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.
If a tornado is approaching, seek shelter in a basement or an interior room on the lowest level of a sturdy building. Cover yourself with heavy blankets or a mattress to protect against flying debris. Stay tuned to a weather radio or local news for updates on the situation.
An F5 tornado can potentially kill dozens to hundreds of people, depending on population density, time of day, and warning lead time. These tornadoes are among the most powerful and destructive, capable of causing widespread devastation and loss of life.
Kansas is part of an area known as Tornado Alley, where weather conditions are favorable for tornado formation. Kansas also has a high population density in its tornado-prone areas, increasing the likelihood of tornado deaths. Additionally, the state's expansive rural areas may make it difficult for residents to seek shelter quickly during tornado warnings.
12. It is very hard to find the most updated news. So the most updated one I could find said 12 people. However not all of those people were in Greensberg however they were all killed by the same tornado.
On average, tornadoes in Canada are responsible for causing 10 fatalities per year. However, this number can vary widely from year to year depending on the severity and frequency of tornado events.
The largest tornado on record (the Hallam, Nebraska tornado of May 22, 2004) was produced by a supercell thunderstorm that most likely was associated with a cold front or dry line.
The dry line can cause tornadoes. The dry line can in fact be more conducive for the formation of tornadoes than a cold front is. The area where a cold front and dry line intersect, called a triple point, is often a hot spot for tornado formation.
Tornadoes typically form in severe thunderstorms that have a combination of warm, moist air near the surface and cool, dry air aloft. A change in wind direction and speed with height (wind shear) is also important for creating the rotation necessary for tornado formation. Additionally, a trigger, such as a cold front or a dry line, can initiate the storm that produces the tornado.
You can't without it
A tornado.
On the day of the Waco tornado a weather system pushed dry air from New Mexico across Texas, where it collided with warm, humid air from the Gulf of Mexico, forming what is called a dry line. As the moist air was force over the dry air, thunderstorms began to develop. These storms were particularly strong and, when they encountered wind shear, began to rotate and produce tornadoes. One of these storms, possibly strengthened by air flowing out of a nearby storm, became especially strong and spawned an especially violent tornado southwest of Waco. That tornado tracked right through Waco.
Tornado: A violent, rotating column of air extending from a thunderstorm to the ground. Funnel cloud: A rotating, funnel-shaped cloud that forms before a tornado touches down. Wind speed: The strength of the winds in a tornado, measured in miles per hour. Debris: Objects and materials that are lifted and carried by a tornado's strong winds, causing damage.
Tornado Alley is marked by its flat terrain, which allows warm, moist air from the Gulf of Mexico to mix with cool, dry air from the Rockies, creating the ideal conditions for tornado formation. Additionally, the lack of geographic barriers in this region allows storms to develop and rotate more easily, increasing the likelihood of tornadoes.
A number of climatic factors come together in the region known as Tornado Alley. Warm moist air from the Gulf of Mexico moves over the region, carrying enormous amounts of energy to fuel thunderstorms. It can then collide with cool air from Canada (along a cold front) or dry air from the Rockies (along a dry line). This releases the energy carried by the warm, moist air producing thunderstorms that can become very strong. They can be especially violent where a dry line intersects a cold front. Additionally, Tornado Alley gets a lot of strong wind shear. This can intensify the storms even further and can also give the the rotation they need to produce tornadoes and generally speaking the stronger the storm, the stronger the tornado it can produce.
A tornado.
dry places like Texas and Colorado
By definition the wind in a tornado rotates, regardless of the tornado's intensity. Straight line winds travel on a relatively straight path and don not contain a circulation, though they can reach intensity similar to that of a tornado, in some cases equivalent to an EF2.