{"id":3263,"date":"2012-11-08T22:00:32","date_gmt":"2012-11-09T03:00:32","guid":{"rendered":"http:\/\/ezweather.com\/myblog\/?p=3263"},"modified":"2012-11-25T22:25:30","modified_gmt":"2012-11-26T03:25:30","slug":"weather-trends","status":"publish","type":"post","link":"https:\/\/www.ezweather.com\/myblog\/2012\/11\/08\/weather-trends\/","title":{"rendered":"Climate Review – Weather Trends for Thursday, November 8th"},"content":{"rendered":"

Hi Everyone,<\/p>\n

In this blog, I want to share with you a Climate Review on Weather Trends.\u00a0 On Weather Trends, I’ll be sharing with three main sections, Upper Air, Temperatures, and Precipitation Totals.\u00a0 Its always important to see how the weather has been trending.\u00a0 This information is a vital toward weather forecasting.\u00a0\u00a0\u00a0So, let’s begin…<\/p>\n

Part 1 – Weather Trends: Upper<\/strong> Air
\n<\/span>In this section, we’ll be reviewing the Upper Air Pattern.\u00a0 In using 500mb maps, they provide a big picture view of what happening upstairs in the atmosphere. The average 500mb plot allowed me to draw up the jet stream, which typically can be found on the 300mb or 250mb map.\u00a0 Here we can roughly see ridges and troughs.\u00a0 When I mention ridges, think of the height lines increasing, while troughs you see the height lines dip.\u00a0 Trough are typically associated with stormy weather, while ridges are the opposte, drier and stable.\u00a0 The 500mb anomaly maps really show a signal, a tendency or another way to think of it, where ridges and troughs are developing stronger compared to climatology. For these maps, we’ll look at the past 30 days to how the Fall Pattern has developed.<\/p>\n

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