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Category Archives: Meteorology
What is a mesoscale convective complex?
Ordinary thunderstorms are a few miles in diameter and exist for less than an hour. The life cycle of an ordinary thunderstorm contains three stages: cumulus, mature and dissipating.
The cumulus stage is the initial stage of a thunderstorm as warm moist air near the ground rises. The mature stage of an ordinary thunderstorm begins when precipitation starts to fall from the cloud. During the mature stage, the thunderstorm produces the most lightning, rain, and can produce even small hail. The dissipating stage of a thunderstorm occurs when the updraft, which provides the required moisture for cloud development, begins to weaken and collapse. During this stage, the downdraft dominates the updraft and the storm begins to disappear. Continue reading
What is a landspout?
According to the American Meteorology Society’s glossary, a landspout is a colloquial name for a small tornado whose vorticity (a vector that measures local rotation in a fluid flow) originates in the boundary layer and has a parent cloud in its growth stage. Landspouts occur when colliding winds at the surface begin to make a vortex and then a developing thunderstorm passes overhead. The updrafts from that thunderstorm draw the rotating vortex upward and give it a tornado-like appearance. While relatively weak compared to traditional tornadoes, landspouts can be strong enough to cause damage and warrant caution.
The term “landspout” was coined by atmospheric scientists in the 1980s to describe a type of vortex associated with thunderstorms that do not possess a strong mid-level mesocyclone. A mesocyclone is a cyclonically rotating vortex, around 2–10 km in diameter, in a convective storm. Strong tornadoes form in mesocyclones.
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Has the EPA rolled back regulations on greenhouse gas emissions?
On June 11, Environmental Protection Agency Administrator Lee Zeldin proposed repealing all “greenhouse gas” (their quotes, not ours) emission standards for the power sector under Section 111 of the Clean Air Act.
This proposal is based upon the false assertion that “emissions from fossil fuel-fired power plants do not contribute significantly to dangerous air pollution.” This assertion flies in the face of centuries of evolving understanding of the influence that carbon dioxide, the primary by-product of such combustion, has on the radiation balance of Earth’s atmosphere. Continue reading
Category: Climate, Meteorology
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Did weather forecasting play a role in D-Day?
Last Friday was the 81st anniversary of the Allied invasion of Europe that began with the landings on the beaches at Normandy. The combined land, air, and sea assault of June 6, 1944 remains the largest such event in history. The success of the invasion was extraordinarily dependent of weather conditions. More than three months before the invasion, a combined British and American forecasting team began rigorous forecast exercises designed to iron out the physical and logistical kinks of such a coordinated effort. As June drew near, the nature of this collaboration was still problematic as the two groups employed vastly different methods in fashioning the requisite 3-5 days forecasts – at the time, absolutely primitive in the underlying science as compared to what is possible at such ranges today. The British were attempting to make such forecasts based upon the understanding of atmospheric dynamics that had grown substantially during the war. The Americans were employing a method based on a statistically- based search through old weather data for historical analogues that could be used to guide the forecast. Continue reading
Category: History, Meteorology, Severe Weather
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What causes tornados and do they have a lifecycle?
A tornado is a powerful column of winds that rotate around a center of low pressure. The winds inside a tornado spiral inward and upward, often exceeding speeds of 300 mph. We don’t know if a particular storm will produce a tornado but we do know the necessary conditions needed for tornado formation.
The required conditions for a thunderstorm to produce a tornado are warm humid air near the surface with cold dry air above. These conditions make the atmosphere very unstable, in the sense that once air near the ground is forced upward, it moves upward quickly and forms a storm. Severe thunderstorm conditions also include a layer of hot dry air between the warm humid air near the ground and the cool dry air aloft. This hot layer acts as a lid that allows the sun to further heat the warm humid air, making the atmosphere even more unstable. Continue reading
Category: Meteorology, Phenomena, Severe Weather
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