Sabine was followed by Victoria
Last week, we looked at low Sabine in this post. Sabine felt much more present in the media than Victoria and also caused more widespread gale-force winds (at the UK Met Office, Victoria is called Dennis this time). From a meteorological point of view, however, Victoria also had a lot to offer. Like Sabine, it originated from the strong westerly flow over the Atlantic. Victoria reached an impressively low core pressure of around 920hPa on its way towards northern Europe, making it one of the top 5 "deepest lows" in the North Atlantic. It underwent a bombogenesis (the WeatherBlog is happy every time it has the opportunity to use this beautiful word). This means that the core pressure drops by at least 1hPa per hour for at least 24 hours - in other words, the low intensifies extremely quickly.