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  2. Sea surface microlayer - Wikipedia

    en.wikipedia.org/wiki/Sea_surface_microlayer

    The sea surface microlayer (SML) is the boundary interface between the atmosphere and ocean, covering about 70% of Earth's surface. With an operationally defined thickness between 1 and 1,000 μm (1.0 mm), the SML has physicochemical and biological properties that are measurably distinct from underlying waters.

  3. Alpha particle - Wikipedia

    en.wikipedia.org/wiki/Alpha_particle

    Alpha particles, also called alpha rays or alpha radiation, consist of two protons and two neutrons bound together into a particle identical to a helium-4 nucleus. [5] They are generally produced in the process of alpha decay but may also be produced in other ways. Alpha particles are named after the first letter in the Greek alphabet, α.

  4. Radiation - Wikipedia

    en.wikipedia.org/wiki/Radiation

    This means that alpha particles from ordinary alpha decay do not penetrate the outer layers of dead skin cells and cause no damage to the live tissues below. Some very high energy alpha particles compose about 10% of cosmic rays, and these are capable of penetrating the body and even thin metal plates. However, they are of danger only to ...

  5. Sea surface skin temperature - Wikipedia

    en.wikipedia.org/wiki/Sea_surface_skin_temperature

    The maximum temperature can be found in the subskin layer, where the external heating per depth is lower than in the skin layer, but where the surface cooling has a smaller effect. With further increasing depth, the temperature declines, as the proportional heating is smaller and the layer is mixed via turbulent processes.

  6. Aphotic zone - Wikipedia

    en.wikipedia.org/wiki/Aphotic_zone

    The layers of the pelagic zone. All but the epipelagic zone make up the aphotic zone. Zones of the water column as defined by the amount of light penetration. The mesopelagic is sometimes referred to as the dysphotic zone. In the ocean, the aphotic zone is sometimes referred to as the dark ocean.

  7. Mesopelagic zone - Wikipedia

    en.wikipedia.org/wiki/Mesopelagic_zone

    A fraction of this production is exported out of the surface mixed layer and into the mesopelagic zone. One pathway for carbon export from the euphotic layer is through sinking of particles, which can be accelerated through repackaging of organic matter in zooplankton fecal pellets, ballasted particles, and aggregates. [8]

  8. Alpha decay - Wikipedia

    en.wikipedia.org/wiki/Alpha_decay

    This increases the chance of double-strand breaks to the DNA in cases of internal contamination, when ingested, inhaled, injected or introduced through the skin. Otherwise, touching an alpha source is typically not harmful, as alpha particles are effectively shielded by a few centimeters of air, a piece of paper, or the thin layer of dead skin ...

  9. Bathypelagic zone - Wikipedia

    en.wikipedia.org/wiki/Bathypelagic_zone

    Layers of the pelagic zone. The bathypelagic zone or bathyal zone (from Greek βαθύς (bathýs), deep) is the part of the open ocean that extends from a depth of 1,000 to 4,000 m (3,300 to 13,000 ft) below the ocean surface.