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uk.sci.weather (UK Weather) (uk.sci.weather) For the discussion of daily weather events, chiefly affecting the UK and adjacent parts of Europe, both past and predicted. The discussion is open to all, but contributions on a practical scientific level are encouraged. |
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#1
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I know Philip Eden has already mentioned it, but why and what has
caused the the Greenland High to be so dominant over the past 3 months? http://www.wetterzentrale.de/pics/bracka.html If only this was Winter, we may be in for some interesting cold weather. However in Summer it is just a spoiler. If this continues, people may stop talking about global warming and start talking about localised cooling! |
#2
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On Jul 8, 10:13*pm, Bonos Ego wrote:
I know Philip Eden has already mentioned it, but why and what has caused the the Greenland High to be so dominant over the past 3 months? http://www.wetterzentrale.de/pics/bracka.html If only this was Winter, we may be in for some interesting cold weather. However in Summer it is just a spoiler. If this continues, people may stop talking about global warming and start talking about localised cooling! If only anyone actually knew! And; if only anyone could have actually predicted its persistence and be confident of doing it again in the future!! Weather life would then be a much more forecastable place.....though perhaps much more boring too! Paul |
#3
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On Jul 8, 10:13 pm, Bonos Ego wrote:
I know Philip Eden has already mentioned it, but why and what has caused the the Greenland High to be so dominant over the past 3 months? http://www.wetterzentrale.de/pics/bracka.html If only this was Winter, we may be in for some interesting cold weather. However in Summer it is just a spoiler. If this continues, people may stop talking about global warming and start talking about localised cooling! With the Low ancillary n the North American side whilst we have a local low and a nearer Scandinavian one, snow is unlikely fopr us whilst Ice Storms or their summer solstice equivalents are likely for N. America. From: Stephen Wolfram, A New Kind of Science Notes for Chapter 8: Implications for Everyday Systems Section: The Growth of Crystals Page 992 History of snowflake studies. Rough sketches of snowflakes were published by Olaus Magnus of Uppsala around 1550. Johannes Kepler made more detailed pictures and identified hexagonal symmetry around 1611. Over the course of the next few centuries, following work by René Descartes, Robert Hooke and others, progressively more accurate pictures were made and correlations between weather conditions and snowflake forms were found. Thousands of photographs of snowflakes were taken by Wilson Bentley over the period 1884-1931. Beginning in 1932 an extensive study of snowflakes was made by Ukichiro Nakaya, who in 1936 also produced the first artificial snowflakes. Most of the fairly small amount of more recent work on snowflakes has been done as part of more general studies on dendritic crystal growth. Note that tree-like snowflakes are what make snow fluffy, while simple hexagons make it denser and more slippery. The proportion of different types of snowflakes is important in understanding phenomena such as avalanches. http://www.wolframscience.com/reference/notes/992h Might help explain the slushy stuff we are prone to. |
#4
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Forgot to mention the obvious:
While an adjacent Low and High to our north will provide a south flowing air mass (Winter's cold north winds) two Lows to our north will just make a mess. The cylone on the one side will have winds flowing opposite the way the cyclone on the other side is flowing. Strangely it might explain how it is that Highs and Lows don't cancel each other out. At least it indicates that twin cyclones or for that matter twin anticyclones will never form a perfect storm. As for the Perfect Storm: PHAH! |
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