What can be learned from the recurrence of extreme weather events?

Roberto Salas, left, and Lewis Sternhagen check a flooded car in Houston on May 26. This spring the Houston area has experienced five separate rain events that have been classified as "once in a hundred year" events, which have a 1 percent chance (or a 1-in-a -100 chance) of occurring in any given year. (Photo credit: Associated Press)

Roberto Salas, left, and Lewis Sternhagen check a flooded car in Houston on May 26. This spring the Houston area has experienced five separate rain events that have been classified as “once in a hundred year” events, which have a 1 percent chance (or a 1-in-a -100 chance) of occurring in any given year. (Photo credit: Associated Press)

In 2004, the Boston Red Sox won the World Series for the first time in 86 years and their loyal fans were ecstatic. In the very next year, the Chicago White Sox won their first World Series title in 88 years.

Never in the long history of baseball had two teams that had been denied championships for so long won those long-coveted titles in successive years. This circumstance was at least partially a function of the changes in baseball brought about by free agency — a fundamental change to the rules.

This spring the Houston area has experienced five separate rain events that have been classified as “once in a hundred year” events. A 100-year event has a 1 percent chance (or 1-in-a-100 chance) of occurring in any given year.

This designation is meant to suggest that the intensity of these events is not likely to return to Houston except every 100 years or so. Thus, to have experienced five such storms in a single season is extremely unlikely and points toward an alteration in the climate (a fundamental change in the “rules”) of the region.

In a similar way, readers might recall that here in Madison in March 2012 we recorded five days with temperatures at or above 80 degrees. In the prior 100 years, only five other March days had ever topped 80 degrees, so that was also exceptionally unusual and provided evidence also suggestive of a shift in the climate toward a warmer world.

As isolated incidents, these meteorological phenomena can be expected every so often even in an unchanging climate as there is a lot of internal variability in the atmosphere.

In the seemingly recurring sequence we have experienced in the past couple of decades, however, there is little doubt that such events are among the fingerprints of a changing climate — a reality that we simply must confront in a coordinated, scientifically informed manner. A great number of dedicated scientists at UW-Madison are actively seeking better understanding of the complicated weather/climate system.

Category: Climate, Meteorology, Severe Weather

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How will a warmer planet affect the severity of mid-latitude storms?

Motorists and a fire engine brave high water on East Washington Avenue between the cross streets of Blount and Livingston Streets after a strong storm dumped large amounts of rain in Madison on June 30, 2014.  Storms in the warmer, moister atmosphere of the future have the potential to be more severe than otherwise similar storms today.  (Photo credit:  M. P. King, State Journal archives)

Motorists and a fire engine brave high water on East Washington Avenue between the cross streets of Blount and Livingston Streets after a strong storm dumped large amounts of rain in Madison on June 30, 2014. Storms in the warmer, moister atmosphere of the future have the potential to be more severe than otherwise similar storms today. (Photo credit: M. P. King, State Journal archives)

In an individual storm, the release of latent heat results in stronger updrafts of air (which form the precipitation) and in stronger winds associated with the storm.

One of the consequences of the gradual global warming that is currently occurring is that more water vapor finds its way into the atmosphere when the temperature rises.

As the temperature continues to warm, even more water vapor will reside in the atmosphere. Thus, storms in the warmer, moister atmosphere of the future have the potential to be more severe than otherwise similar storms today.

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Though the storms themselves develop in response to their large-scale environments, their development also directly impacts those environments in ways that are not yet well understood.

Especially unknown is the way in which the more abundant moisture of a warmer atmosphere will help shape the large-scale environments of the future.

Some studies suggest that the overall number of storms may decrease but that particularly severe storms may become more frequent.

Still others suggest no increase in the number of severe storms.

One thing seems certain: As the planet continues to warm, increases in the water vapor content of the atmosphere will likely change the frequency and distribution of mid-latitude storms and our agricultural and transportation infrastructure will have to adapt to those changes.

Category: Climate, Meteorology, Severe Weather

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What is the hydrologic cycle?

Because the cyclic nature of the water cycle, removal of groundwater can reduce surface water in lakes and streams. (Photo credit: The Capital Times archives)

Due to the cyclical nature of the hydrologic cycle, removal of groundwater can reduce surface water in lakes and streams. (Photo credit: The Capital Times archives)

The hydrologic cycle describes the circulation of water from the ocean and other watery surfaces to the atmosphere and to the land.

A major source of atmospheric water vapor is evaporation from the oceans. Precipitation — rain, snow, sleet or freezing rain — falls from clouds and is a loss of atmospheric water as it removes water from the atmosphere.

Precipitation returns water to the Earth’s surface and is a source of water for land. Precipitation on land may collect in lakes, run in rivers back to the ocean or percolate into the soil.

The hydrologic cycle is an interactive system. Water in the atmosphere, in the ocean, on land and underground is linked, and changing one modifies the others.

Since water plays a major role in weather and climate, it is important to understand the hydrologic cycle. A change in one component of the hydrologic cycle can affect weather. For example, a decrease in the amount of cloud cover over land during the day will allow more solar energy to reach the surface and warm the ground and the atmosphere above.

Another example is how an increased frequency in intense precipitation events over land areas can lead to flooding rather than waters seeping into aquifers.

While the hydrologic cycle is a global phenomenon, there are regional aspects that impact Wisconsin as hydrological changes across watersheds impact water supply. With ongoing climate change, shifts in precipitation patterns can impact water resources and thus management practices.

A drop in precipitation over a watershed will reduce the amount of surface waters and thus percolation into the ground. Most Wisconsin residents get their drinking water from groundwater.

Similarly, because of the cyclical nature of the water cycle, removal of groundwater can reduce surface water in lakes and streams. Groundwater recharge, water filtration and flood prevention practices may have to adapt to our observed regional climate change. Such adaptations need to consider the water cycle as an interactive system and not an isolated event.

Category: Climate, Meteorology

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How does weather impact forest fires?

Wildfires south of Fort McMurray in Alberta Canada on 5/7/16. (Credit: Jonathan Hayward –  Canadian Press)

Fires require fuel to burn, heat to ignite and oxygen to feed the chemical reaction. Weather plays a key role in all of these requirements to start and spread a forest fire.

Weather and climate are important in making fuel available by determining the moisture content of the vegetation. A long period without rain dries out the vegetation, making it easier to burn and thus a better fuel source.

Low humidity makes it easier to start and spread a fire. Trees and shrubs wet from rains make it more difficult to start a fire.

Lightning from thunderstorms often starts a wild fire in remote areas. Hot days will warm and dry potential fuels, making the fire easier to start and increasing the rate at which it can spread.

Winds also play an important role in starting and spreading a fire by fanning the flames of the initial spark from a lightning bolt. The winds provide fresh oxygen that can also stir a fire that has died down. Winds help steer, along with fuel availability and topography, the direction and progress of a fire.

A large fire can generate a wind pattern of its own that can help to spread the fire. Rotating winds can develop along the edge of a hot fire. These vortices are a result of the contrast between the hot air associated with the fire edge and the cooler air over the adjacent, non-burning region.

Fire tornadoes can be generated when the vortices are tilted from the horizontal to a vertical direction. Fire tornadoes can be composed of flames or black smoke and can toss burning debris into the non-burning area, helping to spread the fire.

The substantial influence that the fire has on the winds surrounding it makes the precise direction and speed of the spread of the fire difficult to forecast.

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, Phenomena, Weather Dangers

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Is our growing season getting longer?

Khadga Acharya, right, and her mother-in-law, Kala Acharya, harvest an early season crop of herbs from their family's garden plot at the Fountain of Live Community Garden in Madison last June. Wisconsin's growing season has lengthened by about 12 days, allowing production of longer-season crop types and varieties. (Photo credit: John Hart - State Journal)

Khadga Acharya, right, and her mother-in-law, Kala Acharya, harvest an early season crop of herbs from their family’s garden plot in Madison.  Wisconsin’s growing season has lengthened by about 12 days, allowing production of longer-season crop types and varieties. (Photo credit: John Hart – State Journal)

Yes. There are several studies that demonstrate shifts in the timing and length of the growing season.

One way to measure the length of the growing season is to count the number of days between the last frost in spring and the first frost in fall. By this measure, Wisconsin’s growing season lengthened by about 12 days between 1950 and 2006.

Longer growing seasons allow production of longer-season crop types and varieties.

The Growing Degree Days, or GDD, is a heat index that is related to plant development and is used to predict when a crop will reach maturity.

Each day’s GDD is calculated by subtracting a reference temperature, which varies with plant species, from the daily mean temperature, setting values less than zero to zero.

The reference temperature for a given plant is the temperature below which development for that plant either slows or stops.For example, cool season plants, like peas, have a reference temperature of 40 degrees, while warm season plants, like sweet corn and soybeans, have a reference temperature of 50 degrees.

The development of plants depends on the accumulation of heat. Since cool season plants have a lower reference temperature, they accumulate GDDs faster than warm season plants.

When drought or pests do not overly stress plants, the summation of the GDD can be used to measure the accumulation of heat and thus predict when a crop will reach maturity.

GDDs can be computed using climatic temperatures of an area. With that computation, we can estimate good crops to grow in a given region, similar to plant hardy zones. The longer growing season and warmer temperatures results in a changing GDD that is favorable to warm season plants.

Category: Climate, Seasons

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