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Kona storm

Kona storm 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 Kona storm rather than just read about it. In short: Kona storms (also called Kona lows) are a type of seasonal cyclone in the Hawaiian Islands, usually formed in the winter from winds coming from the westerly "kona" (normally leeward) direction. They are mainly cold core cyclones, which places them in the extratropical cyclone rather than the subtropical cyclone category.

Kona storm — main illustration
Kona storm — illustration

Key takeaways

  • Kona storm 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 Kona storm to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Kona storm from memory before moving on to harder problems.

Reference excerpt

Kona storms (also called Kona lows) are a type of seasonal cyclone in the Hawaiian Islands, usually formed in the winter from winds coming from the westerly "kona" (normally leeward) direction. They are mainly cold core cyclones, which places them in the extratropical cyclone rather than the subtropical cyclone category. Hawaii typically experiences two to three annually, which can affect the state for a week or more. Among their hazards are heavy rain, hailstorms, flash floods and their associated landslides, high elevation snow, high winds which result in large surf and swells, and waterspouts.

Origin of term Kona is a Hawaiian language term (related to similar words in other Polynesian languages) for the western (to southwestern) side of an island. The Kona District for example on the Big Island of Hawaiʻi still uses this name. Although normally dry and leeward, the traditional easterly (to northeasterly) tradewinds slacken and reverse during one of these cyclones.

Character of the cyclones Once termed as subtropical cyclones, a change in the definition of the term during the early 1970s makes categorization of the systems not straightforward. Kona lows are typically cold core, making them extratropical cyclones. However, they generally share the subtropical cyclone characteristic of losing their associated weather fronts with time, since the cyclones tend to retrograde slowly. Otkin and Martin identified three types of kona storms: cold-frontal cyclogenesis cyclones (CFCs), trade wind easterlies, and cold-frontal cyclogenesis/trade wind easterlies cyclones. Of the three, CFC cyclones are the most common. Rainfall in a Kona storm is more pronounced than a cold front storm, and most intense from south to east of the storm and in front of the storm's center. Steady rains may last from several hours to days, with longer lasting storms typically interrupted by intervals of lighter rain and partial clearing. Intense showers may appear on more moderate but steady rain.

Frequency and effects While some winters occur without a single Kona storm, other winters see a high of four or five. Hawaii typically experiences two to three annually between October and April. The cyclone events for Hawaii can be long-lived, affecting the state for a week or more. Kona lows produce a wide range of weather hazards for Hawaii. Among them are heavy rain, hailstorms, flash floods and their associated landslides, high winds which result in large surf and swells, waterspouts, and heavy snows on the higher mountains.

Kona winds Kona winds are associated with cyclones with central pressures below 1,000.0 hectopascals (29.53 inHg) which pass within 500 miles/820 km northwest of the Hawaiian Islands. Strong Kona winds usually last for a day. Considerable damage is caused to boats lying southwest of the islands. On land, trees are uprooted and roofs can be blown off homes. When passing through mountain gaps and over mountains, downsloped winds gust over 100 mph/165 km/h, which causes much of the destruction.

Examples

The most powerful Kona storm in the last fifty years struck the Hawaiian islands between 8 January and 11 January 1980. The low pressure primarily responsible for the severe conditions had a barometric pressure of 975mb on January 8, while passing north of the state, one of the lowest pressure readings ever recorded in Hawaiian waters as a result of an extratropical storm. The storm caused severe weather across the entire state, forcing the closure of all airports. Rainfall from the storm was extremely heavy, surpassing twenty inches in many locations, particularly on the Big Island and Maui. High surf from the storm caused extensive damage, particularly along the Kona coast of the Big Island, where the towns of Kailua-Kona and Puako received extensive damage. Winds from the storm averaged around 40-50 mph on the open ocean, but varied tremendously on land due to unique geographic features. Some areas experienced wind gusts well over hurricane force, including a low altitude gust of 106 mph (171 km/h) on Lahaina Roads, Maui. Haiku, on the windward coast of Maui, experienced a wind gust of 75 mph (121 km/h). On the high mountain summits of the Big Island and Maui, winds of over 110 mph (180 km/h) were recorded. Damage from the storm was estimated at between $25 and 35 million (in 1980 dollars). In December 2008, lightning strikes from a Kona storm caused the entire power grid of the island of Oahu to black out, while then President-elect, Barack Obama was visiting. In December 2010, a Kona storm became fully subtropical and eventually became Tropical Storm Omeka.

In popular culture The fourth episode of the sixth season of Magnum, P.I. is entitled "The Kona Winds."

References

Illustrations

Kona storm: Subtropical Storm Omeka on December 19, 2010, originally a Kona storm
Subtropical Storm Omeka on December 19, 2010, originally a Kona storm
Kona storm: A kona storm on November 4, 1995
A kona storm on November 4, 1995

Worked examples

Example 1 — a first encounter with Kona storm

Start with the simplest possible case. Write down what Kona storm 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 Kona storm 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 Kona storm 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 Kona storm

In research
Kona storm 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 Kona storm 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
Kona storm is common in secondary-school and first-year university syllabi. It links to neighbouring topics Extratropical cyclones, Storm, Subtropical cyclones, so understanding it makes those chapters shorter.
In everyday life
Look for Kona storm 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 Kona storm in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Kona storm 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 Kona storm out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Kona storm in simple terms?

Kona storms (also called Kona lows) are a type of seasonal cyclone in the Hawaiian Islands, usually formed in the winter from winds coming from the westerly "kona" (normally leeward) direction. They are mainly cold core cyclones, which places them in the extratropical cyclone rather than the subtro…

Why does Kona storm 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 Kona storm?

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 Kona storm.

Tags

  • Extratropical cyclones
  • Storm
  • Subtropical cyclones
  • Types of cyclone
  • Weather events in Hawaii

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