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- W2740479890 abstract "Nowadays, practically all NWP and climate models use a mass flux concept to parameterize convective transport. In such a mass flux framework the fractional entrainment (ǫ) and detrainment (δ) coefficients are the key parameters. The fractional entrainment coefficient describes the inflow of environmental air into the cloudy area, whereas the fractional detrainment coefficient describes the outflow of cloudy air into the environment. Despite numerous efforts to parameterize ǫ and δ, there is still no concensus on a particular parameterization, satisfying in all possible conditions. Neither do we have much insight into the behavior of these lateral mixing coefficients. For example: Why is the detrainment more variable from case to case and hour to hour than the entrainment? (see e.g. [de Rooy and Siebesma(2008)]) To gain more insight into the behavior we derive analytical expressions for ǫ and δ from first principles and with a minimum of assumptions. In contrast with most other studies we are not directly targeted towards the development of a new parameterization." @default.
- W2740479890 created "2017-08-08" @default.
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- W2740479890 date "2009-01-01" @default.
- W2740479890 modified "2023-09-27" @default.
- W2740479890 title "Lateral mixing in shallow convection: In theory and in practice" @default.
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