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January, 2005
Are we in for a cold spell?
Frozen pond by Dave Jonese Jackson
Frozen pond by Dave Jones

According to Look North weatherman Paul Hudson, despite daffodils being spotted, "winter may not be over yet"!

Are we going to be in for a cold one? Find out here...

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So far it's been a winter like we've grown accustomed to over the last few years - mild and with very few frosts, and little snow fall to speak of.

The three spells of 'wintry' weather, notably in November, Christmas day, and again for a time in January lasted no more the 48 hours, quickly replaced by milder Atlantic air. Indeed, it is the west or southwest winds blowing in from the Atlantic which have kept us so mild.

In fact it's been so mild that I received a picture from a Look North viewer in Lincolnshire in December showing his first daffodil! Since then I have had numerous picture, with daffodils in bloom across quite a few places by the end of January.

But it's also been a stormy spell of weather. During the early hours of Saturday January 8th a vicious area of low pressure tracked across the Borders, leading to gusts of wind of 85mph at Leeming, North Yorkshire.

Much of Yorkshire and Lincolnshire were battered by these winds, with structural damage and uprooted tress quite widespread. A second vigorous depression followed on the following Tuesday night - this brought heavy rain and severe gales again - but also a tidal surge down the East Coast.

The waves generated by the storm coincided with a high spring tide and an uplift of the sea due to the very low pressure of the storm system - 940mb - which lead to coastal flooding.

A third night of severe gales followed the next week, with gusts in Sheffield of 76mph, and 85mph at Pateley Bridge, causing more structural damage.

Interestingly as we end January, New England and the near continent are experiencing real winter, with heavy snow and bitterly cold air.

These two weather events are in fact linked by the upper air planetary wave, otherwise known as the Rossby wave. Effectively the upper air is behaving like someone is shaking a skipping rope. The Rossby wavelength is such that the cold trough of air over New England is followed by a warm ridge of air over the Atlantic, which in turn is followed by a cold trough of air over Europe.

Sometimes the wavelength is such that the cold trough falls over us; hence we hear people say that if it snows in New York, we will get it seven days later - this is not quite the old wives' tale people make out!

As we end January we are only just in the milder ridge - but interestingly the long range predictors for February are beginning to suggest that we may see some of the cold European air migrating westwards towards us.

Winter may not be done with yet!

Paul Hudson

Feel free to contact Paul by e-mail: look.north@bbc.co.uk.

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