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  2. Cyclones Gulab and Shaheen - Wikipedia

    en.wikipedia.org/wiki/Cyclones_Gulab_and_Shaheen

    [89] 52 mph (84 km/h) winds were recorded on Suwaiq on October 3 and 36 mph (58 km/h) sustained winds and gusts up to 51 mph (82 km/h) were reported on Muscat International Airport at that day. [95] In total, at least 14 [6] people died in Oman. Many towns and cities saw their average annual rainfall or more in just one day or less.

  3. Open ocean convection - Wikipedia

    en.wikipedia.org/wiki/Open_ocean_convection

    Open ocean convection is a process in which the mesoscale ocean circulation and large, strong winds mix layers of water at different depths. Fresher water lying over the saltier or warmer over the colder leads to the stratification of water, or its separation into layers. Strong winds cause evaporation, so the ocean surface cools, weakening the ...

  4. Atmospheric thermodynamics - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_thermodynamics

    Atmospheric thermodynamics is the study of heat-to-work transformations (and their reverse) that take place in the Earth's atmosphere and manifest as weather or climate. . Atmospheric thermodynamics use the laws of classical thermodynamics, to describe and explain such phenomena as the properties of moist air, the formation of clouds, atmospheric convection, boundary layer meteorology, and ...

  5. Downwelling - Wikipedia

    en.wikipedia.org/wiki/Downwelling

    Buoyancy-forced downwelling, often termed convection, is the deepening of a water parcel due to a change in the density of that parcel.Density changes in the surface ocean are primarily the result of evaporation, precipitation, heating, cooling, or the introduction and mixing of an alternate water or salinity source, such as river input or brine rejection.

  6. Atmospheric convection - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_convection

    Although, the temporal resolution of forecast model soundings is greater than the direct measurements, where the former can have plots for intervals of up to every 3 hours, and the latter as having only 2 per day (although when a convective event is expected a special sounding might be taken outside of the normal schedule of 00Z and then 12Z ...

  7. Madden–Julian oscillation - Wikipedia

    en.wikipedia.org/wiki/Madden–Julian_oscillation

    Enhanced surface (upper level) westerly winds occur near the west (east) side of the active convection. [5] Ocean currents, up to 100 metres (330 ft) in depth from the ocean surface, follow in phase with the east-wind component of the surface winds. In advance, or to the east, of the MJO enhanced activity, winds aloft are westerly.

  8. Hurricane dynamics and cloud microphysics - Wikipedia

    en.wikipedia.org/wiki/Hurricane_dynamics_and...

    They found high concentrations of small and middle sized drops regardless if larger drops were present. The total number of droplets was between 600 and 1000 m −3, the liquid water content was around 1 g m −3, and a rain rate of approximately 20 mm per hour. The droplets had a mean mass diameter of ~1.6 mm and the maximum diameter recorded ...

  9. Geophysical fluid dynamics - Wikipedia

    en.wikipedia.org/wiki/Geophysical_fluid_dynamics

    [2]: 171 Convection in the Earth's outer core drives the geodynamo that is the source of the Earth's magnetic field. [3]: Chapter 8 In the ocean, convection can be thermal (driven by heat), haline (where the buoyancy is due to differences in salinity), or thermohaline, a combination of the two. [4]

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