Abstract
In this paper, we examine the return and volatility spillovers, together with the trend spillovers on the sectoral equity returns for Australian and New Zealand markets. We find that the return spillovers of industrial, local and global shocks have a limited effect on Australian and New Zealand sector returns, whereas the volatility spillovers play a significant role on explaining the volatility of sector equity indices. Furthermore, we discover that the volatility spillover effects of the global and industrial shocks are greater in magnitude for explaining the volatility of the Australian sectors than those of New Zealand, particularly basic materials, oil and gas, technology and telecom sectors. By employing the trend spillover model, we find that the volatility spillover effects of global sector indices have been increasing over the volatility of the Australian sectoral returns until now. This finding proposes that Australian sector equity market is more integrated with the world than the New Zealand counterpart.
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Notes
For a detailed survey, see Balli et al. (2013a).
In this paper, “industrial” and “sectoral” are used interchangeably. Additionally we used “global” and “world” words interchangeably as well. For the sake of brevity, when we refer the “industrial” shocks, we refer the global industrial shocks.
Level 1 is the market index which covers all the sectors in each region or countries. Level 2 divides the total market into 10 industries and covers all the sectors within each group in each region or country. Level 3–6 subdivide the level 2 classifications into sector classifications in increasing detail.
The sector indices are listed in Table 1.
However, the data for telecom, utilities, industrials and technology of New Zealand are available from 29/07/1991; 18/05/1992; 11/04/1994 and 18/06/2007 while the data for technology and telecom of Australia only available from 28/05/2001 and 17/06/1996 respectively.
Some global sector indices (oil & gas, telecom and technology) might have affected national equity returns, and may not be able to claim that 𝜖 NZ,t is a isolated local shock, therefore we use Cholesky decomposition to explore the idiosyncratic innovations of the national equity markets. After applying this decomposition, the results did not change substantially. For more the details of Cholesky decomposition, see Balli and Balli (2011).
The application of variance ratio to Australian sector equity index can be easily driven from these formulas.
Due to the political and economic integration between New Zealand and Australia, there might be some spillover effects from Australia to New Zealand. For the NZ index, indeed, the literature is pointing out. However, for sectoral indices, we have run the following model: R s,t =a s+b s R s,t−1+η NZ,t−1 R NZ,t−1+η w,t−1 R w,t−1+η GS,t−1 R GS,t−1+η A,t−1 R A,t−1+ε s,t . Different from Eq. (2), we have tested the Australia effect via R A,t−1 and 𝜖 A,t . However, after performing the models for NZ sectoral returns, we have observed that the coefficients of Australia effect are mostly insignificant. More importantly, the effect of Australia’s sectoral equity indices on the variance ratios of New Zealand sector indices is negligible.
The variance ratio results for the constant spillover and time-varying spillover models are similar, and therefore we did not post the results of variance ratios for the time-varying model.
Local shock represents the ratio of the aggregate New Zealand (Australia) equity index on the volatility of the sector equity indices, global shock represents the ratio of the aggregate world equity index on the volatility of sector’s equity indices and industrial shock represents the ratio of the global sector equity indices on the volatility of the sector equity indices. Own shock is the idiosyncratic shock of the sector indices on its own volatility, which equals 1 − (local shock+ global shock+ industrial shock)
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Balli, F., Balli, H.O. & Hong, R. Spillover effects on the sectoral returns for australian and New Zealand equity markets. J Econ Finan 40, 568–589 (2016). https://doi.org/10.1007/s12197-015-9326-6
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DOI: https://doi.org/10.1007/s12197-015-9326-6