G. Gong et al., REGIONAL AND SEASONAL ESTIMATES OF FRACTIONAL STORM COVERAGE BASED ONSTATION PRECIPITATION OBSERVATIONS, Journal of climate, 7(10), 1994, pp. 1495-1505
Simulated climates using numerical atmospheric general circulation mod
els (GCMs) have been shown to be highly sensitive to the fraction of G
CM grid area assumed to be wetted during rain events. The model hydrol
ogic cycle and land-surface water and energy balance are influenced by
the parameter <(kappa)over bar>, which is the dimensionless fractiona
l wetted area for GCM grids. Hourly precipitation records for over 170
0 precipitation stations within the contiguous United States are used
to obtain observation-based estimates of fractional wetting that exhib
it regional and seasonal variations. The spatial parameter <(kappa)ove
r bar> is estimated from the temporal raingauge data using conditional
probability relations. Monthly <(kappa)over bar> values are estimated
for rectangular grid areas over the contiguous United States as defin
ed by the Goddard Institute for Space Studies 4 degrees X 5 degrees GC
M. A bias in the estimates is evident due to the unavoidably sparse ra
ingauge network density, which causes some storms to go undetected by
the network. This bias is corrected by deriving the probability of a s
torm escaping detection by the network. A Monte Carlo simulation study
is also conducted that consists of synthetically generated storm arri
vals over an artificial grid area. It is used to confirm the ii estima
tion procedure and to test the nature of the bias and its correction.
These monthly fractional wetting estimates, based on the analysis of s
tation precipitation data, provide an observational basis for assignin
g the influential parameter <(kappa)over bar> in GCM land-surface hydr
ology parameterizations.