A Rare Europe Summer Scorcher
So what is the culprit for the development of this heat wave? It all begins with a robust ridge of high pressure that is situated between the middle and upper levels of the atmosphere. Geopotential height, a measure of the height of a constant pressure surface above the mean sea level, is a useful diagnostic tool and proxy for determining the strength of a ridge or trough affecting a region, and higher (lower) heights usually correspond to warmer (cooler) surface temperatures. During this heat wave, most of Europe has been faced with 500 hPa (~5,500 meters above sea level) geopotential heights that are 2-3 standard deviations above normal for this time of year, which equates to anywhere from 5,800-5,900 m. Specifically, most of western Europe At the surface, maximum temperatures have been 6-10°C above normal. Furthermore, the positioning of the jet stream also favors south-to-north advection of warmer air in the upper levels.
The excessive warmth is expected to continue once again by the end of this week as the current Global Forecast System (GFS) model runs indicate the development of another high-pressure system and upper-level ridge. Southwesterly winds will once again facilitate robust warm air advection over much of Europe and keep temperatures several degrees above normal as the air above the surface warms considerably. In addition, moisture over western France and the UK will likely yield heat indices that exceed 38°C (~100°F) there while much warmer temperatures are forecast over Spain. Under this level of warmth, it is imperative to stay hydrated and cool to escape potentially harmful heat-related illnesses, especially in regions that are not adapted to very warm conditions.
To learn more about other high-impact weather events across Europe, be sure to click here!
© 2018 Meteorologist Brian Matilla
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