How do citrus farmers battle the cold?

Last week was one of the coldest of the season in the southeast United States. Though not as bad as prior cold air outbreaks in late January or early February, such events have been known to present a substantial threat to the citrus industry in Florida. The problem is that when the temperature gets below freezing, the fruit itself can freeze rendering it substantially less valuable to the market.

One of the most ingenious tricks citrus farmers can use to combat this takes advantage of the fact that phase changes of water involve substantial amounts of energy known as latent heats. Everyone knows that ice only melts into liquid water after some energy has been supplied to the ice — the latent heat of melting. In the process, the environment that surrounds the original ice becomes colder since it has been forced to spend some energy to do the melting.

A classic, kitchen-ready example involves placing ice cubes in a glass of water. Two things happen — the ice melts and the original liquid water cools. The water cools because it has spent some of its energy in accomplishing the phase change. The interesting thing is that if liquid water is converted to solid ice, the same amount of energy is released to the environment — this time it is called the latent heat of fusion.

So, when a freeze is forecast for a citrus farm, the farmers often spray the trees with water. When the temperature drops, this water freezes and releases heat to its environment, some of which is the still-ripening fruit. This heat is enough to preserve the fruit inside from freezing. So, paradoxically, causing ice to form on the fruit saves it from freezing.

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How are climates classified?

There are a few ways to classify climates. The plant hardiness zones often published with seed packages are one way to group climates. That approach is based on minimum wintertime temperatures but is limited in its usefulness because a good climate map should include reference to more than one weather variable.

Between 1918 and 1936 Vladimir Köppen (pronounced KEPP-in) devised the climate classification scheme that is most widely used today. He used vegetation and temperature as natural indications of the climate of a region. Climate scientists have made improvements to the original Köppen scheme, most recently in 2007; it is now called the Köppen-Geiger map.

The current Köppen-Geiger classification scheme has five main groups, each designated with a letter: Tropical Moist (A), Dry (B), Moist with Mild Winters (C), Moist with Severe Winters (D) and Polar (E).

Some groups are described by two- and three-letter designations. The second letter usually refers to whether and when a dry season occurs, and the third letter denotes differences in temperatures. The dominant climate classification over land is arid B (about 30 percent) followed by cold D (about 25 percent) and tropical A (19 percent). The moist and mild C climate only occupies about 13 percent, about the same as polar E zones. Following this major classification, denoted by a capital letter, is a second letter that is not capitalized that usually refers to whether and when a dry season occurs.

Wisconsin is a “Df” climate type. The “D” part of this classification means the climate includes variable weather patterns with a large variation in seasonal temperatures. The average temperature of the coldest month is less than 32 degrees F, and the warmest month has an average temperature exceeding 50 degrees. These climate types usually have snow on the ground for extended periods. The “f” designation indicates that there is no dry season.

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Why has it snowed nearly every day recently?

Lately our fair city has been the recipient of continuous dustings of light snow evoking images of a Brueghel painting. In fact, Thursday was the ninth consecutive day with measurable snow, tying a record set only one other time (Feb. 23-March 3, 2007) in Madison’s history.

One might wonder if it is unusual to have such a parade of frequent light snowfalls. As it turns out, the large-scale setup that has brought our current snow streak is quite normal for the winter around here. Nearly every winter the western Great Lakes states experience extended periods in which the airflow in the middle part of the troposphere (about two to three miles above the surface) is from the northwest, with origins in arctic Canada.

Embedded within this northwesterly flow are barely perceptible vortices that are carried rapidly southeast. Such vortices are enhanced by passage over the Canadian Rockies in Alberta. These mid-level vortices are capable of creating rising air which, in turn, produces clouds and precipitation.

Since the air that is forced to rise is cold and quite dry, there is usually not sufficient water available to these so-called Alberta Clippers to create big snowfalls — just lots of small ones. It has long been our sense that the total seasonal snowfall in Madison (approximately 40 inches each year) is largely the result of many small snowfalls and very few more substantial ones. This is consistent with the prevalence of cold northwesterly flow that characterizes our winters.

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What are ice pellets?

Ice pellets are a form of precipitation. They are small, translucent or clear balls of ice. Ice pellets are rain drops that have frozen before they hit the ground. When they hit the ground, they bounce. Ice pellets are also called sleet and can be accompanied by freezing rain.

In winter, precipitation usually begins falling out of a cloud as ice particles. If the temperature underneath a cloud stays below freezing all the way to the ground, the ice crystals never melt and snow falls. If the temperature is above freezing below the cloud bottom to the ground, the frozen particles melt into liquid droplets that reach the surface and this is called rain.

Ice storms occur when precipitation particles melt and then fall through a layer of cold air near the ground. Sleet results when the layer of subfreezing air at the surface extends upward far enough so that raindrop freezes into a little ball of ice. Freezing rain forms when a very shallow layer of cold air at the surface causes freshly melted raindrops to freeze on contact with exposed objects on the ground, whose temperature is below freezing.

Another type of precipitation is graupel. Ice crystals may encounter small drops of water whose temperatures are below freezing.  These supercooled liquid droplets freeze when they come into contact with the snow crystal. When this process continues so that the shape of the original snow crystal is no longer identifiable, the resulting ice particle is called graupel.  Graupel is brittle and will fall apart when it strikes the ground.

On Sunday afternoon, Jan. 27, Madison experienced rain, freezing rain, sleet and snowfall all in one day.

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How cold has this winter been, historically?

Wednesday is the 62nd anniversary of the coldest day ever in Madison — Jan. 30, 1951 — when the temperature dropped to minus 37 F.

As we described in a column a couple of years ago, to get the air that desperately cold in Madison a healthy snow cover is necessary. This January, we had a warm spell near mid-month that effectively melted most of the snow remaining from our December snowstorm. Thus, even though last week’s cold was the worst of the season thus far, it was a lot less cold than it might have been had it occurred while we had a deep, fresh snow cover.

Looking ahead for the rest of the season, we are nearing winter’s coldest point, climatologically (approximately Feb. 1), and until or unless there is fresh snow on the ground we are likely to escape the kind of cold that keeps the temperature below zero throughout the day. In fact, in the last five years there have been only two days on which the daily high temperature has been below zero — Jan. 15, 2009, and Jan. 19, 2008 — both with a high of minus 2 F in Madison.

In a related item of local interest pertaining to the severity of the winter thus far, state climatologist Dr. John Young officially declared two weeks ago that Lake Mendota froze over on Jan. 14, the third-latest date in an unbroken 159 years of observation.

This late date was a combination of the very warm summer and relatively warm autumn that allowed anomalous amounts of heat to be stored in the lake as winter approached. Then, given the lack of truly cold air in our area until recently, it has taken longer for the lake to give up its excess heat. These factors led to the very late freezing date this year.

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