Tropical-wide teleconnection and oscillation. I: Teleconnection indices and type I/type II states

The tropical oscillation of the ENSO-monsoon (EI Nino Southern Oscillation- Asian monsoons) system is studied based on 34-year simulations of an atmosp heric general-circulation model with specified sea surface temperature (SST ), together with some observed data for the same period. In particular, two indices are studied: the first is the generalized index of Indian monsoon rainfall (IMR), and the other is an index by which the interaction/non-inte raction between the ENSO and the Indian monsoon system is assessed. In order to examine the validity of the first index, the Indian subcontinen t and the near-equatorial western Pacific were selected as two key location s. They correspond, approximately, to the dominant regions in the first emp irical orthogonal function of precipitation, for boreal summer and winter, respectively. These two regions form the western rim of a 'horseshoe' telec onnection pattern in their respective seasons. The time coefficients of emp irical orthogonal function mode I in the two seasons are taken as the key i ndices which are referred to as the Tropical-wide Oscillation Index (TOI). Having defined the spatial patterns in both seasons, the lead-lag teleconne ction structure associated with the ENSO-monsoon system is studied; the res ult is that the TOI for boreal summer is more useful than the TOI for borea l winter for identifying the lead-lag nature of the ENSO-monsoon. The new i ndex is then related to traditional indices like the IMR and the Southern O scillation Index, but proves to be a more comprehensive index for lead-lag correlations with key variables, while the latter, the TOI for winter, has no precursory signal for the Indian monsoon for the following summer. The second index is the Walker circulation Index (WAI), which represents th e eastward/westward shift of the updraught region of the Walker circulation . It is proposed that the WAI can usefully distinguish between years when t he ENSO-monsoon oscillation operates (type I) and years when it does not (t ype II). If the SST in the key region has a climatologically close-to-norma l condition, the slate of the coupled equatorial system is in type II. On t he other hand, if the deviation from climatology is large, the tropical-wid e oscillation will continue to be active; these years are type I. Eliminati on of the type II years from the data significantly enhances the time-lagge d correlations between the TOI and some key variables, such as SST. As a re sult, the biennial oscillation becomes clearer.