National Weather Service United States Department of Commerce

Powerful Pacific System Impacting the West; First Significant Snow for Portions of the East

Power Pacific system will continue to bring significant impacts for Pacific Northwest into northern California the remainder of the week. Dangerous coastal affects, heavy rain, flooding, strong winds, and higher elevation mountain snow continues. Meanwhile, a storm across the east is set to bring the first accumulating snow to many higher elevations of the Catskills into the central Appalachians. Read More >

 

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Ceiling and Visibility

 Ceilings are a common problem when precipitation occurs.  In the Southeast US, they tend to be a greater hazard during the wintertime, when temperatures are colder and freezing levels are much lower than during the summer.

 

 

 

Many aircraft and pilots are rated for various ceiling minimums and thus use their rating and experience to determine whether or not it is safe to fly.  In general, ceiling heights and resulting safety fall into four different categories:

 

Ceiling Height (AGL) Flight Category
> 3000ft Visual Flight Rules (VFR)
1000ft-3000ft Marginal Visual Flight Rules (MVFR)
500ft-900ft Instrument Flight Rules (IFR)
<500ft Low Instrument Flight Rules (LIFR)

 


Low visibilities can occur due to fog, falling snow, heavy smoke, or even haze.  Similar to the ceiling categories above, visibility conditions fall into four aviation flight rule categories:

 

Visibility

Flight Category
> 5SM Visual Flight Rules (VFR)
3-5SM Marginal Visual Flight Rules (MVFR)
1-3SM Instrument Flight Rules (IFR)
< 1SM Low Instrument Flight Rules (LIFR)

 

There are two types of fog that can form:  Radiation Fog and Advection Fog

Radiation Fog  Two ingredients are needed for radiation fog to develop:  Very light or calm winds, and a relative humidity of 100%.  On a weather map, 100% RH is also indicated when the air temperature is the same as the dewpoint temperature.  When this occurs, moisture condenses into tiny droplets, essentially forming a cloud right at the ground level.  In pure ground fog environments, it is not uncommon for the fog to be very shallow with low forward visibility and clear skies above.  Most of the time, this type of fog forms overnight, then dissipates the following morning after a couple hours of sunshine.

 

Advection Fog  This type tends to develop when moist air moves into an area (usually from a body of water such as the ocean, lake or river).  Unlike radiation fog, the winds can continually replenish the moisture so that even sunshine cannot improve the conditions.  It is not uncommon for this type of fog to persist for most of the day, and is usually accompanied by stratus clouds and low ceilings.

 

 

 

 Click the image for a current map of ceiling and visibility conditions across the ZME airspace.

 

 

To avoid landing in bad weather conditions, look at the current and forecasted weather conditions for the destination before departing.  While in flight, listen for hazardous weather information that indicate poor conditions.  AIRMETs are issued for widespread IFR conditions, and Center Weather Advisories (CWA) are generally issued for LIFR conditions.

For a current display of AIRMETs in effect, click here. To view only the IFR products, check the Ceil&Vis box and uncheck all others.

 

For a current display of CWAs in effect, click here.

 

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Ceiling and Visibility

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Density Altitude