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Here's our latest thinking on storm timing Saturday evening into early Sunday AM. A few storms may occur to the west and northwest of the DFW Metroplex in the evening hours. These storms may be severe with a tornado and hail risk, but the primary hazard will be damaging winds. Thereafter, they will likely grow upscale into a line of storms, resulting in mostly a damaging wind threat. There will be an enhanced threat for brief spin-up tornadoes within the line, as well as with any storms that MAY develop ahead of the line. For midnight and beyond, most activity should be in the form of a squall line promoting a continued risk for damaging winds. Brief spin up tornadoes cannot be out as well as a threat for hail.
A Severe Thunderstorm Watch has been issued for portions of North- Central Texas, in effect until 2:00 AM CDT Sunday. A Severe Thunderstorm Watch is issued when conditions are favorable for severe thunderstorms. This watch includes the Dallas/Fort Worth Metroplex. The main threats tonight will be damaging wind gusts in excess of 60 MPH and hail larger than one inch in diameter. A few isolated tornadoes will also be possible, especially near the Red River. Stay tuned to NOAA Weather Radio and/or media outlets for additional information and possible warnings.
Chances of showers and thunderstorms will continue through mid morning southeast of a Sulphur Springs to Temple line, followed by decreasing cloudiness. Elsewhere, skies will be mostly sunny. It will be breezy and cooler with highs will be in the 70s. Winds will be northerly at 10 to 20 mph. Gusts over 25 mph are likely through midday.
Low chances of showers and thunderstorms will return Friday east of a Bonham to Hearne line. Otherwise, we will have dry weather next week. Gusty north to northwest winds and drier air behind a cold front Tuesday will result in elevated fire weather concerns.
Here is some information on Wireless Emergency Alerts (WEA). Take time to review this information as we prepare for severe weather across the region!

 
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It's the Heat AND Humidity

It has been said that "It's not the heat, it's the humidity". Well, actually it's both. Our bodies dissipate heat by varying the rate and depth of blood circulation, by losing water through the skin and sweat glands, and, as the last extremity is reached, by panting. As the body heats up, the heart begins to pump more blood, blood vessels dilate to accommodate the increased flow, and the tiny capillaries in the upper layers of skin are put into operation.

The body's blood is circulated closer to the skin's surface, and excess heat drains off into the cooler atmosphere by one or a combination of three ways...
  • radiation,
  • convection, and
  • evaporation.
At lower temperatures, radiation and convection are efficient methods of removing heat. However, once the air temperature reaches 95°F, heat loss by radiation and convection ceases. It is at this point that heat loss by sweating becomes all-important. But sweating, by itself, does nothing to cool the body, unless the water is removed by evaporation (sweat changing to water vapor). The downside of this method of cooling is that high relative humidity retards evaporation.

Relative humidity is a measure of the amount of water vapor contained in the air, divided by the maximum amount the air can hold, expressed as a percent. A relative humidity of 50% means the air contains ½ of the water vapor it can actually hold. The maximum amount of water vapor the air can hold is dependent upon the temperature (the "relative" in relative humidity). The higher the temperature, the more water (actually water vapor) the air can hold. For example, air with a temperature of 32°F can hold about 0.16 ounces of water. Air with a temperature of 80°F can hold about an ounce of water.

So, what does this all mean? Sweat is evaporated (changes from a liquid to a gas, i.e. water vapor) when heat is added. The heat is supplied by your body. The results are summed up in the table below...

Relative
Humidity
Capacity for air
to hold water
Amount of
Evaporation
HEAT removed
from the body
LOW LARGER HIGHER MORE
HIGH SMALLER LOWER LESS

If the condition where the lack of heat removed from the body is prolonged, the results can be very serious and even fatal.

DID YOU KNOW...
  • In a normal year, approximately 175 Americans die from extreme heat. Young children, elderly people, and those who are sick or overweight are more likely to become victims.
  • Between 1936 and 1975, nearly 20,000 people succumbed to the effects of heat and solar radiation.
  • Because men sweat more than women, men are more susceptible to heat illness because they become more quickly dehydrated.
Knowing how the body deals with excessive heat is critical in understanding the dangers to you and proper steps to take to prevent becoming a victim of excessive heat.
  NEXT: The Heat Index
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