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  2. Free convective layer - Wikipedia

    en.wikipedia.org/wiki/Free_convective_layer

    In atmospheric sciences, the free convective layer (FCL) is the layer of conditional or potential instability in the troposphere. It is a layer in which rising air can experience positive buoyancy (PBE) so that deep, moist convection (DMC) can occur.

  3. Water cycle - Wikipedia

    en.wikipedia.org/wiki/Water_cycle

    The processes that drive these movements are evaporation, transpiration, condensation, precipitation, sublimation, infiltration, surface runoff, and subsurface flow. In doing so, the water goes through different forms: liquid, solid and vapor. The ocean plays a key role in the water cycle as it is the source of 86% of global evaporation.

  4. Level of free convection - Wikipedia

    en.wikipedia.org/wiki/Level_of_free_convection

    Diagram showing an air parcel path when raised along B-C-E compared to the surrounding air mass Temperature (T) and humidity (Tw); see CAPE. The level of free convection (LFC) is the altitude in the atmosphere where an air parcel lifted adiabatically until saturation becomes warmer than the environment at the same level, so that positive buoyancy can initiate self-sustained convection.

  5. Condensation - Wikipedia

    en.wikipedia.org/wiki/Condensation

    Condensation is the change of the state of matter from the gas phase into the liquid phase, and is the reverse of vaporization. The word most often refers to the water cycle . [ 1 ] It can also be defined as the change in the state of water vapor to liquid water when in contact with a liquid or solid surface or cloud condensation nuclei within ...

  6. Condensate - Wikipedia

    en.wikipedia.org/wiki/Condensate

    Condensate may refer to: . The liquid phase produced by the condensation of steam or any other gas; The product of a chemical condensation reaction, other than water; Natural-gas condensate, in the natural gas industry

  7. Dropwise condensation - Wikipedia

    en.wikipedia.org/wiki/Dropwise_condensation

    In dropwise condensation the condensate liquid collects in the form of countless droplets of varying diameters on the condensing surface, instead of forming a continuous film, and does not wet the solid cooling surface. The droplets develop at points of surface imperfections (pit, scratch), called nucleation sites, and grow in size as more ...

  8. Dew point - Wikipedia

    en.wikipedia.org/wiki/Dew_point

    If the air is very dry and has few water molecules, the dew point is low and surfaces must be much cooler than the air for condensation to occur. If the air is very humid and contains many water molecules, the dew point is high and condensation can occur on surfaces that are only a few degrees cooler than the air. [8]

  9. The Voyage of the Mimi - Wikipedia

    en.wikipedia.org/wiki/The_Voyage_of_the_Mimi

    Each video segment has accompanying student and teacher handouts or worksheets. [2] Four software modules are available that covered topics and skills in navigation and map reading, computer literacy and programming, the elements of ecosystems, and the natural environment of whales. [5] [6]

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