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Project NIMROD

Project NIMROD is a earth science topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Project NIMROD rather than just read about it. In short: Project NIMROD (Northern Illinois Meteorological Research On Downburst) was a meteorological field study of severe thunderstorms and their damaging winds conducted by the National Center for Atmospheric Research (NCAR). It took place in the Greater Chicago area from May 15 to June 30, 1978.

Project NIMROD — main illustration
Project NIMROD — illustration

Key takeaways

  • Project NIMROD belongs to earth science; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Project NIMROD to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Project NIMROD from memory before moving on to harder problems.

Reference excerpt

Project NIMROD (Northern Illinois Meteorological Research On Downburst) was a meteorological field study of severe thunderstorms and their damaging winds conducted by the National Center for Atmospheric Research (NCAR). It took place in the Greater Chicago area from May 15 to June 30, 1978. Data collected was from single cell thunderstorms as well as mesoscale convective systems, such as bow echoes. Using Doppler weather radars and damage clues on the ground, the team studied mesocyclones, downbursts and gust fronts. NIMROD was the first time that microbursts, very localized strong downdrafts under thunderstorms, were detected; this helped improve airport and public safety by the development of systems like the Terminal Doppler Weather Radar and the Low-level windshear alert system.

Description The project was set up by Ted Fujita and Ramesh Srivastava from the University of Chicago, with research assistants from the university Roger Wakimoto and Gregory S. Forbes helping, along with researcher Jim Wilson from NCAR. The network was composed of 3 Doppler weather radars (2 C-band radars, 1 CP-3 and 1 CP-4, along with a CHILL S-band radar) disposed in a triangular baseline approximately 37 mi (60 km) from one another, and 27 Portable Automated Mesonets (PAMs) from NCAR forming a mesonet in and around the Chicago area. O'Hare International Airport was intentionally part of the location used for the project, so that the low-level winds of the area could be measured near a large airport. The location was also chosen to include corn crops, as a way to measure wind, and the study was performed in late spring so the corn would be in its growing season. The nominal height of the PAMs were 13 ft (4 m); they were placed in both suburban areas and fields. Operations were made from the site of the CP-3 radar, where roughly 200 rawinsondes every 30–60 minutes upon request. Field offices of the National Weather Service informed the project on "significant" tornadoes and downbursts, and helped complete damage surveys.

Aim and results

Not many studies had been conducted on downdrafts from thunderstorms before this one, and the extension of their effects was not well known. Fujita suspected that localized downdrafts, later called microbursts, were responsible for damage on the ground and were involved in some airplane crashes, such as the June 24, 1975 Eastern Air Lines Flight 66, which crashed during landing at New York's John F. Kennedy International Airport, killing 113 and injuring the other 11 on board. Fujita had hypothesized during the inquiry that the cause was a sudden burst of air coming down from a thunderstorm from his previous study of the effects of the damage caused by the atomic bomb dropped on Nagasaki in August 1945, and some unexplained damage during the 1974 Super Outbreak of tornadoes. However, there was strong resistance from the meteorological community. He convinced the National Science Foundation and NCAR to fund projects to study thunderstorm downdrafts. NIMROD was the first large scale experiment to study this phenomenon. and it was the first time that Fujita had used Doppler radar data; he had no previous experience in the interpretation of their data, but quickly became comfortable with them. Shortly after the start of the field program, the first recorded microburst on Doppler weather radar was viewed on the CP-3 radar at Yorkville, Illinois, on May 29, 1978. On the first scan of a thunderstorm, the Doppler velocity display showed a doublet of inbound-outbound velocities which was followed by observation of a gust front. Data obtained during the whole project permitted to describe the three-dimensional motion of the air in thunderstorms and their structure as different types of systems, such as single cells, multi-cells, and bow echoes, but including others as well.

Legacy This first experiment has been followed by numerous others since 1978. Some of these include the JAWS (Joint Airport and Weather Studies) in 1982, the MIST (Microburst and Severe Thunderstorm Experiment) in 1986 led by Fujita, and the VORTEX projects. All of them have led to a better understanding of severe weather during the summer, leading to better airport and public safety.

References

Bibliography Fujita, T. T. (1978). Manual of downburst identification for project Nimrod (PDF). Satellite and Mesometeorology Research Paper. Vol. 156. Dept. of Geophysical Sciences, University of Chicago. Archived from the original (PDF) on 2017-02-19. Fujita, T. T. (1978). Objective, operation, and results of Project NIMROD. 11th Conf. on Severe Local Storms. Kansas City, MO: Amer. Meteor. Soc. pp. 259–266..

Illustrations

Project NIMROD illustration
Project NIMROD: Bow echoes are associated with different types of severe winds.
Bow echoes are associated with different types of severe winds.

Worked examples

Example 1 — a first encounter with Project NIMROD

Start with the simplest possible case. Write down what Project NIMROD claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In earth science, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Project NIMROD before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Project NIMROD ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Project NIMROD

In research
Project NIMROD appears in earth science research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses Project NIMROD in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
Project NIMROD is common in secondary-school and first-year university syllabi. It links to neighbouring topics Meteorology research and field projects, Severe weather and convection, so understanding it makes those chapters shorter.
In everyday life
Look for Project NIMROD outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.

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How to study Project NIMROD in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Project NIMROD means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain Project NIMROD out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Project NIMROD in simple terms?

Project NIMROD (Northern Illinois Meteorological Research On Downburst) was a meteorological field study of severe thunderstorms and their damaging winds conducted by the National Center for Atmospheric Research (NCAR). It took place in the Greater Chicago area from May 15 to June 30, 1978.

Why does Project NIMROD matter?

Because it connects several earth science ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study Project NIMROD?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on Project NIMROD.

Tags

  • Meteorology research and field projects
  • Severe weather and convection

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