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What is a haboob?
A haboob is dust storm that can be several miles long, several thousand feet high, and can travel hundreds of miles. Haboobs are caused when an intense column of sinking air in a thunderstorm hits the ground and lofts soil particles into the air. These downdrafts, referred to as a microburst, can hit the ground at 50-80 mph and then spread in all directions. The resulting winds stir up dust and dirt from large arid areas which then get blown along in front of the approaching thunderstorm. The lofted particles can reach heights of 5000 ft and can extend up to 100 miles wide.
The name “haboob” is derived from the Arabian word ‘hab’, meaning ‘to blow,’ and was originally the name for a dust storm or sandstorm in the northern part of Sudan. Continue reading
What is the longest lightning bolt?
Lightning is a huge electrical discharge, or spark, that results from vigorous motions in thunderstorms.
Storms are composed of ice crystals and liquid water droplets. Winds inside the storm cause particles to rub against one another, causing electrons to be stripped off, making the particles either negatively or positively charged. The charges get grouped in the cloud, often negatively charged near the bottom of the cloud and positively charged up high. This is an electric field, and because air is a good insulator, the electric fields become incredibly strong. Eventually a lightning bolt happens, and the flow of electrons neutralizes the electric field. Continue reading
Category: Meteorology, Phenomena, Severe Weather
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Has it been unusually rainy so far this summer?
As we head into the last week of August, it is of interest to review aspects of this summer’s precipitation in Madison.
First of all, every one of the three traditional summer months has been wetter than normal with June, July, and August (through Aug 20) coming in at 0.26”, 1.55” and 2.02” above normal for a total surplus of nearly 4”. Continue reading
How does this summer dew point temperature compare with previous years?
The dew point temperature is the temperature to which the air must be cooled, at constant pressure, to get dew to form. As the grass and other objects near the ground cool and reach the dew point temperature, some of the water vapor in the atmosphere will condense into liquid water on the objects. While the dew point temperature is a temperature, it is also a measure of the humidity of the air. The higher the dew point temperature, the greater the amount of water vapor in the air.
To know how close the air is to saturation, we need to know the dew point and the air temperature. The closer the dew point is to the air temperature, the closer the air is to saturation. When the dew point equals the air temperature, the air is saturated, so the dew point temperature cannot be greater than the air temperature. Continue reading
Category: Climate, Meteorology, Seasons
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Does the Dept. of Energy’s latest climate report ring true?
The Trump Administration continues to double down on its naked denialism of the nature of, and threat posed by, human-induced changes to the global climate.
Late last month the Department of Energy released a 151-page report entitled “A Critical Review of Impacts of Greenhouse Gas Emissions on the U.S. Climate.” This report was commissioned this spring and work on it was conducted from early April until late May with a May 28 deadline to deliver a draft. It was authored by 5 scientists who share a deep skepticism regarding the broad scientific consensus that industrialization has played a leading role in altering the chemical composition of our atmosphere in such a way as to encourage global warming, ocean acidification, increased wildfire threat and an increased risk of high impact weather systems in all seasons. Continue reading
