Your Storm Forecast Is Going to Get More Precise

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Just about every alert you hear before a storm creeps up on the horizon was issued by the National Weather Service (NWS). We use this federal agency's services almost every day without thinking about it. Daily forecasts, storm alerts, weather radars, and satellite images are all produced by thousands of meteorologists who work day and night to keep us safe. One part of keeping us safe is making sure we understand what they're trying to tell us. After all, what good is a warning if you don't know exactly what they're trying to say? The NWS is working to simplify the warning process to give us better information and help us make better decisions to stay safe during hazardous weather.

Right now, the NWS issues dozens of different alerts that cover all sorts of dangerous conditions. These alerts are called watches, advisories, and warnings, with each respective category carrying a greater sense of urgency. There are alerts for tornadoes, severe thunderstorms, floods, hurricanes, winter storms, and even conditions like dense fog or blowing dust.

The sheer number of alerts can be daunting, not to mention the sometimes-convoluted language forecasters use to tell us what's going on. It's easy to miss the distinction between a tornado watch and a tornado warning, for example. The Hazards Simplification Project is an ongoing effort within the National Weather Service to whittle down the number of alerts and use clearer language to give us a leg-up on dangerous weather conditions.

The first couple of changes will go into effect later in 2017. The NWS currently issues 10 different alerts for winter weather events such as blizzards, ice storms, lake effect snow, and snowstorms. In the winter, the agency will reduce the number of alerts to just six. They're getting rid of the blizzard watch, for example, merging it with the winter storm watch. Winter weather alerts will also be issued in a “what/where/when” format, outlining exactly how much snow or ice you can expect, where it's expected, and when it's expected to happen. Previously, you had to scour a few paragraphs of text to figure out what was coming your way.

The NWS will also look into changing their weather maps to display just four different colors when weather alerts are in effect—a dramatic change from the hodgepodge of colors that smear weather maps today. Each weather alert currently has its own unique color on weather maps, so these maps are almost indecipherable when there's a lot of active weather across the country. The agency may soon replace all of these colors with just four hues—yellow, orange, red, and purple—to convey the severity and urgency of the alert in effect.

improved hazardous weather map from the NOAA
A swath showing the probability of a tornado near Birmingham, Alabama, under the new FACETs project. The old tornado warning polygon is outlined in red.
NOAA/NSSL

There are also some big changes in the works for warnings in the future. Meteorologists used to issue tornado and severe thunderstorm warnings for entire counties, which didn't work out too well as some counties in the United States are enormous compared to the size of a single thunderstorm. About a decade ago, they reduced these warnings to polygons that covered just the area expected to be impacted by the storm. This greatly reduced false alarms and helped warn only the people who needed to take shelter.

In the next couple of years, the NWS will roll out a project called Forecasting a Continuum of Environmental Threats (FACETs). This project will reduce those old warning polygons even further into a swath that shows the probability that a certain area will be affected by a tornado, large hail, or damaging winds. The resulting warning area, seen above, looks similar to the cone of uncertainty forecasters use ahead of hurricanes and covers a much smaller area than the old polygons. This will allow forecasters to warn only those directly affected by the approaching hazards, reducing false-alarm rates even further and giving people greater confidence that they should take action right away instead of waiting it out.

Why Does Humidity Make Us Feel Hotter?

Tomwang112/iStock via Getty Images
Tomwang112/iStock via Getty Images

With temperatures spiking around the country, we thought it might be a good time to answer some questions about the heat index—and why humidity makes us feel hotter.

Why does humidity make us feel hotter?

To answer that question, we need to talk about getting sweaty.

As you probably remember from your high school biology class, one of the ways our bodies cool themselves is by sweating. The sweat then evaporates from our skin, and it carries heat away from the body as it leaves.

Humidity throws a wrench in that system of evaporative cooling, though. As relative humidity increases, the evaporation of sweat from our skin slows down. Instead, the sweat just drips off of us, which leaves us with all of the stinkiness and none of the cooling effect. Thus, when the humidity spikes, our bodies effectively lose a key tool that could normally be used to cool us down.

What's relative about relative humidity?

We all know that humidity refers to the amount of water contained in the air. However, as the air’s temperature changes, so does the amount of water the air can hold. (Air can hold more water vapor as the temperature heats up.) Relative humidity compares the actual humidity to the maximum amount of water vapor the air can hold at any given temperature.

Whose idea was the heat index?

While the notion of humidity making days feel warmer is painfully apparent to anyone who has ever been outside on a soupy day, our current system owes a big debt to Robert G. Steadman, an academic textile researcher. In a 1979 research paper called, “An Assessment of Sultriness, Parts I and II,” Steadman laid out the basic factors that would affect how hot a person felt under a given set of conditions, and meteorologists soon used his work to derive a simplified formula for calculating heat index.

The formula is long and cumbersome, but luckily it can be transformed into easy-to-read charts. Today your local meteorologist just needs to know the air temperature and the relative humidity, and the chart will tell him or her the rest.

Is the heat index calculation the same for everyone?

Not quite, but it’s close. Steadman’s original research was founded on the idea of a “typical” person who was outdoors under a very precise set of conditions. Specifically, Steadman’s everyman was 5’7” tall, weighed 147 pounds, wore long pants and a short-sleeved shirt, and was walking at just over three miles per hour into a slight breeze in the shade. Any deviations from these conditions will affect how the heat/humidity combo feels to a certain person.

What difference does being in the shade make?

Quite a big one. All of the National Weather Service’s charts for calculating the heat index make the reasonable assumption that folks will look for shade when it’s oppressively hot and muggy out. Direct sunlight can add up to 15 degrees to the calculated heat index.

How does wind affect how dangerous the heat is?

Normally, when we think of wind on a hot day, we think of a nice, cooling breeze. That’s the normal state of affairs, but when the weather is really, really hot—think high-90s hot—a dry wind actually heats us up. When it’s that hot out, wind actually draws sweat away from our bodies before it can evaporate to help cool us down. Thanks to this effect, what might have been a cool breeze acts more like a convection oven.

When should I start worrying about high heat index readings?

The National Weather Service has a handy four-tiered system to tell you how dire the heat situation is. At the most severe level, when the heat index is over 130, that's classified as "Extreme Danger" and the risk of heat stroke is highly likely with continued exposure. Things get less scary as you move down the ladder, but even on "Danger" days, when the heat index ranges from 105 to 130, you probably don’t want to be outside. According to the service, that’s when prolonged exposure and/or physical activity make sunstroke, heat cramps, and heat exhaustion likely, while heat stroke is possible.

Have you got a Big Question you'd like us to answer? If so, let us know by emailing us at bigquestions@mentalfloss.com.

This article has been updated for 2019.

Is the Heat Index Real?

MarianVejcik/iStock via Getty Images
MarianVejcik/iStock via Getty Images

Complaining about the humidity is a mainstay of small talk. “It’s not the heat that gets you, it’s the humidity” is a common refrain around the South, just as “it’s a dry heat” is a go-to line in the desert Southwest. The clichés aren’t wrong on this one—a hot and humid day can have a dramatic effect on both your comfort and your health. We can measure this very real impact on your body using the heat index. 

The heat index is the temperature it feels like to your body when you factor in both the actual air temperature and the amount of moisture in the air. If the heat index is 103°F, that means that the combination of heat and humidity has a similar physical impact on your body as it would if the actual air temperature were 103°F. Even though it’s tempting to think of the heat index as an exaggerated temperature that only exists to make the heat sound worse than it really is, scientists came up with the measurements after decades of medical and meteorological research devoted to studying the impact of heat and humidity on the human body. It’s the real deal.

The dew point is an important component of the heat index. The dew point is the temperature at which the air would reach 100 percent relative humidity, or become fully saturated with moisture like on a foggy morning. Since cooler air can’t hold as much moisture as warmer air, lower dew points reflect lower moisture levels and higher dew points indicate higher moisture levels. Dew points below 60°F are comfortable, while readings reaching 70°F and even 80°F range from muggy to downright oppressive.

Measuring humidity on a hot day is important because moisture is how your body naturally cools itself off. Your sweat cools the surface of your skin through a process known as evaporative cooling. If the air is packed with moisture, it takes longer for your sweat to evaporate than it would in more normal conditions, preventing you from cooling off efficiently. The inability to lower your body temperature when it’s hot can quickly lead to medical emergencies like heat exhaustion or heat stroke, which is why the heat index is such an important measurement to pay attention to during the summer months.

The heat index is generally considered “dangerous” once the value climbs above 105°F, and your risk of falling ill increases the higher the heat index climbs.

Dry climates can have the opposite effect on your body, with the distinct lack of moisture in the air making it feel cooler to your body than it really is. Summers get oppressively hot in places like Arizona and Iraq, but the heat doesn’t affect residents as severely because the air is extremely dry. Dew points in desert regions can hover at or below 32°F even when the air temperature is well above 100°F, which is about as dry as it can get in the natural world.  

In 2016, a city in Kuwait measured the all-time highest confirmed temperature ever recorded in the eastern hemisphere, where temperatures climbed to a sweltering 129°F during the day on July 21, 2016. The dew point there at the same time was nearly 100 degrees cooler, leading to a heat index of just 110°F, much lower than the actual air temperature. That’s not necessarily a good thing. Extreme heat combined with extreme aridity can make your sweat evaporate too efficiently, quickly dehydrating you and potentially leading to medical emergencies similar to those you would experience in a much more humid region of the world. 

Have you got a Big Question you'd like us to answer? If so, let us know by emailing us at bigquestions@mentalfloss.com.

This story has been updated for 2019.

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