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  2. Coriolis force - Wikipedia

    en.wikipedia.org/wiki/Coriolis_force

    The stronger the force from the Coriolis effect, the faster the wind spins and picks up additional energy, increasing the strength of the hurricane. [ 37 ] [ better source needed ] Air within high-pressure systems rotates in a direction such that the Coriolis force is directed radially inwards, and nearly balanced by the outwardly radial ...

  3. Tropical cyclogenesis - Wikipedia

    en.wikipedia.org/wiki/Tropical_cyclogenesis

    Depth of 26 °C isotherm on October 1, 2006. There are six main requirements for tropical cyclogenesis: sufficiently warm sea surface temperatures, atmospheric instability, high humidity in the lower to middle levels of the troposphere, enough Coriolis force to sustain a low pressure center, a preexisting low level focus or disturbance, and low vertical wind shear. [3]

  4. Cyclogenesis - Wikipedia

    en.wikipedia.org/wiki/Cyclogenesis

    Cyclogenesis is an umbrella term for at least three different processes, all of which result in the development of some sort of cyclone, and at any size from the microscale to the synoptic scale. Tropical cyclones form due to latent heat driven by significant thunderstorm activity, developing a warm core.

  5. Mesoscale meteorology - Wikipedia

    en.wikipedia.org/wiki/Mesoscale_meteorology

    A meso-beta scale vortex. Mesoscale meteorology is the study of weather systems and processes at scales smaller than synoptic-scale systems but larger than microscale and storm-scale. Horizontal dimensions generally range from around 5 kilometres (3 mi) to several hundred kilometres. Examples of mesoscale weather systems are sea breezes, squall ...

  6. Focus on research: What meteorologists look for as they hunt ...

    www.aol.com/news/focus-research-meteorologists...

    The Coriolis force is caused by the Earth’s rotation, which makes moving air turn and swirl. Warm sea surface temperatures: The sea surface temperature must be at least 26.5 degrees Celsius ...

  7. Intertropical Convergence Zone - Wikipedia

    en.wikipedia.org/wiki/Intertropical_Convergence_Zone

    The Intertropical Convergence Zone (ITCZ / ɪtʃ / ITCH, or ICZ), [ 1 ] known by sailors as the doldrums[ 2 ] or the calms because of its monotonous windless weather, is the area where the northeast and the southeast trade winds converge. It encircles Earth near the thermal equator though its specific position varies seasonally.

  8. Extratropical cyclone - Wikipedia

    en.wikipedia.org/wiki/Extratropical_cyclone

    A hurricane-force extratropical cyclone in the north Atlantic in January 2016 with a distinct eye-like feature, caused by a warm seclusion. This system would later undergo tropical cyclogenesis and become Hurricane Alex. There are two models of cyclone development and life cycles in common use: the Norwegian model and the Shapiro–Keyser model ...

  9. See what spaghetti models show for Hurricane Helene's path - AOL

    www.aol.com/see-spaghetti-models-show-hurricane...

    Spaghetti models do not show Hurricane Helene veering off into the Treasure Coast, but the tri-county area should prepare for tropical storm conditions that can include wind speeds from 39-73 mph.