A dryline is a meteorological boundary that separates moist air from dry air, typically found in the Great Plains of the United States. It is characterized by a significant difference in humidity and can lead to the development of thunderstorms when moist air rises over the dry air. Drylines often form during the warmer months and can be a key factor in severe weather forecasting. They are distinct from cold fronts and warm fronts, which are associated with temperature changes rather than humidity differences.
Dryline thunderstorms most frequently form in the southern Great Plains region of the US, including parts of Texas, Oklahoma, Kansas, and Nebraska. The dryline is a boundary between moist air from the Gulf of Mexico and dry air from the southwestern US, creating an environment conducive for thunderstorm development.
Considering the dryline runs right down the state it is not unusual at all for classified storms to develop without pre warning. Said storms can range from high winds with downpours all the way to dropping baseball size hail.
Warm fronts play a can major role in many severe weather events. They often bring several key ingredients with them including lift and moisture. Although they are not totally necessary for tornado development, they do play a major role in a substantial number of tornadic events. However, warm fronts are typically cause simple rain shows rather than severe weather of any sort. Tornadoes and other forms of severe weather occur more often with cold fronts.
Dryline thunderstorms most frequently form in the southern Great Plains region of the US, including parts of Texas, Oklahoma, Kansas, and Nebraska. The dryline is a boundary between moist air from the Gulf of Mexico and dry air from the southwestern US, creating an environment conducive for thunderstorm development.
Tornadoes are caused by the rotation of supercell thunderstorms within a specific atmospheric environment. The combination of wind shear, instability, moisture, and a triggering mechanism such as a cold front or dryline sets the conditions for tornado formation. The rotation within the storm can intensify into a tornado when it reaches the ground.
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Well, What makes dryline storms so great is they are usually easily visible, rise quickly, and can provide a clear view of the tornado from beginning to end. If you have ever chased in dew points in the middle 70's with moisture streaming in continually, usually you can't see more than 1/4 a mile ahead of you. Trying to spot a storm in low visibility is often not worth the effort. You can be 1/2 mile away from a tornado and can't see it because the humid air 'cuts' your view. Where-as Dryline storms can pop up from clear blue skies at a rapid rate, and often leave you with a full 360 degree view while they build giving you a spectacular show.
Considering the dryline runs right down the state it is not unusual at all for classified storms to develop without pre warning. Said storms can range from high winds with downpours all the way to dropping baseball size hail.
Thunder storms are caused by warm, moist air rising through the atmosphere. As this air rises it cools and the moisture condenses, forming clouds. If the updrafts driving this are strong enough the clouds develop from cumulus clouds, to tall cumulus congestus clouds, to large cumulonimbus clouds. It is these clouds that are usually called thunderstorms. Often the updrafts are triggered when the warm air mass meets a cooler and/or drier air mass (along a cold front or dryline). The lighting itself comes from positive and negative charges within the thunder cloud and on the ground. The ground and top of the cloud generally carry positive charges and the bottom of the cloud generally carries a negative charge. Eventually enough of a charge difference builds up the the electricity discharges in the form of lightning. The lightning superheats the air to tens of thousands of degrees in a fraction of a second, creating a shockwave that is hear as thunder.
Warm fronts play a can major role in many severe weather events. They often bring several key ingredients with them including lift and moisture. Although they are not totally necessary for tornado development, they do play a major role in a substantial number of tornadic events. However, warm fronts are typically cause simple rain shows rather than severe weather of any sort. Tornadoes and other forms of severe weather occur more often with cold fronts.
They don't happen instantly, but they do certainly form quickly compared with other types of storm. This simply has to do with the scale on which they exist. In weather terms tornadoes are microscale weather patterns, referring to things that are less than a few kilometers in size. (The largest known tornado was 4 km, or 2.5 miles wide. Most are much smaller.) Because of their small size the mechanisms behind microscale systems operate quickly, causing them to form and dissipate in minutes or seconds in most cases. In addition to tornadoes, other microscale systems include turbulence and individual cumulus clouds.
Tornadoes occur mainly in the United States, particularly in the middle part of the country, in the region of the Great Plains states known as Tornado Alley. But very severe outbreaks have occurred in Florida and the Gulf Coast, and around the Great Lakes. Tornadoes can occur nearly anywhere that gets thunderstorms, which is anywhere in the world except Antarctica. They are rare in the Northern polar region as well. They are very prevalent in the 40 to 60 degree latitudes in both hemispheres. Tornadoes are more common in the United States, UK, and Australia. Tornadoes may be spawned by tropical storms and cyclones when they make landfall. These are seldom as severe as those associated with supercells in the interior US.
Thunder is caused by lightning. Thunder is the sound caused by rapidly expanding gases a channel of lightning discharge. Lightning has enough energy to heat the air up to 18,000 degrees Fahrenheit. This causes a rapid spreading of the air, creating a sound wave heard as thunder. The sharp click or crack heard very near, right before the main crash of thunder.Thunder is the sound produced after a lightening strike. Lightening is a huge electrical discharge. The charge pushes apart the air molecules. The molecules are heated rapidly and expand quickly. This creates vibration that reaches our ears as sound. You can tell how far apart the lightening strike is by counting the number of seconds between the flash and the sound. Approximately 1 miles is equal to 1 second, more or less. This works because of the speed at which sound travels.Thunder is the rumbling or crack of sound that can usually be heard from the sky during a storm.Thunder is caused because lightning heats up the air, to about 30 000ºC, causing it to expand quickly. The rumbling occurs as the sound passes through atmospheric layers at different temperatures.