Monthly sea surface temperatures from January 1982 to December 2018 observed by the optimum interpolation sea surface temperature.
data(ElNino_OISST_region_1and2)
data(ElNino_OISST_region_3)
data(ElNino_OISST_region_4)
data(ElNino_OISST_region_3and4)An object of class sfts.
These averaged monthly sea surface temperatures are measured by the different moored buoys in the "Nino region" defined by the coordinates 0-10 degree South and 90-80 degree West.
A. Antoniadis and T. Sapatinas (2003) "Wavelet methods for continuous-time prediction using Hilbert-valued autoregressive processes", Journal of Multivariate Analysis, 87(1), 133-158.
P. C. Besse, H. Cardot and D. B. Stephenson (2000) "Autoregressive forecasting of some functional climatic variations", Scandinavian Journal of Statistics, 27(4), 673-687.
F. Ferraty, A. Rabhi and P. Vieu (2005) "Conditional quantiles for dependent functional data with application to the climate EL Nino Phenomenon", Sankhya: The Indian Journal of Statistics, 67(2), 378-398.
F. Ferraty and P. Vieu (2007) Nonparametric functional data analysis, New York: Springer.
R. J. Hyndman and H. L. Shang (2010) "Rainbow plots, bagplots, and boxplots for functional data", Journal of Computational and Graphical Statistics, 19(1), 29-45.
E. Moran, R. Adams, B. Bakoyema, S. Fiorini and B. Boucek (2006) "Human strategies for coping with El Nino related drought in Amazonia", Climatic Change, 77(3-4), 343-361.
A. Timmermann, J. Oberhuber, A. Bacher, M. Esch, M. Latif and E. Roeckner (1999) "Increased El Nino frequency in a climate model forced by future greenhouse warming", Nature, 398(6729), 694-697.
plot(ElNino_OISST_region_1and2)
plot(ElNino_OISST_region_3)
plot(ElNino_OISST_region_4)
plot(ElNino_OISST_region_3and4)
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