How do you measure how hot the summer is?

One way to gauge how hot a summer season was is to count how many days reached 90 degrees F or above. It turns out that this number is extremely variable here in Madison. (Photo credit: State Journal archives)

One reasonable way to gauge how hot a summer season was is to consider how many days that year reached 90F or above. It turns out that this number is extremely variable here in Madison.

From 1971 to 2016, the average number of days at or above 90F in Madison is 10.9. As is often the case with statistics, however, the average does not convey a sense of the variability. A better way to express that variability is by calculating the standard deviation, which, when added to or subtracted from the average, sets a range in which approximately 2/3 of the years will fall.

In this case the standard deviation is 9.0. Thus, we might expect that 2/3 of the years would range from having 19.9 to 1.9 days at or above 90F. As it turns out, 34 of the last 46 summers have been in that range!

It is interesting to note that six summers have had 20 or more hot days (1975, 1976, 1983, 1988, 1995 and 2012) — the recent scorching summer of 2012 had 39 days (one short of the record 40 of 1955)!

Notably cold summers (by this measure) include 1979, 1996, 1998, 2000, 2004, 2008 and 2014 with 2004 being the only summer in the last 46 years in which the temperature never reached 90F.

Broken down into decades, there had been a trend toward fewer hot days each summer with the averages being 15.8, 11.7, 8.2 and 7.3 days for the 1970s, 1980s, 1990s and 2000s, respectively. The summer of 2012 singlehandedly accounts for a departure from this trend as this decade has thus far averaged 11.42 days (only 6.83 without 2012).

These data remind us how complicated the interplay between weather and climate can be since the global average temperature has been trending the other way in these same decades.

Category: Climate, Meteorology, Seasons

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When is the summer solstice?

This full disk image, one day before the 2017 summer solstice, illustrates the abundance of daylight in the northern hemisphere.

The summer solstice in the Northern Hemisphere is the day when the sun is farthest north.

In 2017, this occurs Tuesday at 11:24 p.m. Central Time.

As Earth orbits the Sun, its axis of rotation is tilted at an angle of 23.5 degrees from its orbital plane. Because Earth’s axis of spin always points in the same direction — toward the North Star — the orientation of Earth’s axis to the Sun is always changing as Earth orbits around the Sun.

As this orientation changes throughout the year, so does the distribution of sunlight on Earth’s surface at any given latitude. The summer solstice is the day of the year with the most daylight.

On the Northern Hemisphere’s summer solstice, the northern spin axis is tilted toward the sun and latitudes north of the Arctic Circle (66.5 degrees N) have 24 hours of daylight.

At the summer solstice, the sun reaches its highest point in the sky and daylight is longest. However, our earliest sunrise in Madison occurs in mid-June while our latest sunset occurs in late June.

So, while the summer solstice has the longest daylight hours, that day does not correspond to the earliest sunrise or the latest sunset. The reason that the earliest sunrise and latest sunset do not occur on the summer solstice is a combined effect of the tilt of Earth’s axis and the elliptical path of Earth around the sun.

On our solstice, the sun rises and sets farthest north of due east and due west. The farther the sun sets from due west along the horizon, the shallower the angle of the setting sun. That means a longer duration for sunset at the solstices.

Steve Ackerman and Jonathan Martin, professors in the UW-Madison department of atmospheric and oceanic sciences, are guests on WHA radio (970 AM) at 11:45 a.m. the last Monday of each month.

Category: Seasons

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What is a derecho?

A derecho (pronounced deh-RAY-cho, a Spanish word meaning “straight ahead”) is an hours-long windstorm associated with a line of severe thunderstorms.

It is a result of straight-line winds, not the rotary winds of a tornado — hence its name. Derechos in the United States are most common in the late spring and summer (May through August).

The extreme winds of a derecho — up to 150 mph in the strongest storms — come about in the following way. Derechos are often associated with a quasi-stationary front in mid-summer. If the atmosphere just north of the front is very unstable, the front may trigger rapidly developing thunderstorms. A line of thunderstorms that forms in the vicinity of the stationary front can, via its cold downdrafts, drag down high-speed air from above. This can cause the high winds of a derecho.

At the same time, the high winds push the line of thunderstorms outward, causing it to bend or “bow.” This results in a bow echo image on weather radar. Once they get going, derechos can cover lots of territory — up to 1,000 miles.

Derechos leave significant property damage in their wake, even flattening entire forests. In some cases, derechos wreak as much havoc as a hurricane or tornado.

The June 29, 2012, derecho swept across from U.S. from west of Chicago to the East Coast, leaving as many as 5 million households without power. The storm traveled at speeds of more than 60 mph, with wind gusts approaching 80 mph. At least 22 people were killed.

About 40 percent of all thunderstorm-related injuries and deaths occur because of derechos.

Category: Meteorology, Phenomena, Severe Weather

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Is the weather nicer on Memorial Day or Labor Day?

Suomi NPP VIIRS view of the Great Lakes Region on Memorial Day Weekend 2017 (5/27)

Memorial Day traditionally marks the beginning of the summer, while Labor Day marks the end.

People are bound to have their own recollections and opinions about which weekend more reliably delivers agreeable weather here in southern Wisconsin, and those opinions can be colored by many non-meteorological influences.

If forced to opine on this question while sticking to strictly meteorological factors, we would suggest that Labor Day weekend’s weather is more reliably summerlike.

The reason for this comes directly from the fact that Memorial Day comes as winter is ending and Labor Day as winter approaches.

As the winter ends, the entire Northern Hemisphere gradually warms up and the leftover cold air from the polar regions is gradually bled away to lower latitudes where it disappears.

This “bleeding” of cold air occurs in distinct blobs, known as cutoff lows. It is verifiable that there are many more cutoff lows in the hemisphere in May than in September.

These cutoffs can sometimes remain over a location for days at a time and negatively impact the local weather by engendering conditions that favor the development of thundershowers and persistent clouds, not to mention below normal temperatures. Our cooler weather early last week was related to such an event.

Since these features are more common in May, the weather is more prone to these undesirable unsettled periods this month than in September.

Category: Meteorology, Seasons

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Did someone predict the recent Wisconsin tornado?


Ron Bloomberg, who witnessed victim and neighbor Eric Gavin’s body being recovered, embraces his girlfriend as he returns to his home in Chetek, Wis., after a tornado flattened a trailer park and nearby trees. (Richard Tsong-Taatarii/Star Tribune via AP)

We cannot yet forecast tornado occurrence with any accuracy. One problem is the small size of a tornado, which is a narrow column of strong winds that rotate around a center of low pressure.

Over the last 60 years, forecasts of the development of large-scale low-pressure systems, which often organize the ingredients needed to form a tornado, have steadily improved. Because of these advances, meteorologists are better able to predict those conditions a few days in advance, enabling forecasters to identify counties where there is a threat of severe weather sometimes as many as three days in advance. Two days in advance of the recent EF-2 tornado (later upgraded to EF-3) that hit southeastern Polk County, the National Weather Service’s Storm Prediction Center’s convective outlook issued a slight-risk for the area.

For a thunderstorm to produce a tornado requires warm humid air near the surface with cold dry air above. These conditions make the atmosphere very unstable, in the sense that once air near the ground is forced upward, it ascends freely and quickly (like a helium balloon), cools as it expands and forms a storm. Severe thunderstorm conditions also include a layer of hot, dry air between the warm, humid air near the ground and the cool dry air aloft. This hot layer acts as a lid that allows the sun to further heat the warm, humid air — making the atmosphere even more unstable. In the central U.S., such air is created over the plateau of Mexico and sent northeastward over the Great Plains.

To form a tornado, the host thunderstorm must also rotate. This happens in a storm when wind at the ground is moving in a different direction and speed than the air above. The change in wind speed and direction with height is known as wind shear. Both wind shear and atmospheric instability are needed for tornado formation.

Recent advanced models have been able to simulate development of a tornado, a first step to better predictions. Advances in radar technologies have helped to identify storms that are producing a tornado, or about to produce one. Based on observations from such advanced technologies, the Storm Predication Center (SPC) issued a warning about one hour before the Polk County tornado, and the NWS issued a tornado warning about 10 minutes before the first sighting of a funnel cloud.

Steve Ackerman and Jonathan Martin, professors in the UW-Madison department of atmospheric and oceanic sciences, are guests on WHA radio (970 AM) at 11:45 a.m. the last Monday of each month.

Category: Meteorology, Severe Weather

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