#MEwx Darn cold, sun and thge difference between Sleet and Freezing rain

Good morning Augusta

A direct, real-time feed from my personal weather station is available for you here.

It’s darn cold and slippery out there so SLOW DOWN on your way to work.

Today it’s going to be mostly cloudy with highs in the lower 30s. Light and variable winds.

Tonight we’ll have mostly cloudy skies, Not as cold with lows in the mid 20s. Light and variable winds.

The readings from my weather instruments are:

Our outdoor temperature is 9.1°F, the humidity is 69% and the Dew Point is 1.0°F.

The wind direction is Northwest between 0.1 MPH and 0.3 MPH with a wind chill of 9.1°F.  

The Relative pressure is 30.42, the Absolute pressure is 20.22 and steady with a weather graphic indicating sun/snow.

Visibility is 10.0 Miles / 16.1 Kilometers with clear skies.

The UV rating is 1 out of 16, Sunrise is 6:33 AM Sunset is 4:13 PM, Moonrise is 5:52 PM, moonset is 8:23

AM and the moon phase is Waning gibbous. 

The RAW METAR readings from Augusta’s airport are:

METAR KAUG 141053Z AUTO 00000KT 8SM CLR M12/M14 A3046 RMK AO2 SLP324 T11221139

We didn’t receive any snow or rain here over the past 24 hours.

Do you know what the difference is between Freezing Rain and Sleet?

Both freezing rain and sleet occur by the same general process: liquid raindrops in a layer of warm air well above the surface fall into a layer of freezing

air hugging the ground.  The difference between these two wintry precipitation types depends on the thickness of the layer of freezing air.

 

Freezing rain occurs when the layer of freezing air is so thin that the raindrops do not have enough time to freeze before reaching the ground.  Instead,

the water freezes on contact with the surface, creating a coating of ice on whatever the raindrops contact.

 

Sleet is simply frozen raindrops and occurs when the layer of freezing air along the surface is thicker.  This causes the raindrops to freeze before reaching

the ground. 

 

Why are Freezing Rain and Sleet Dangerous?

Both of these wintry precipitation types are hazardous for travelers.  With either type, the ice can create slick spots on roadways, causing motorists

to lose control of their automobiles with little to no warning.  Bridges, overpasses and elevated roadways are especially suseptible to icing as they are

surrounded on all sides by the cold air and freeze more quickly. 

In addition, ice caused by freezing rain can rapidly add weight to tree branches and power lines, causing them to snap or break.  In addition to these

fallen branches causing damage to whatever they land on, power outages may also occur.

 

How is Icing Caused by Freezing Rain Measured?

Ice accumulation from freezing rain does not coat the surface of objects evenly.  Gravity will usually cause the rain water to run to the underside of

an object before it freezes.  Wind can create the same effect.  In either case, the result would be a thicker coating of ice on one side of the object

compared to the opposite side.

You can accurately estimate the thickness of the ice with the method below.  You will need a ruler and possibly a piece of paper and pencil.

1. Locate an ice-covered object that is out in the open.  A small tree branch in the middle of the yard or clothesline is usually easiest to handle.

2. Move to a position where you can see both the thickest and thinnest portions of ice coating the object from one side to the other.

3. Using the ruler, measure the thickest part of the ice, from the edge of the object to the edge of the ice. Record that value on your paper.

4. Similarly, measure the thinest part of the ice, from the edge of the object to the edge of the ice. Record that value on your paper.

5. Add the two values together and then divide by two.  The resulting value is your ice accumulation. 

 

How is Sleet Measured?

Sleet is measured much the same way snow depth is measured. You will need a ruler, and possibly a piece of paper and a pen.

1. Locate a surface that is solid, level and in the open.  Avoid measuring sleet depth under trees or directly next to buildings.

2. Slide the ruler directly downward into the sleet until it reaches the ground.

3. Read the value on the ruler to the nearest tenth of an inch, if possible.

4. Record this value on your piece of paper.