The most common temperature stratification during winter in the central Europe is an inversion – i.e. temperature of air increases with height. The best way to visualize these situations are vertical cross sections and thermodiagrams. Figure 1 – Vertical change of temperature (solid line) and dew point (dashed line) in Wien on Dec 19th (blue), […]
According to theory, the most typical circulation difference between mid- and tropical latitudes is there is almost no vertical wind shear in the tropics, i.e. there is the same wind speed and direction with the height. However, situation is much more complex in the reality. Nice example of the tropical weather complexity is the Southeast […]
There are lot of meteorologic variables and many of them are very advanced, but still, we are able to obtain key information just from a single parameter. If we are familiar with the parameter’s natural background, the only trick is – visualisation 🙂 We choose a dew point today which is – by definition – […]
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