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  2. Water activity - Wikipedia

    en.wikipedia.org/wiki/Water_activity

    Water activity is the thermodynamic activity of water as solvent and the relative humidity of the surrounding air after equilibration. As temperature increases, aw typically increases, except in some products with crystalline salt or sugar. Water migrates from areas of high aw to areas of low aw.

  3. Köppen climate classification - Wikipedia

    en.wikipedia.org/wiki/Köppen_climate_classification

    The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, [ 1 ][ 2 ] with several later modifications by Köppen, notably in 1918 and 1936. [ 3 ][ 4 ] Later, German climatologist Rudolf Geiger (1894–1981 ...

  4. Moisture sorption isotherm - Wikipedia

    en.wikipedia.org/wiki/Moisture_sorption_isotherm

    An increase in a w is usually accompanied by an increase in water content, but in a non-linear fashion. This relationship between water activity and moisture content at a given temperature is called the moisture sorption isotherm. These curves are determined experimentally and constitute the fingerprint of a food system.

  5. Wallemia sebi - Wikipedia

    en.wikipedia.org/wiki/Wallemia_sebi

    Wallemia sebi have lower limits for growth below water activity of 0.75 (0.69-0.75)aw, [5] while most microorganisms are limited to 0.95 and above. [6] Wallemia sebi has been isolated from hair, hay, textiles and man. [7] It can grow slowly without additional solute in the growth medium, and form small, reddish-brown, powdery colonies. [3]

  6. Lofoten Vortex - Wikipedia

    en.wikipedia.org/wiki/Lofoten_Vortex

    Through the eddy activity of the Lofoten Basin and the persistence of the Lofoten Vortex, the residence time of the warm water is lengthened, leading to additional cooling of the AW before it reaches the Arctic Ocean. [4] Due to heat loss, the temperature decreases and the light-to-dense water transformation takes place.

  7. Osmotic pressure - Wikipedia

    en.wikipedia.org/wiki/Osmotic_pressure

    Osmotic pressure is the minimum pressure which needs to be applied to a solution to prevent the inward flow of its pure solvent across a semipermeable membrane. [1] It is also defined as the measure of the tendency of a solution to take in its pure solvent by osmosis. Potential osmotic pressure is the maximum osmotic pressure that could develop ...

  8. Raoult's law - Wikipedia

    en.wikipedia.org/wiki/Raoult's_law

    Raoult's law (/ ˈ r ɑː uː l z / law) is a relation of physical chemistry, with implications in thermodynamics.Proposed by French chemist François-Marie Raoult in 1887, [1] [2] it states that the partial pressure of each component of an ideal mixture of liquids is equal to the vapor pressure of the pure component (liquid or solid) multiplied by its mole fraction in the mixture.

  9. Tropical climate - Wikipedia

    en.wikipedia.org/wiki/Tropical_climate

    Tropical climate is the first of the five major climate groups in the Köppen climate classification identified with the letter A. Tropical climates are defined by a monthly average temperature of 18 °C (64 °F) or higher in the coolest month, featuring hot temperatures and high humidity all year-round. Annual precipitation is often abundant ...