Why don’t trees freeze and burst in the winter like cold pipes?

When liquid water freezes, it expands as the water molecules spread out to form a solid crystalline lattice. If the freezing water is contained in a closed vessel, such as a metal pipe, it can press hard on the sides as it expands, causing the container to burst.

Frost cracks are longitudinal openings that can run the entire length of the trunk, often extend deep into the wood, and permanently damage a tree. In wintertime, the tree may even look like it’s splitting in half! Then warmer weather comes, and the crack seems to close, repeating this process annually. Over time, frost cracks may even develop a raised area where callus tissue develops in an attempt to close over the wound, only to reopen again next winter. (Photo credit: Wisconsin Dept of Natural Resources)

Trees contain water that is transported throughout the tree by the phloem and xylem, which we can think of as pipes.

Trees are cold hardy because of many factors. In preparation for winter, many trees reduce the amount of water held in their tissue. They usually enter a dormant state to survive cold winters. Some trees, such as maple trees, produce more sugar. When this sugar dissolves in the water, it lowers the freezing point of the fluid. Unlike plumbing pipes, tree tissue is somewhat flexible; as water in the channels freezes and expands, the tree’s tissue can stretch somewhat.

Trees can suffer damage during periods of cold winter nights followed by warm sunny days. The bark alternately contracts with freezing temperatures and expands on warm days. The alternating freezing and thawing temperatures can result in a vertical crack called a “frost crack.” This often happens during late winter or early spring. The formation of a frost crack can be accompanied by a loud noise, like a gunshot sound. But the trees don’t “explode” in the in subzero weather.

Dangerous winter weather for trees are storms that lead to heavy snow and ice accumulating on the trees. The weight of frozen precipitation can put enormous stress on tree limbs, causing them to break and fall.

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

Category: Climate, Seasons

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Will the recent the groundhog predictions come true?

Punxsutawney Phil saw his shadow, which means there will be six more weeks of winter. On the other hand, Jimmy the Groundhog in downtown Sun Prairie did not see his shadow at sunrise during the 78th annual Groundhog Day Prognostication, which per tradition means we are due for an early spring. Which to believe?

Groundhog Day stats (Image credit: NWS LaCrosse)

We don’t put stock in either.

Humans have long needed weather forecasts. Farmers and sailors particularly needed to know if storms were approaching. Over time, various folklore forecasts, often in the form of short rhymes, were devised and passed down through the generations. The forecast made on Groundhog Day is an example of a folklore weather forecast. Although memorable, the folklore forecasts are of uneven quality — some good, others bad.

The roots of Groundhog Day go back to the sixth century. Feb. 2 is 40 days after Christmas and is known as Candlemas. On this day, candles that are used for the rest of the year are blessed. This is also about the midpoint of winter, in astronomical not meteorological terms. If the day is bright and clear, the groundhog “sees” his shadow and we have more winter.

Of course, after Feb. 2, there are only 47 days left of astronomical winter — which ends on or about March 21, so the forecast accuracy should be more than luck. The predictions made by Punxsutawney Phil with this folk forecast are correct only about 40% of the time, and Jimmy the Groundhog is about 60% accurate — both vastly inferior to what is delivered by modern science.

Of course, the weather conditions on a single day at a single location tell us very little about the weather for the rest of the winter season. But right or wrong, they are fun community celebrations, as well as an entertaining movie.

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

Category: History, Seasons

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Why does the morning low temperature sometimes occur after sunrise?

Those who keep a particularly vigilant eye on the weather might have noticed that on certain mornings, in all seasons, the lowest temperature is often recorded just after sunrise.

Sunrise in winter. (Photo credit: Steve Ackerman)

One of us had a morning paper route as a boy and was puzzled for years about this seemingly counterintuitive phenomenon. How could the temperature continue to fall for the few minutes after sunrise on a cold winter morning?

The answer lies in the fact that Earth and the sun radiate different kinds of energy and one needs to consider the budget of this energy to make sense of this recurring observation. But first a bit about measuring temperature. Atmospheric temperature is measured using thermometers placed in shaded enclosures at a height of about 5 to 6 feet above the ground.

On a clear, calm winter night, Earth’s surface radiates infrared energy upward towards space. With the sun already down, there is no shortwave solar radiation (and only a very little infrared energy from the overlying atmosphere) directed downward toward the surface. Consequently, with each passing second, the surface emits more energy than it receives and the surface temperature drops.

This continues all through the night with the accumulated loss of infrared energy from the surface accounting for the continued decrease in the surface temperature. When the sun finally rises above the horizon and spreads the first faint rays of solar energy across the surface, there is finally some incoming radiation. However, for several minutes the meager amount of incoming radiation is not sufficient to counter the amount of infrared energy still being emitted from the surface. As a result, the surface temperature continues to drop even in the face of the newly risen sun.

Steve Ackerman and Jonathan Martin, professors in the UW-Madison department of atmospheric and oceanic sciences, are guests on WHA radio (970 AM) at noon the last Monday of each month. send them your questions at stevea@ssec.wisc.edu or jemarti1@wisc. edu.

Category: Meteorology, Phenomena

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Why are viruses more common in Winter?

Colds and the flu are caused by viruses, not by cold wintery conditions. Viruses such as rhinoviruses, which cause the common cold, and influenza viruses spread from person to person through respiratory droplets or physical contact, regardless of the temperature outside.

However, weather and climate do play a role in why colds and the flu are more common in winter though. The colder temperatures associated with winter affect how viruses behave in the environment. Winter’s colder temperatures and lower humidity help viruses survive longer and spread more easily. Research studies show that many respiratory viruses survive longer and remain infectious for extended periods of time in cold, dry environmental conditions.

This 2009 photograph captured a sneeze in progress, revealing the plume of salivary droplets as they are expelled in a large cone-shaped array from this man’s open mouth… (Photo credit: Wikipedia)

Dry air also causes tiny droplets released when people breathe, talk, cough, or sneeze to evaporate quickly. These droplets evaporate quickly, creating smaller particles that stay suspended in the air longer and travel farther, increasing the chance that others will inhale them.

Winter’s low humidity can dry the lining of one’s nose and throat. This reduces the effectiveness of mucus, which normally traps viruses and helps move them out of the airways.

In cold weather, social events tend to be indoors, bringing us in close contact with others.  This increases the chance of the spread of a virus. Preventive measures such as vaccinations, good hygiene practices, and wearing masks in crowds help to reduce the risk of viral infections. Improving indoor ventilation and maintaining adequate humidity during winter can also reduce transmission risk. Cold weather can be challenging for people with existing respiratory conditions such as asthma.

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

Category: History, Seasons

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Why is Wisconsin winter weather so cloudy and grey?

Climatologically, the winter months are the cloudiest time of the year in Wisconsin. Wisconsin’s average monthly cloud cover for December, January, and February for the years 2006 to 2024 was 65.3%, 61.1% and 50.5% respectively. There are a few factors that contribute to this climate observation.

Thanks to Amanda Latham and Ed Hopkins of the WI State Climate Office for providing the analysis. (Image credit: Iowa Environmental Mesonet)

Wisconsin sits in a latitude band where synoptic scale storm systems often pass nearby. This scale is associated with large weather patterns like mid-latitude cyclones and anticyclones. During the winter, the mid-latitude storm tracks tend to be along the polar front and the upper tropospheric jet stream. These winter storms have large stratiform cloud shields that move across the Midwest, producing more persistent cloudy conditions. Even when storm centers miss the state, these cloud shields can linger for days afterward.

As winter arrives, we experience fewer hours of sunlight and the sun is lower on the horizon. This reduces solar heating at the ground and adds a factor that leads to increased cloudiness. The absence of solar warmth causes a cooling effect on Earth’s surface and affects the lower atmosphere.

However, with the low angle of the sun, the surface doesn’t warm as much. This can lead to cold air staying at the surface, with a warmer layer of air developing above; this is called a temperature inversion. In the layer between the warm and cold air, moisture gets stuck and clouds persist there. If the sun were able to warm the air at the surface, it would dry out easier, thus allowing air to rise and skies to clear.

Much winter cloud cover in Wisconsin is low-level stratus. These clouds form in cold, stable air and can exist for days without producing much snow or rain, just gray skies.

But when clear days do happen in Wisconsin’s winter, they’re often very crisp and bright.

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

Category: Climate, Meteorology, Seasons

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