Sk. Park et Kk. Droegemeier, Sensitivity analysis of a moist 1D Eulerian cloud model using automatic differentiation, M WEATH REV, 127(9), 1999, pp. 2180-2196
An automatic differentiation tool (ADIFOR) is applied to a warm-rain, time-
dependent 1D cloud model to study the influence of input parameter variabil
ity, including that associated with the initial state as well as physical a
nd computational parameters, on the dynamical evolution of a deep convectiv
e storm.
Storm dynamics are found to be controlled principally by changes in model i
nitial states below 2 km; once perturbed, each grid variable in the model p
lays its own unique role in determining the dynamical evolution of the stor
m. Among all model-dependent variables, the low-level temperature field has
the greatest impact on precipitation, followed by the water vapor field. M
ass field perturbations inserted at upper levels induce prominent oscillati
ons in the wind field, whereas a comparable wind perturbation has a negligi
ble effect on the thermodynamic field. However, the wind field does influen
ce the precipitation in a more complex way than does the thermodynamic fiel
d, principally via changes in time evolution.
The simulated storm responds to variations in three physical parameters (th
e autoconversion/accretion rate, cloud radius, and lateral eddy exchange co
efficient) largely as expected, with the relative importance of each, quant
ified via a relative sensitivity analysis, being a strong function of the p
articular stage in the storm's life cycle.