24 Aug 2016
The progression of the boreal winter monsoon through the western Maritime Continent as differentiated by ENSO phase
Related authors
Atmos. Chem. Phys., 19, 5363–5385, 2019
Cited articles
Aldrian, E. and Susanto, R. D.: Identification of three dominant rainfall regions within Indonesia and their relationship to sea surface temperature, Int. J. Climatol., 23, 1435–1452, 2003.
Aldrian, E., Gates, L. D., and Widodo, F. H.: Variability of Indonesian Rainfall and the Influence of ENSO and Resolution in ECHAM4 simulations and in the Reanalyses, MPI Report 346, 30 pp., available from Max Planck- Institut für Meteorologie, Bundesstr. 55, 20146, Hamburg, Germany, 2003.
Ashok, K., Behera, S. K., Rao, S. A., Weng, H., and Yamagata, T.: El Niño Modoki and its possible teleconnection, J. Geophys.Res., 112, 2156–2202, 2007.
Atlas, R., Hoffman, R. N., Ardizzone, J., Leidner, S. M., Jusem, J. C., Smith, D. K., and Gombos, D.: A cross-calibrated, multiplatform ocean surface wind velocity product for meteorological and oceanographic applications, B. Am. Meteorol. Soc., 92, 157–174, 2011.
Braak, C.: Atmospheric variations of short and long duration in the Malay Archipelago, Verhandelingen No. 5, Koninlijk Magnetisch en Meteorologisch Observatorium te Batavia, Batavia, Indonesia, 1919.
