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[1] Dee, D.P., Uppala, S.M., Simmons, A.J., Berrisford, P., Poli, P., Kobayashi, S., Andrae, U., Balmaseda, M.A., Balsamo, G., Bauer, P., Bechtold, P., Beljaars, A.C.M., van de Berg, L., Bidlot, J., Bormann, N., Delsol, C., Dragani, R., Fuentes, M., Geer, A.J., Haimberger, L., Healy, S.B., Hersbach, H., H&amp;oacute;lm, E.V., Isaksen, L., K&amp;aring;llberg, P., K&amp;ouml;hler, M., Matricardi, M., McNally, A.P., Monge-Sanz, B.M., Morcrette, J.-J., Park, B.&amp;amp;#8208;K., Peubey, C., de Rosnay, P., Tavolato, C., Th&amp;eacute;paut, J.-N. and Vitart, F. (2011), The ERA-Interim reanalysis: configuration and performance of the data assimilation system. Q.J.R. Meteorol. Soc., 137, 553-597. doi:10.1002/qj.828&#xD;
&#xD;
[2] Murray, R. J., &amp;amp; Simmonds, I. (1991). A numerical scheme for tracking cyclone centres from digital data. Part I: development and operation of the scheme. Australian Meteorological Magazine, 39, 155-166.
Data quality: 
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3. The results for successive years were checked to ensure that all cyclone tracks starting between 00Z on 1-Nov of year N and 00Z on 1-Mar of year N+1 were identical between the cyclone tracking software runs for year N and year N+1.&#xD;
&#xD;
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