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  2. Bulk Richardson number - Wikipedia

    en.wikipedia.org/wiki/Bulk_Richardson_number

    The Bulk Richardson Number (BRN) is an approximation of the Gradient Richardson number. [1] The BRN is a dimensionless ratio in meteorology related to the consumption of turbulence divided by the shear production (the generation of turbulence kinetic energy caused by wind shear) of turbulence.

  3. Mixing ratio - Wikipedia

    en.wikipedia.org/wiki/Mixing_Ratio

    In atmospheric chemistry, mixing ratio usually refers to the mole ratio r i, which is defined as the amount of a constituent n i divided by the total amount of all other constituents in a mixture: r i = n i n t o t − n i {\displaystyle r_{i}={\frac {n_{i}}{n_{\mathrm {tot} }-n_{i}}}}

  4. Richardson number - Wikipedia

    en.wikipedia.org/wiki/Richardson_Number

    The Richardson number, or one of several variants, is of practical importance in weather forecasting and in investigating density and turbidity currents in oceans, lakes, and reservoirs. When considering flows in which density differences are small (the Boussinesq approximation ), it is common to use the reduced gravity g' and the relevant ...

  5. Talk:Triclopyr - Wikipedia

    en.wikipedia.org/wiki/Talk:Triclopyr

    Ortho manufactures two virtually identical triclopyr products that are marketed for different applications. One product is named 'Weed B Gon for Chickweed, Clover & Oxalis'. It has a purple label, and is not to be confusd with regular 'Weed B Gon for Broadleaf Weeds in Lawns', which contains totally different herbicidal ingredients.

  6. Paraquat - Wikipedia

    en.wikipedia.org/wiki/Paraquat

    Paraquat (trivial name; / ˈ p ær ə k w ɒ t /), or N,N′-dimethyl-4,4′-bipyridinium dichloride (systematic name), also known as methyl viologen, is a toxic organic compound with the chemical formula [(C 6 H 7 N) 2]Cl 2.

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  9. Convective available potential energy - Wikipedia

    en.wikipedia.org/wiki/Convective_available...

    Severe weather and tornadoes can develop in an area of low CAPE values. The surprise severe weather event that occurred in Illinois and Indiana on April 20, 2004, is a good example. Importantly in that case, was that although overall CAPE was weak, there was strong CAPE in the lowest levels of the troposphere which enabled an outbreak of ...

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