables are available as tiny links for your mobile device. qblan.html qtiger.html qeast.html and qebey.html

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National Weather Service forecasts.
NWS Forecast Western Whatcom County
Pre-set digital forecasts for Flying Sites
New graphical forecast tool
 
LAMP gfs based hourly forecasts updated every three hours. Localized Aviation MOS Program
25 hour Full GFS LAMP for Bellingham
25 hour Meteogram of above from LAMP
LAMP text forecast from Nested Grid Model
LAMP meteogram from Nested Grid Model
National Surface Map Fronts and Isobars
Daily National Weather Maps


Pros Calls:   Jim's Call | Tom's Call |   Airspace charts at skyvector.com



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