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My Sitemap
Alphabetical Sitemap
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To find your local weather 7-day weather forecast, enter your zip code or City and State information below. Also,current updated weather map.
Zip-Code-Weather-Forecast.html
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index.html
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Best Aviation Weather Observer Course, SAWRS, LAWRS, AWO, METAR, SPECI' Become Certified
Observer-COURSES.php
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Most Comprehensive Weather Observer home study course available. Learn METAR SAWRS LAWRS. Read and code Aviation Weather reportrs.
Home-Study-Observer-Course.html
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Professional Weather Observer Training. for corporations. Learn Metar, Speci, NWS certification examination.SAWRS, LAWRS, general observer training.
On-Site-Training.html
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Current watches and warnings map from the National Weather Service
Current-Weather-Maps.html
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see how weather balloons are released and how computers track the radiosonde to record information from the atmosphere..
Wx-Balloon-Videos.html
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Learn everything about clouds, how they form, what they weigh, what colors they are.. PHOTOGRAPHS OF CLOUDS.
More-About-Clouds.php
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White-Clouds.php
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Blue-or-Grey-Clouds.php
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Green-Clouds.php
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Red-Clouds.php
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Cumulonimbus is a heavy and dense cloud, with considerable vertical extent, in the form of a mountain or huge towers.
Cumulonimbus-Clouds.php
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Cumulonimbus-Mammatus.php
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Contrails form from the exhaust of jet engines when humidity is high and air is cold.
Contrails.php
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Lenticularis clouds are lens shaped clouds formed on the lee side of mountains
Lenticular-Clouds.php
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Cirrus clouds are detached clouds in the form of white, delicate filaments, sometimes shaped like commas, or white patches or narrow bands.
Cirrus-Clouds.php
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Grey cloud layer, often dark. Its appearance is diffused by more or less continuously falling rain or snow.
Nimbostratus-Clouds.php
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Stratus clouds form a generally grey cloud layer with a faily uniform base.
Stratus-Clouds.php
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Stratocumulus clouds are grey or whitish, or both grey and whitish, patch, sheet or layer of cloud which almost always has dark parts, composed of rounded masses, rolls, etc, which may or may not be merged.
Stratocumulus-Clouds.phpl
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Cumulus clouds are detached clouds that often resemble cauliflower. They are "puffy" in appearance, generally dense and with sharp outlines.
Cumulus-Clouds.php
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These are turbulent altocumulous type clouds
Rotor-Cloud.php
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Cirrocumulus clouds are thin, white patchy, sheet or layer of cloud without shading.
Cirrocumulus-Clouds.php
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Transparent, whitish cloud veil of fibrous, hair-like or smooth appearance, totally or partly covering the sky and generally producing halo phenomena
Cirrostratus-Clouds.php
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Altocumulus clouds are white or grey, or both. They appear as a sheet or layer of cloud, generally with shading composed of rounded masses, rolls, etc.
Altocumulus-Clouds.php
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Altostratus is a greyish or bluish cloud sheet or layer of striated, fibrous or uniform appearance which totally or partly covers the sky, but having parts thin enough to reveal the sun at least vaguely, as through ground glass.
Altostratus-Clouds.php
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As the radiosonde is lifted up into the sky, sensors measure pressure, temperature, and relative humidity and a battery powered transmitter sends the readings to a ground receiver.
Radiosonde.php
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Psychrometer is used to determine the amount of humidity in the air. It is used to determine relative humidity and dew point,
psychrometer.php
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The Dew Point Table can be used to calculate dew point. This table is for instruction purposes only. Never use this table for actual observations.
Sample-Dew-Point-Table.html
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How to determine and record temperature and dew point.
Procedure-For-Recording-Temperature-and-DewPoint.php
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How to read and aircraft altimeter
Reading-Aircraft-Altimeters.php
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How to use the Psychrometric Calculator to determine dew point and relative humidity
Psychrometric-Calculator.php
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Quite simply put, barometers measure the weight of the air in the atmosphere. As the air presses down on the mercury in the container, the mercury in the column moves up. When air pressure decreases and the mercury in the column weighs more than the air pressing upon it, the mercury in the column drops.
Barometer.php
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anemometers measure wind
Anemometers-Measure-Wind.php
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Photograph of blowing snow in Antarctica
Blowing-Snow.html
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Photograph of blowing snow in Antarctica
squall.html
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sandstorm video
Sandstorm.html
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dust devil video
Dust-Devil.html
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Tornado video
Tornado.html
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Invormation and video of thunderstorm.
Thunderstorm.html
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Hurricanes.html
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The Saffir-Simpson Hurricane Wind Scale is a newer 1 to 5 categorization based on a hurricane's intensity at landfall. Historically, the scale (then known as the Saffir-Simpson Hurricane Scale) used central pressure and storm surge as components of the categories. The problem with this method was that there are too many variables that influence storm surge.
Hurricanes-Categories.php
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More-about-Hurricane-Names.html
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Retired-Hurricane-Names.html
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Retired Hurricane Names that will not be used again for at least 10 years.
2004 Hurricane Names
2005 Hurricane Names
2006 Hurricane Names
2007 Hurricane Names
2008 Hurricane Names
2009-Hurricane-Names.html
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Retired Hurricane Names that will not be used again for at least 10 years.
2004 Hurricane Names
2005 Hurricane Names
2006 Hurricane Names
2007 Hurricane Names
2008 Hurricane Names
2004-Hurricane-Names.html
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Retired Hurricane Names that will not be used again for at least 10 years.
2004 Hurricane Names
2005 Hurricane Names
2006 Hurricane Names
2007 Hurricane Names
2008 Hurricane Names
2005-Hurricane-Names.html
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Retired Hurricane Names that will not be used again for at least 10 years.
2004 Hurricane Names
2005 Hurricane Names
2006 Hurricane Names
2007 Hurricane Names
2008 Hurricane Names
2006-Hurricane-Names.html
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Retired Hurricane Names that will not be used again for at least 10 years.
2004 Hurricane Names
2005 Hurricane Names
2006 Hurricane Names
2007 Hurricane Names
2008 Hurricane Names
2007-Hurricane-Names.html
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Retired Hurricane Names that will not be used again for at least 10 years.
2004 Hurricane Names
2005 Hurricane Names
2006 Hurricane Names
2007 Hurricane Names
2008 Hurricane Names
2008-Hurricane-Names.html
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This photograph is of a rare snowfall in New Orleans, Louisiana in mid December, 2009. It was responsible for stopping traffic, business and school closures, and happy children.
Snow.php
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Lightning.php
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Pressure differences can be caused by uneven heating of the earth's surface. When the sun heats the earth's surface, the air expands. With heating, air molecules move faster and bump each other farther apart. This is why the air can hold more moisture as well. If you were to measure the weight of a cubic foot of warm air, it would weigh less than a cubic foot of cold air because it has less molecules in it. This phenomea explains the normal small changes in pressure each day (relatively higher in the morning and lower in the afternoon.)
Air-pressure.php
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Pressure differences can be caused by uneven heating of the earth's surface. When the sun heats the earth's surface, the air expands. With heating, air molecules move faster and bump each other farther apart. This is why the air can hold more moisture as well. If you were to measure the weight of a cubic foot of warm air, it would weigh less than a cubic foot of cold air because it has less molecules in it. This phenomea explains the normal small changes in pressure each day (relatively higher in the morning and lower in the afternoon.)
Air-Pressure-and-Weather.php
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A study in Sweden provides an interesting insight into the possibility of a connection between suicide and excessive daylight. Greenland has the world’s highest suicide rate, and in its northern part, where the sun doesn’t set between April and August, suicide occurs more frequently, especially among young men.
Daylight-and-Suicide.php
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Sun-Exposure.html
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Aches-and-Pains.html
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Sun-&-Moon.html
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Wind-Chill-Heat-Index.html
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Humidity can harm your health and home. Condensation mold growth, humidifiers, insulation, vapor barrier
Home-Humidity.php
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There is a relationship between air pollution and weather. Certain weather conditions, such as thermally inversions which to name one, in combination with air pollutants, can create a serious public health issue.
Air-Quality-Weather.php
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But humidity impacts many other aspects of daily life including health and safety, as well. Mold, condensation, moisture damage, dry rot, etc. are related topics that concern anyone who works, plays or lives in a home.
Why-Care-About-Humidity.php
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A relative humidity of 0% will never occur naturally. Even the driest of deserts have at least a couple of percentages of humidity.
Is-Desert-Humidity-0%.php
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Altostratus is a greyish or bluish cloud sheet or layer of striated, fibrous or uniform appearance which totally or partly covers the sky, but having parts thin enough to reveal the sun at least vaguely, as through ground glass.
Does-Rain-Mean-RH-is-100%.php
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SAD-Seasonal-Affective-Disorder.html
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What-Causes-SAD.html
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Symptoms-of-SAD.html
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Reverse-SAD.html
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Treatment-of-SAD.html
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Photo-Therapy-for-SAD.html
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Where-to-Buy.html
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Answers to your weather questions. What makes the sky blue, what do radar image colors mean.
Weather-FAQ.html
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Twenty miles above earth, the sky is not blue, but black. But the earth’s atmosphere, which is largely nitrogen refracts light in a manner that makes it appear a beautiful blue color.
Why-Is-The-Sky-Blue.html
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How to order Home Study Course
How-Can-I-Buy-the-Home-Study-Course.html
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This is one of the most commonly asked questions. The answer depends on which maps you are looking at. Most often this question refers to the radar maps commonly seen in television broadcasts, which tell about weather moving through your area.
What-do-the-Colors-On-the-Weather-map-Mean.html
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Cloud colors can tell us about the clouds we are observing. Dark grey or black cloud bottoms tell us that the clouds contain rain-sized moisture, green clouds indicate the presence of ice. For more detailed answers, go to More About Clouds.
Why-Are-Some-Clouds-Different-Colors.html
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What-is-UTC-time.html
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World-Meteorological-Association.html
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weather calculator allows you to calculate and convert temperatures, dew point, and more.
Weather-Calculator.html
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Contact WeatherWing about courses or the website
Contact.html
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Privacy information for our site
Privacy-Policy.html
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Resources and Links
Resources-and-Links.html
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sitemap-alphabetical.html
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"I'd worked as an observer for years, but needed to
re-certify. I learned more in this course than I ever imagined
I could and I passed the exam with flying colors. I am also definately a better observer" TS,
Louisiana
I knew nothing about weather at all. My new
job depended on passing the weather observer certification test. Thanks to the patience and personal
attention you gave us all, the entire class passed. JB, Texas
"When my company sent
me to this class I thought I didn't need the training. I was wrong.
Thanks" RB, Texas
You are the "Gold
Standard" of teaching. Absolutely the best teacher I have ever had. DG,
Louisiana
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