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Homogenization of Portuguese long-term temperature data series: Lisbon, Coimbra and Porto

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Figure

Table 1. The 90 %, 95 % and 99 % critical values for the following homogeneity test statistics: N of the von Neumann ratio test, T0 of theSNHT, XK of the Pettitt test and Q of the Buishand partial sum tests, for data sets with different lengths (114, 141 and 153 elements).
Figure 1. Homogenization procedure. Top – main procedure. Bottom – correction procedure for known non-climatic breaks.
Table 2. Major volcanic eruptions from 1850 to 2000. DVI valuestaken from the NCDC database.
Table 3. Known dates of changes in thermometer heights (ht) and locations for the three Portuguese stations of Lisbon, Coimbra and Porto.
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