Research Article

Improving Regional Dynamic Downscaling with Multiple Linear Regression Model Using Components Principal Analysis: Precipitation over Amazon and Northeast Brazil

Table 1

Configuration of the seven simulations.

SimulationPrecipitation Efficiency (PEFF)SUBEX
(RHmin)
Dynamic control (closure)

GR_PD_SD0.25–1.000.65 Arakawa and Schubert (1974) [13]
GR_PD_SW0.25–1.000.90Arakawa and Schubert (1974) [13]
EM_SD0.65
EM_SW0.90
GR_PW_SD0.25–0.500.65Arakawa and Schubert (1974) [13]
GR_PW_SW0.25–0.500.90Arakawa and Schubert (1974) [13]
GR_PW_SW_FC0.25–0.500.90 Fritsch and Chappell (1980) [14]

GR: parameterization of cumulus Grell; MS: parameterization of cumulus MIT-Emanuel; PD: PEFF dry (high evaporation rate of the raindrop, therefore decreases precipitation); PW: PEFF wet (low evaporation rate of the raindrop, therefore increases the precipitation); SD: SUBEX dry (low minimum relative humidity for cloud formation); SW: SUBEX wet (high minimum relative humidity for cloud formation); FC: closure cloud Fritsch and Chappell (1980) [14].