Atmospheric and Oceanic Sciences turns 75

The rooftop of the UW–Madison Atmospheric, Oceanic and Space Sciences building. (Photo credit; UW-Madison)

On Friday, the Department of Atmospheric and Oceanic Sciences at the University of Wisconsin-Madison celebrated its 75th anniversary.

When the department was founded in June 1948, the modern science of meteorology was arguably just a few years old, and even basic understanding of the nature of the mid-latitude cyclones that batter us from October to May was truly in its infant stages.

The scholarship within our department over this three-quarters of a century has made enormous contributions to our science and, in turn, to the protection of lives and property through improved forecasts of both tropical and mid-latitude cyclones.

Some of the highlights include the launching of the first weather satellites in the late 1950s and early 1960s. These tools now contribute a huge amount of data to global weather forecasting models, and the UW-Madison remains at the very forefront of the research efforts dedicated to remotely sensing the atmosphere and oceans of Earth.

Developments in the computer models that make such forecasts also has a strong Wisconsin pedigree. The recently retired director of the National Weather Service got all three of his degrees from UW-Madison. The Space Science and Engineering Center, or SSEC, originally developed as an outgrowth of the department, has been at the heart of improved forecasts of tropical weather systems, fire detection and severe storms research for decades.

Clearer understanding of both tropical and extra-tropical weather systems, the global oceans and their interactions with sea ice, the complex climate system and many other important, fundamental issues in the atmospheric and oceanic sciences are being generated every day in our dynamic and diverse department. We are grateful to the citizens of the state of Wisconsin for their support of our endeavors, and those of all of our colleagues at our great University of Wisconsin-Madison.

On, Wisconsin!

Steve Ackerman and Jonathan Martin, professors in the UWMadison department of atmospheric and oceanic sciences, are guests on WHA radio (970 AM) at 11:45 a.m. the last Monday of each month. Send them your questions at stevea@ssec. wisc.edu or jemarti1@wisc.edu.

Category: History, Meteorology

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Higher overnight lows led to warm September

As we enter the month of October and the traditional end of the warm season, it’s interesting to note that the average temperature last month, through Sept. 28, was 4.0 degrees above normal in Madison.

Monthly climate observations for September 2023 showing deviation from normal. (Image credit: NOAA/NWS Sullivan office)

That is by far the biggest deviation among traditional warm-season months — June, July, August and September. All were warmer than average this year: June was 0.8 degrees, July just 0.5 degree and August only 1.2 degree above the respective norm.

If we break down the September temperature departure into contributions made by increased daytime highs and those made by higher overnight lows, the story gets even more interesting — and more telling. Through Sept. 28, the daily maximum temperatures have averaged 2.7 degrees Fahrenheit above normal, while the overnight lows have been 5.5 degrees warmer than average. Thus, warmer overnight lows last month have contributed about two-thirds of the total temperature anomaly.

Underlying the spike in overnight lows is the fact that the air is systematically a bit more humid as the global temperature increases, and water vapor is a very efficient greenhouse gas. Consequently, if there is more water vapor in the air, it is harder for the surface of the planet to lose energy to space overnight.

Change in overnight lows (°F)
Credit: WICCI

Our lowest daily temperatures have been a bit higher as a result.

This physics is not limited to the warm season — it applies generally.

The bias toward overnight temperature increases as the emblem of climate change is yet another way that the current slow warming of the planet nurtures a level of public skepticism that is out of proportion to the urgency of the threat.

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. send them your questions at stevea@ssec.wisc.edu or jemarti1@wisc.edu.

Category: Climate, History, Seasons

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Are day and night of equal hours on the equinox?

The two solstices happen in June (20 or 21) and December (21 or 22). These are the days when the Sun’s path in the sky is the farthest north or south from the Equator. A hemisphere’s winter solstice is the shortest day of the year and its summer solstice the year’s longest. In the Northern Hemisphere the June solstice marks the start of summer: this is when the North Pole is tilted closest to the Sun, and the Sun’s rays are directly overhead at the Tropic of Cancer. The December solstice marks the start of winter: at this point the South Pole is tilted closest to the Sun, and the Sun’s rays are directly overhead at the Tropic of Capricorn. (In the Southern Hemisphere the seasons are reversed.) (Image credit: Britannica)

This year, the autumnal equinox occurred on Saturday, Sept. 23, at 1:50 a.m. Central Time. During the equinox, the sun shines directly on the equator as its position moves from one hemisphere to the other. The word “equinox” is derived from the Latin word “aequus,” which means “equal,” and “nox,” which is the Latin word for “night.” During the 24 hours of the equinox, there are about 12 hours of day and 12 hours of night.

You may hear that daylight and nighttime are of equal length on the equinox. But during the equinox at our midlatitude location, there are approximately eight more minutes of daylight for two reasons: the sun’s shape and atmospheric refraction.

Sunrise time is most frequently defined as when the leading edge of the sun first touches the eastern horizon. Sunset occurs when the sun’s trailing edge touches the western horizon. This provides an extra 2½ to 3 minutes of daylight at our latitude.

In addition, our atmosphere acts like a lens, bending the light from the sun. When the sun is near the horizon, this refraction of the sunbeams has the effect of making the sun appear about a half a degree from its true position. When the sun appears to be on the horizon, it is actually just below the horizon geometrically. Atmospheric refraction advances the time of sunrise and delays the sunset, adding approximately six minutes of daylight. So, we have more daylight than night at the equinox.

The fall equinox marks the midpoint between the summer and winter solstices, and our daylight hours will continue to decrease as we approach the shortest day of the year, with about nine hours of daylight on Dec. 21. Our temperatures will also be getting colder.

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. Send them your questions at stevea@ssec.wisc.edu or jemarti1@wisc.edu.

Category: Meteorology, Seasons

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Do hurricanes affect Wisconsin?

Map showing the previous tracks of tropical systems that have traveled close to Wisconsin. Blue line segments indicate where the systems where tropical depressions and grey line segments indicate where they weakened to extratropical cyclones. (Image credit: NOAA/NWS Sullivan, WI)

A tropical cyclone is a rotating low-pressure system that has organized thunderstorms but no fronts. When a tropical cyclone’s maximum sustained winds reach 74 mph, it is called a hurricane. Hurricanes have never directly impacted the Upper Midwest region of the U.S.; however, the remnants of a hurricane or tropical storm have impacted the weather in the Midwest, including Wisconsin.

If a hurricane is particularly strong at landfall, it can move far enough northward to cause a significant rain event for areas in the Midwest. For the most part, such storms originally make landfall in Texas, Louisiana or Mississippi. These storms can be tracked by satellites or surface weather observations because they maintain an identifiable circulation pattern along their entire path.

A University of Iowa study analyzed discharge measurements of the U.S. Geological Survey (USGS) stream gauge stations from 1981 to 2011. Their study analyzed the stream gauge water discharges with the passage of the storms over the Midwest and eastern states and constructed maps of the relationship between inland flooding and tropical cyclones. The analysis demonstrated that these tropical storms can impact large areas of the United States, including Illinois, Wisconsin and Michigan. The natural hazards associated with these weather events are similar to flooding, which can impact 10 to 15 states hundreds of miles from the coast.

The amount of financial damage caused by such storms in the Midwest and the eastern United States will be a subject of future study.

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. Send them your questions at stevea@ssec.wisc.edu or jemarti1@wisc.edu.

Category: History, Meteorology, Severe Weather, Tropical

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Can we measure air pollution from satellites?

The TEMPO instrument is a UV-visible spectrometer, and will be the first ever space-based instrument to monitor air pollutants hourly across the North American continent during daytime. It will collect high-resolution measurements of ozone, nitrogen dioxide and other pollutants, data which will revolutionize air quality forecasts. (Image credit: NASA and Smithsonian Astrophysical Observatory)

The National Oceanic and Atmospheric Administration (NOAA) operates weather satellites with instruments capable of locating fires and determining fire characteristics such as size and intensity. These satellites also are critical to observing and monitoring smoke from those fires.

NASA recently launched a new satellite instrument to monitor air pollution. The Tropospheric Emissions: Monitoring of Pollution, or TEMPO, was launched into geostationary orbit on April 6, 2023. TEMPO measurements join an international satellite constellation of observations that will track pollution around the globe. The instrument measures sunlight reflected off Earth’s surface and solar energy scattered by clouds and the atmosphere. Gases in the atmosphere absorb sunlight at particular wavelengths, and the measured color spectra is used to determine the concentrations of several gases in the air, including nitrogen dioxide.

TEMPO is the first space-based instrument to monitor major air pollutants hourly and at high spatial resolution of 4 square miles. Observations of nitrogen dioxide concentration at this temporal and spatial detail will enable scientists to study rush hour pollution and the movement of pollution from forest fires. It can also help measure nitrogen dioxide released when the application of fertilizer on farms is followed by rainfall.

TEMPO data will help scientists evaluate the health impacts of pollutants and aid in the creation of air pollution maps at the neighborhood scale, improving understanding of disparities in air quality within a community. NASA will share the data with other agencies that monitor and forecast air quality, such as the Environmental Protection Agency (EPA) and the National Oceanic and Atmospheric Administration (NOAA).

Scientists at the University of Wisconsin’s Space Science and Engineering Center are members of NASA’s TEMPO science team and will monitor the presence of air pollutants over North America to help improve air quality forecasts.

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. Send them your questions at stevea@ssec.wisc.edu or jemarti1@wisc.edu.

Category: Meteorology, Weather Dangers

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