<SYSTEM_TASK:>
Solve the following problem using Python, implementing the functions described below, one line at a time
<END_TASK>
<USER_TASK:>
Description:
 def pseudoadiabat(T,p):
 """Compute the local slope of the pseudoadiabat at given temperature and pressure Inputs: p is pressure in hPa or mb T is local temperature in Kelvin Output: dT/dp, the rate of temperature change for pseudoadiabatic ascent in units of K / hPa The pseudoadiabat describes changes in temperature and pressure for an air parcel at saturation assuming instantaneous rain-out of the super-saturated water Formula consistent with eq. (2.33) from Raymond Pierrehumbert, "Principles of Planetary Climate" which nominally accounts for non-dilute effects, but computes the derivative dT/dpa, where pa is the partial pressure of the non-condensible gas. Integrating the result dT/dp treating p as total pressure effectively makes the dilute assumption. """

    esoverp = clausius_clapeyron(T) / p
    Tcel = T - tempCtoK
    L = (2.501 - 0.00237 * Tcel) * 1.E6   # Accurate form of latent heat of vaporization in J/kg
    ratio = L / T /  Rv
    dTdp = (T / p * kappa * (1 + esoverp * ratio) /
        (1 + kappa * (cpv / Rv + (ratio-1) * ratio) * esoverp))
    return dTdp