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  2. Marine cloud brightening - Wikipedia

    en.wikipedia.org/wiki/Marine_cloud_brightening

    In the earliest published studies, John Latham and Stephen Salter proposed a fleet of around 1500 unmanned Rotor ships, or Flettner ships, that would spray mist created from seawater into the air. [5] [31] The vessels would spray sea water droplets at a rate of approximately 50 cubic meters per second over a large portion of Earth's ocean ...

  3. CLOUD experiment - Wikipedia

    en.wikipedia.org/wiki/CLOUD_experiment

    The nucleation process of water droplets/ice micro-crystals from water vapor reproduced in the CLOUD experiment and also directly observed in the Earth atmosphere do not only involve ions formation due to cosmic rays but also a range of complex chemical reactions with sulfuric acid, ammonia and organic compounds emitted in the air by human ...

  4. Cloud physics - Wikipedia

    en.wikipedia.org/wiki/Cloud_physics

    the cloud IR emissivity, with values between 0 and 1, with a global average around 0.7; the effective cloud amount, the cloud amount weighted by the cloud IR emissivity, with a global average of 0.5; the cloud (visible) optical depth varies within a range of 4 and 10. the cloud water path for the liquid and solid (ice) phases of the cloud particles

  5. Cloud formation and climate change - Wikipedia

    en.wikipedia.org/wiki/Cloud_formation_and...

    Recent studies also suggest that cloud formation is sensitive to aerosols – tiny particles in the atmosphere. Aerosols can act as cloud condensation nuclei, around which cloud droplets can form. Changes in aerosol concentrations, due to human activities or natural processes, can therefore influence cloud properties and, consequently, the climate.

  6. Cloud condensation nuclei - Wikipedia

    en.wikipedia.org/wiki/Cloud_condensation_nuclei

    A typical raindrop is about 2 mm in diameter, a typical cloud droplet is on the order of 0.02 mm, and a typical cloud condensation nucleus is on the order of 0.0001 mm or 0.1 μm or greater in diameter. [1] The number of cloud condensation nuclei in the air can be measured at ranges between around 100 to 1000 per cm 3. [1]

  7. Sea salt aerosol - Wikipedia

    en.wikipedia.org/wiki/Sea_salt_aerosol

    Cloud drops formed on giant sea salt aerosols may grow much more rapidly by condensation that cloud drops formed on small soluble aerosol particles, as giant sea salt cloud drops may remain concentrated solution drops for long times after they are carried into cloud. Such drops may have condensational growth rates more than two times faster ...

  8. Hurricane dynamics and cloud microphysics - Wikipedia

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

    The shape of liquid water drops is generally spherical because of the effects of surface tension. Depending on the size of the drop the friction of the air flowing past a falling drop may squish the bottom on the drop so that it is slightly non-spherical. However, solid ice does not generally form into nice spherical shapes.

  9. Cloud seeding - Wikipedia

    en.wikipedia.org/wiki/Cloud_seeding

    Cloud seeding in the United Arab Emirates is a weather modification technique used by the government to address water challenges in the country. Cloud seeding is also referred to as man made precipitation and artificial rain making. [61] The United Arab Emirates is one of the first countries in the Persian Gulf region to use cloud seeding ...