adiabatic_ascent: Properties of an air parcel after adiabatic ascent
Description
A particle located at Pstart pressure (Pa), Tstart temperature (K) and wstart mixing ratio (kg/kg) ascends (pseudo)adiabatically to Pend (Pa). The evolution is computed by numerically integrating the dT/dP ordinary differential equation (ODE) using a 4th order Runge-Kutta scheme, assuming hydrostatic equilibrium and that the particle is saturated after the Lifted Condensation Level (LCL).
deltaP (Pa) represents the numerical increment used for integrating the Ordinary Differential Equation (ODE) representing the vertical evolution
Value
The function returns a list that includes Tend (final value of temperature) and mixRatioEnd (mixing ratio of the air parcel at the end of the evolution).