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Weather Education

Chance of Rain? (credit: Meteorologist Ash Bray)

4/30/2018

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It’s common to hear from meteorologists, our weather apps, or even our weather-obsessed friends about the “chance of rain”. At one point in our lives, we have all scoffed, “Well, the weatherman said there was a ninety percent chance of rain today, but we didn’t see a single drop!” While ninety percent is quite high, there was a still a ten percent probability of no rain. Let’s break it down, shall we?

Meteorologists use a percentage to describe the chance of precipitation occurring at a given point. The National Weather Service defines the probability of precipitation, or PoP, as the probability of precipitation occurring at a given point. Mathematically, PoP is defined as: PoP = C * A - In this equation, “C” equals the confidence that precipitation will occur somewhere within the forecasted area, while “A” equals the percent of the forecasted area that will receive measurable precipitation, if any is to occur. For example, the NWS states, “...if the forecaster knows precipitation is sure to occur (confidence is 100%), he/she is expressing how much of the area will receive measurable rain. (PoP  = “C” * “A”, or “1” times “.4” which equals .4 or 40%). Most of the time however, the forecaster is expressing a combination of degree of confidence and areal coverage. If the forecaster is only 50% sure that precipitation will occur, and expects that, if it does occur, it will produce a measurable rain over about 80% of the area, the PoP is 40%. (PoP = .5 x .8 = .4 or 40%).”

Predicting the chance of precipitation is difficult enough when we consider said chances at a given time, but what about the chance of precipitation on a given day? This can often become confusing, mostly because when we hear “high percent chance of rain”, we tend to perceive that as meaning it could rain all day long. While that could be true if dealing with widespread rain, this logic is flawed when dealing with pop-up storms and/or a thin band of storms in which it only rains for an hour or two, but a large area receives rain. Therefore, rain chances would technically be rather high (70% - 100%) despite it only raining for a few hours. In summation, the NWS’s take on the chances of precipitation, they define PoP as there being a given percent chance that precipitation that rain will occur at any point in the forecasted area throughout the entire forecasted period, often being 6 to 12 hours. This interpretation may seem daunting and raise additional questions. Realistically, most of us are only concerned with the chance of rain for our region, not a large swatch of land. For all we know, the area our weatherman is discussing could be 2 square miles around us or the entire county. That’s why many on-air meteorologists have multiple interpretations when it comes to PoP.

These interpretations have similar definitions but are not all the same. Steve Hamilton, an on-air meteorologist for The Storm Report, Inc., believes there are “several disconnects between weather presenters, the NWS, and consumers” in regard to PoP. Mr. Hamilton believes the primary reasons for these disconnects are due to most consumers “not understanding the technical aspects of PoP” and the fact “on-air meteorologists rarely have the time to explain PoP in a cognitive way during their short segment.” With multiple interpretations, the definition and understanding of PoP can become confusing. According to a study performed by the University of Georgia, there is inconsistency with the use of the definition of PoP within the meteorological community itself: “Respondents expressed a range of different definitions of PoP and were highly confident in the accuracy of “their” [own] definitions”. This study should concern the weather community simply because it demonstrates that the general misunderstandings about PoP does not solely lie within the listening audience. So, what can we do to solve this issue? Mr. Hamilton suggests that weather presenters “avoid using PoP in favor of similar terms or broad statements”. Instead, the weather presenter could “be more specific about when, where and how much precipitation can be expected within their [consumer] specific coverage area.” Perhaps the weather community as a whole should strive for a single industry standard definition of PoP, thus allowing us to better communicate and educate those around us.

©2018 Meteorologist Ash Bray
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What’s cold air damming and why it’s connected to the cold in North and South Carolina? (National Weather Service, University at Albany – Lance F. Bosart and Gerald D. Bell)

4/19/2018

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It’s the middle of April, and you’re probably wondering why it’s still cold. You are also probably wondering what “cold air damming” is, and why these two are related. 
 
When a high-pressure system moves to the east of a north-south oriented mountain range, a barrier jet will form behind the cold front and move towards the North and South Poles and the Equator. 
 
Bringing you back to science class, cold air is denser than warm air, and will sink to lower elevations faster. Take, for example, oil and vinegar. The vinegar is the cold air; it’s denser and will sink towards the bottom of the glass. Oil, on the other hand, is like the warm air; and will rise towards the top of the glass. The oil and vinegar stay separated until someone, or something shakes it up, just like the warm air will remain on top of the cold air. Even though we really want the cold air to get pushed out and away, in a situation like cold air damming, it’s not that easy. 
 
The cold air sits at the surface, keeping areas like the North and South Carolina and Virginia in a non-stormy cold and cloudy area. The cold air essentially has nowhere to go because of the Appalachian Mountains that stretch north-south. The peaks of these mountains are at a higher height, that cold air cannot rise above. 
 
Cold air damming is most commonly known to affect places like the Carolinas and Virginia in the U.S. But the south of the Alps in Italy and near Taiwan and Korea in Asia are also prone to cold air damming. 
 
One of the simplest ways to get rid of cold air damming is through cold air advection. Cold air advection allows cold air to flow in weakening the warm and cold boundary layer in the atmosphere. Just like in the example above, we needed something to shake up the oil and vinegar so that they weren’t separated. In this case, the cold air advection is that something that comes in and “shakes up” the temperature inversion, allowing solar heating which ultimately warms up the surface. 
 
To learn more about other neat educational topics in meteorology, be sure to click here!

© 2018 Weather Forecaster Allison Finch

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More Insights about the Science of Snowflakes (credit: NOAA National Weather Service)

4/10/2018

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Did you know that no two snowflakes are alike, but they are all 6-sided? https://t.co/eNUWF3T3mS #SnowflakeScience pic.twitter.com/T1KlniIBam

— NWS (@NWS) April 9, 2018
DISCUSSION: During the course of the Winter-time months all over the world, many regions periodically experience various types of snowstorms. During snowstorms, the operative issue which comes into play for the general public aside from colder temperatures and windy conditions is the occurrence of accumulating snowfall.  Thus, a major concern for operational forecasters throughout the National Weather Service is to always have as much information as possible to create as accurate of a snowfall forecast as possible.  There are many parts of a snowfall forecast which are critical to piecing together an accurate snowfall forecast, but some aspects of any given snowstorm are more important than others.  For example, the height at which snowflakes form is a critical factor since that determines what sort of temperature and moisture regime the snowflakes form within.

Moreover, depending upon the persistence of the mid/low-level temperatures within a given snowstorm, that will also chiefly control the type of snowflakes which are generated since gradual differences in temperatures between approximately 32 and 0 degrees generate snowflake types which range from needles, to plates, to bars, to the most classic (and world-famous) dendrites.  Attached below is an exact excerpt from the source article courtesy of the National Weather Service which discusses a bit more about the process by which snowflakes form. 

"The intricate shape of a single arm of the snowflake is determined by the atmospheric conditions experienced by entire ice crystal as it falls. A crystal might begin to grow arms in one manner, and then minutes or even seconds later, slight changes in the surrounding temperature or humidity causes the crystal to grow in another way. Although the six-sided shape is always maintained, the ice crystal (and its six arms) may branch off in new directions. Because each arm experiences the same atmospheric conditions, the arms look identical."

To learn more about this particular snowflake article, please click here!

To learn more about other neat educational topics in meteorology, be sure to click here!

© 2018 Meteorologist Jordan Rabinowitz
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How Southern California Is Trying to Beat the "Urban Heat Island" Effect. (credit: CBS News)

4/10/2018

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To combat climate change, Los Angeles is painting some of its streets white and the reasons why are pretty cool -- literally. https://t.co/jfv1qL6U9m pic.twitter.com/f2Dhyrtd9C

— CBS News (@CBSNews) April 11, 2018
DISCUSSION: In recent days and weeks, the city of Los Angeles, California has made strides to work on fighting against the impacts of the infamous "urban heat island" effect. The "urban heat island" effect is a geographically-driven tendency wherein more urban regions are more prone to encountering greater amounts of increased localized daytime maximum temperatures.  This is a direct result of the fact that in more urban areas there is often much more developed infrastructure along with more paved roads with black-top.  This increased presence of black-top across the more urbanized towns and cities allow for more absorption of incoming shortwave radiation from the Sun which ultimately induces a positive feedback loop that favors hotter temperatures on a localized scale.

However, the city of Los Angeles, California is working to fight back against their local version of the "urban heat island" effect by painting their streets with white paint.  Due to the lighter nature of the white-colored streets across certain parts of the city, this facilitates street-top temperatures of roughly 10 to 15 degrees Fahrenheit less than those painted black.  As a result of this major temperature differential, this also has major consequences for energy interests since such major difference in maximum surface temperatures creates major differences in demands with respect to variable amounts of air conditioning requested by energy customers across the region.  Thus, it will continue to be interesting to see how much of a difference this makes in Los Angeles, California moving forward since it may be advantageous to do in other cities across the United States and around the world as well.

To learn more about other interesting educational stories in meteorology and other related issues, click here!

​
© 2018 Meteorologist Jordan Rabinowitz
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Putting Earth's Water Into Perspective                  (credit: USGS and NASA)

4/3/2018

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DISCUSSION: Many people living around the world are consistently humbled by Earth's oceans and their massive coverage area.  However, what is not readily apparent to many people is the fact that Earth's oceans are actually relatively shallower with respect to the size and mass of the planet Earth itself.  In fact, as shown to scale in the image above (courtesy of research scientists from both the United States Geologic Survey and the National Aeronautic and Space Administration), the total mass of all the surface and near-surface water throughout Earth's rivers, lakes, and oceans put together would likely only amount to a ball with a radius of roughly about 700 kilometers.  As a point of reference, a radius of 700 kilometers is only about half the radius of Earth's moon which is just goes to show how much water there actually is on Earth as compared to the mass of Earth's inner/outer core and the landmasses which make up Earth's continents and such. 

Having said everything above, it is important to still understand and recognize the critical importance and unique value of Earth's water resources (i.e., both fresh-water and salt-water alike).  First and foremost because of the fact that the Earth has a limited supply of freshwater left on the planet and in order to keep Earth in a sustainable mode, mankind must utilize these resources in logically-sound ways so as to not overuse and/or waste unnecessary amounts of freshwater.  

That being said, it is particularly interesting to truly recognize how much of a contrast there actually is between the amount of water on Earth and the relative size of the Earth itself.  Many people often perceive Earth's oceans as a seemingly never-ending feature which has been found to cover a little over 2/3 of Earth's surface. Nonetheless, it certainly puts things into real perspective when one realizes how little water there is in comparison to the rest of the planet.

To read the full story as posted by NASA, click on the following link: 
https://apod.nasa.gov/apod/ap160911.html?utm_content=bufferd7451&utm_medium=social&utm_source=twitter.com&utm_campaign=buffer.

​To learn more about other interesting educational topics across meteorology and related sciences, click on the following link:                           https://www.globalweatherclimatecenter.com/education.

​© 2018 Meteorologist Jordan Rabinowitz
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