What is a Heat Wave?

Because our reaction to weather is relative to the climate we live in, there are a few definitions of a heat wave. All of the definitions indicate it as a period of abnormally and uncomfortably hot and usually humid weather.

The World Meteorological Organization is specific in its definition by stating that a heat wave is when the daily maximum temperature for more than five consecutive days exceeds the average maximum temperature by 9 degrees.

Heat waves are caused by very hot, stagnant air masses. Regions that suffer under intense hot spells are usually dominated by a surface high-pressure system with a mid-tropospheric ridge aloft. Dew points are also high, and to compound matters, wind speeds are often low.

Clear or partly cloudy skies allow intense solar energy to further heat the ground and the air mass. During the heat wave of last week, Wisconsin experienced heat index readings that were over 100 degrees.

High humidity and stagnant air reduce the body’s ability to cool down through sweating. Lives are endangered when these conditions persist day and night for several days. Each summer in the United States, approximately 175 to 200 deaths are attributable to heat waves. Most of these deaths occur in cities, particularly northern cities.

Heat waves also have a strong economic impact. A prolonged heat wave can cause the widespread use of air conditioning, leading to increased demands for power that stress gas and electric utilities. Transportation can be stymied when highway surfaces and railways buckle and warp in the heat. All types of outdoor work, such as landscaping and construction, experience reduced productivity. Agriculture is especially vulnerable as heat waves stunt crops and kill livestock.

Category: Phenomena
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What are Straight-line Winds?

The term “straight-line winds” is used to describe ground-level winds that come out of a thunderstorm and do not have rotation. If these winds travel at speeds that exceed 57 mph, then the storm is classified as a severe thunderstorm. Storms with severe straight-line winds can also have hail and tornadoes.

Straight-line winds can cause considerable damage because these winds often do not let up. Straight-line winds will push objects over, all in the same direction as the wind is blowing.

The lack of rotation, or spin, in these straight-line winds allows meteorologists to differentiate damage from tornadic winds. Tornadoes scatter objects all over because they rotate so quickly.

Straight-line winds can be hazardous as they can push over objects that land on top of people, causing injury and death. On July 1, straight-line winds blew down trees in forested areas of northwest Wisconsin. Many areas had wind speeds of greater than 60 mph, with some wind speeds greater than 100 mph.

Thunderstorms have upward air motions, called updrafts. These supply warm moist air to the storm and help to form the precipitation. There are also downdrafts, or sinking air in a storm. Such downdrafts carry air from high elevations in the atmosphere rapidly to the ground. Since wind speed is nearly always much larger at high elevations, the downdrafts carry very high momentum air to the surface creating the straight-line winds.

Downdrafts also carry liquid water with them. When these downdrafts hit a region of dry air, such as below the cloud base, the drops evaporate. This cools the air in the downdraft, making it denser and thus causing the air in the downdraft to fall to the ground faster. You can sometimes notice this blast of cool air at the surface, often before it rains.

Category: Severe Weather
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What is the Midwest’s hottest summer on record?

Though it has been hot and humid lately in southern Wisconsin, this summer has been relatively mild compared to previous summers.

Since June 1 in Madison, the daily average temperature has been 1.8 degrees above normal and we have had four days with high temperatures hotter than 90 degrees (and three more at 89 degrees).

In 1988, Madison had 35 days with high temperatures over 90 degrees (but only 11 before July 8 ) with one stretch of nine straight days over 90 degrees from late July through the first week of August.

The summer of 1955 has the record of 40 days with highs over 90 degrees. For comparison, the average number of such days in Madison over the last 15 years has been 5.6 per year, with zero occurring in 2004.

The summer of 1936 easily stands as the hottest summer in the modern history of North America. First, in Madison, the hottest day of all time occurred on July 13, 1936, when the temperature reached 107 degrees (the all-time state record of 114 degrees was set the same day at Wisconsin Dells). That second week of July 1936 was so unbearably hot that residents of Madison elected to sleep outside on the Capitol Square seeking relief from the heat of their homes.

Across the Midwest it was even worse. In Steele, N.D., the all-time state record of 121 degrees was set July 6. Chicago’s Midway Airport recorded high temperatures of 100 degrees or higher on 12 consecutive days from July 6-17. Later that summer a string of 18 consecutive days at or above 100 degrees was recorded in Mount Vernon, Ill., from Aug. 12 to Aug. 29. Finally, Lincoln, Neb., recorded a daily minimum temperature of 91 degrees on July 25.

So despite the recent heat, it could be much worse.

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Do we have a new ‘normal temperature’?

Yes, the entire nation now has a new ‘normal temperature.’

These climatological temperatures, and other weather parameters, are computed by averaging all temperatures over a 30-year period. These averages are called normal temperatures. These averages serve as a reference point and are used to help us interpret average climate conditions at a particular location. A comparison of today’s temperature with the normal temperature helps us determine if today is an atypical weather day.

Private industry also uses these temperatures in planning. For example, energy companies use the normal temperature for long-term planning of energy usage. Agriculture uses this as they monitor a particular growing season.

The National Ocean and Atmosphere Administration’s National Climatic Data Center (or NCDC) calculates the normal weather conditions over a 30-year period for more than 7,500 locations in the United States.

Since this time period is a reference point, we have to define the 30-year period. As of July 1, this averaging period is 1981-2010. Prior to that date, the averaging period was 1971-2000. So, what does this new period tell us?

The normal temperature for the entire US is about 0.5 degrees warmer now than it was during the 1971-2000 time period. The normal low temperature for WI is about 0.8 degrees warmer now than it was in the 1971-2000 period; and Wisconsin’s normal high temperature is about 0.6 degrees warmer. According to Assistant State Climatologist, Dr. E. Hopkins, the new normal high and low temperatures for Madison are 56.6 and 36.7, which are 0.2 and 1.2 degrees higher than the previous 30-year period.

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Does lightning travel from the earth to the sky, or from the sky downward?

Lightning travels both ways.

Lightning is a huge electrical discharge that results from vigorous motions that occur in thunderstorms. Lightning can travel from cloud to cloud, within the same cloud, or between the cloud and ground. In-cloud lightning discharges are more common than cloud-to-ground discharges and are not as hazardous. Cloud-to-ground is the best known type of lightning and it poses the greatest risk.

A typical cloud-to-ground flash begins as negative charges travel toward the ground in a sequence of spurts. This makes the ground positively charged. As the negative charges approach the ground, there is an upward stream of positive charges. When the two streams meet an initial flash occurs and a channel forms so that electricity can flow between the cloud and ground. This occurs so quickly that it looks like a single brilliant flash but high speed photography shows several bolts.

Cloud-to-ground lightning starts from the sky and heads downward but what we see can travel from the ground upward.

Over the last twenty years scientists have discovered that lightning also shoots upward out of the top of thunderstorms into the upper atmosphere. These lightning types are known as red sprites, elves and blue jets. We still lack full knowledge about these forms of lightning. We do know that red sprites and elves occur over cloud-to-ground lightning bolts. Blue jets occur in the stratosphere and have been observed by pilots.

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