Gr. Pandey et al., A hybrid orographic plus statistical model for downscaling daily precipitation in northern California, J HYDROMETE, 1(6), 2000, pp. 491-506
A hybrid (physical-statistical) scheme is developed to resolve the finescal
e distribution of daily precipitation over complex terrain. The scheme gene
rates precipitation by combining information from the upper-air conditions
and From sparsely distributed station measurements: thus, it proceeds in tw
o steps. First, an initial estimate of the precipitation is made using a si
mplified orographic precipitation model. It is a steady-state, multilayer,
and two-dimensional model following the concepts of Rhea, The model is driv
en by the 2.5 degrees x 2.5 degrees gridded National Oceanic and Atmospheri
c Administration-National Centers for Environmental Prediction upper-air pr
ofiles, and its parameters are tuned using the observed precipitation struc
ture of the region, Precipitation is generated assuming a forced lifting of
the air parcels as they cross the mountain barrier following a straight tr
ajectory. Second, the precipitation is adjusted using errors between derive
d precipitation and observations from nearby sites. The study area covers t
he northern half of California, including coastal mountains, central valley
, and the Sierra Nevada. The model is run for a 5-km rendition of terrain f
or days of January-March over the period of 1988-95. A jackknife analysis d
emonstrates the validity of the approach. The spatial and temporal distribu
tions of the simulated precipitation field agree well with the observed pre
cipitation, Further, a mapping of model performance indices (correlation co
efficients, model bias, root-mean-square error, and threat scores) from an
array of stations from the region indicates that the model performs satisfa
ctorily in resolving daily precipitation at 5-km resolution.