Three metrological stations (Figure 6 and Table 1) with IDF curves are Ipoh, Kuala Lumpur and Melaka Station.
The temperature records obtained at these stations (Figure 4) revealed the characteristics of BWT variations in the study area.
There are linear relationships between the hydrogen and oxygen isotope distributions and salinity for both stations (Figure 4).
REF predicted 2-year displacements fit the first-order pattern of the seaward motion of the land GPS stations (Figure 3a).
Relative height changes of about 1 cm between these stations (Figure 3b) occurred over the same period, although the signal-to-noise ratio was small.
Variations in site amplifications for high frequencies exist even for borehole Hi-net stations (Figure 7 of Takemoto et al. 2012).
The model developed for the spread of the SM assumes that the moth reaches new areas via access points such as harbours and border stations (Figure 3).
However, the Pc1 pulsations observed at MOS were much weaker than those seen at the other two stations (Figure 6e,f).
The years 2002, 2004 2005, and 2007 showed the warmest surface temperature departures over the past decade at all four stations (Figure 5).
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