Research Article

Impact of Preceding El Niño and the Indian Ocean Dipole on the Southern China Precipitation in Early Summer

Table 2

Designs of the numerical experiment.

Experiment namesApplicationForcing of SSTDuration of the integration

CTLGetting the model climateThe climatological SST varying seasonally within the CAM3.0Integration for 20 years from 1 September

SEXP1Getting the single influence of PE and PISEXP1-PE: P-SSTA imposed over TPTen different integration durations
SEXP1-PI: P-SSTA imposed over TIO

SEXP2Diagnosing the stability and sensitivity of the modelSEXP2-PE: various intensity P-SSTA* imposed over TPIntegrated from September to next June
SEXP2-PI: various intensity P-SSTA* imposed over TIO

SEXP3Getting the combined influence of PEISEXP3-PEI: P-SSTA imposed over TP and TIOIntegrated from September to next June

Based on P-SSTA, the imposed SSTAs were modified by adding/subtracting 0.5°C at all grid points over TP or modified by adding/subtracting 0.3°C at all grid points over TIO.