It can be emphasised that the higher temperatures observed in Moldavia were explained by thethermal advection, but also by the foehn processes occurred over the Eastern Carpathians, as the analysis ofthe Non-Hydrostatic Mesoscale Model (NMM), developed at the National Centers for EnvironmentalPrediction (NCEP), within the U.S. National Oceanic and Atmospheric Administration (NOAA)showed, using vertical sections, rendering the vertical distribution of the relative moisture, cloudinessand air temperature, and the vertical wind profile on both sides of the mountain massifs in the northernpart of the Eastern Carpathians (Figs. 3 a, b, c).
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