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  2. Pressure-wind relationship calculations for tropical cyclones

    en.wikipedia.org/wiki/Pressure-wind_relationship...

    The interchangeability of pressure and wind allows for the two to be used to give equivalencies for the public. [3] Pressure-wind relations can be used when information is incomplete, forcing forecasters to rely on the Dvorak Technique. [8] Some storms may have particularly high or low pressures that do not match with their wind speed.

  3. Low-pressure area - Wikipedia

    en.wikipedia.org/wiki/Low-pressure_area

    In meteorology, a low-pressure area, low area or low is a region where the atmospheric pressure is lower than that of surrounding locations. It is the opposite of a high-pressure area . Low-pressure areas are commonly associated with inclement weather (such as cloudy, windy, with possible rain or storms), [ 1 ] while high-pressure areas are ...

  4. Extratropical cyclone - Wikipedia

    en.wikipedia.org/wiki/Extratropical_cyclone

    The central pressure of the cyclone will lower with increasing maturity, while outside of the cyclone, the sea-level pressure is about average. In most extratropical cyclones, the part of the cold front ahead of the cyclone will develop into a warm front, giving the frontal zone (as drawn on surface weather maps) a wave-like shape. Due to their ...

  5. 30.27 in Pressure. 2 UV Index. 5:53PM Sunset. 6 mph F 10 km/h C Wind. 28 ... Rare cyclone weakens to a tropical low weather system as it approaches the Australian east coast.

  6. Tropical cyclone intensity scales - Wikipedia

    en.wikipedia.org/wiki/Tropical_cyclone_intensity...

    If a tropical cyclone intensify further and reaches wind speeds of 90 knots (170 km/h; 100 mph), it will be classified as an intense tropical cyclone. A very intense tropical cyclone is the highest category on the South-West Indian Ocean Tropical Cyclone scale, and has winds of over 115 knots (213 km/h; 132 mph). [24] [25]

  7. Cold-core low - Wikipedia

    en.wikipedia.org/wiki/Cold-core_low

    A cold-core low, also known as an upper level low or cold-core cyclone, is a cyclone aloft which has an associated cold pool of air residing at high altitude within the Earth's troposphere, without a frontal structure. It is a low pressure system that strengthens with height in accordance with the thermal wind relationship.

  8. List of the most intense tropical cyclones - Wikipedia

    en.wikipedia.org/wiki/List_of_the_most_intense...

    The most intense tropical cyclone in the North Indian Ocean by both sustained winds and central pressure was the 1999 Odisha cyclone, with 3-minute sustained winds of 260 km/h (160 mph) and a minimum pressure of 912 hPa (26.93 inHg). Storms with an intensity of 950 hPa (28.05 inHg) or less are listed.

  9. Portal:Tropical cyclones - Wikipedia

    en.wikipedia.org/wiki/Portal:Tropical_cyclones

    It was the only March Atlantic tropical cyclone on record. 1997 - Cyclone Gavin reached peak intensity with 1-minute sustained winds of 220 km/h (140 mph) and a pressure of 925 mbar as it affected Vanuatu and Fiji, killing 18 people and damaging US$23.7 million. 2008 - Cyclone Jokwe (pictured) struck northern Mozambique, killing 16 people.

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