Tag Archives: Weather

Wimbledon or Washout?

24 Jun

Wimbledon starts tomorrow! I love Wimbledon, or I should say, I used to love Wimbledon when it was filled with players like John McEnroe, Bjorn Borg, Jimmy Connors, Ivan Lendl, Boris Becker, Steffi Graph, Chris Everett and Martina Navaratalova! Yep, I’m showing my age a bit here, but looking back, I have fond memories of great matches involving the above players, exciting rallies and of course long hot summers…

When I look back at some of the matches, I must have been only 12, hard to believe, but my best memories of Wimbledon are from around that age until I was in my late twenties – so around 1995 I guess. By that time, most of the above players had played their last matches and my memories of the Wimbledon tournament are of newer but far less exciting players and matches – and bad weather!

The only benefit of the rained off matches is that sometimes the old classic games are shown on T.V!

The Wimbledon weather this year is looking distictively wet towards middle of the first week – no surprises there – which will mean the tournament going into three weeks possibly, so plenty of time to show old matches maybe? If not, I’ve dredged a few up from U-Tube anyway so in case you’ve all forgotten, you can see what I mean…

First off, some John McEnroe classic tantrums – not Wimbledon, but who cares?!

http://www.youtube.com/watch?v=YxAPKtOe0fQ

And;

http://www.youtube.com/watch?v=wcWNsS6wEps

What about the classic tie break with McEnroe and Borg in 1980?

http://www.youtube.com/watch?v=6qaweRhyAxk

Or this 1986 Becker and Lendl final;

http://www.youtube.com/watch?v=W1NcGiBCHDs

A lot of people say that the reason for those great rallies is because of the older wooden raquets the players used. The modern raquets just give too much speed, meaning the game is all about power shots, rather than exciting rallies, and this seems to be true. Ahh well, it’s a good job the older classic matches are still available to watch, especially on a rained off Wimbledon day.

Going back to the weather, i’ve discovered that not all is as bad as imagined. Here’s some weather facts;

Wimbledon weather facts

  • The warmest Wimbledon Championship on record was 1976, where temperatures averaged at 25.4 C.
  • In 1997, 118.3 mm of rain fell during the championships, making it the wettest Wimbledon on record.
  • Perhaps rather unfairly, Wimbledon has always been associated with bad weather and particularly with rain. But actually play has only been totally rained off 32 times in 125 years.
  • Most years, some rain does fall during the championships, however there have been seven years where rain did not interrupt play at all – 1931, 1976, 1977, 1993 and 1995, 2009 and 2010.

UK winner facts

Last British female singles winner – Virginia Wade 1977

Last British Male singles winner – Fred Perry 1936

So, If you get really bored when/if the tennis is rained off, then there’s always Robert Spire action-adventure thrillers TIPPING POINT, IMPACT POINT and to keep you entertained, or for anyone interested in the bad weather and climate, THE A-Z OF GLOBAL WARMING!

Enjoy the Wimbledon fortnight, and just remember – it used to be so much better, whatever the weather!

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Global Warming – A brief Introduction.

9 Sep

The term Global Warming has been in common usage for some time now and refers to recent warming of Earth’s atmosphere,which also implies a manmade or human influence.

Earth’s atmosphere comprises many gases: oxygen, nitrogen, carbon dioxide (hereafter abbreviated to CO2) and water vapour, to name a few. These gases are collectively called greenhouse gases and they keep the Earth’s temperature at a comfortable 15°C. Without them Earth would be a chilly -18°C.

Since pre-industrial times, usually taken to be before 1750, we know from ice-core records that CO2 levels were about 280 ppm,that’s 280 parts of CO2 per million parts of air. As industrialisation got underway humankind started to farm the land more intensely than ever before, which included deforestation for agriculture and settlements. Later – since about 1850 or so – the burning of fossil fuels for energy and transport has added considerably to greenhouse gas levels, particularly CO2.

This has resulted in CO2 levels increasing to about 390 ppm, a rise of about thirty-nine per cent from pre-industrial levels – mainly as a result of burning fossil fuels.

How do we know this?

Well, data from ice-core records that go back at least 650,000 years now show us that CO2 levels have fluctuated naturally during this time between 280 and 300 ppm. CO2 levels have also been measured accurately from the top of Mauna Loa Volcano in Hawaii since 1958, and results show an increase in CO2 levels from 315 ppm to 390 ppm since that time.

Therefore CO2 is now at ninety ppm more than it has been for at least 650,000 years of Earth’s history, and increasing. It is a known scientific fact that higher levels of greenhouse gases will lead to higher temperatures, which appears to be happening now. The world has warmed by an average of 0.74 degrees during the last 100 years or so. As a result of this warming, polar ice has started to decrease and melt, and so have Earth’s land-based glaciers. This in turn is causing sea levels to rise, which is putting low-lying islands at risk of flooding or total submersion, and will eventually threaten more and more of the world’s coastal cities and regions.

Things may get worse, however, because once Earth’s atmosphere starts to warm, the warming itself may cause further positive feedback mechanisms to kick in. A warmer atmosphere holds more water vapour, which is itself a powerful greenhouse gas. This will in turn cause further warming, and so on.

Melting ice results in more sunlight being absorbed by the surrounding ‘darker’ water and land, and that results in further warming, and more melting ice. Methane deposits currently held in a frozen but stable state under the sea and under the permafrost may be released as the oceans warm and permafrost melts, which will cause further warming. This is very worrying as methane is a potent greenhouse gas and around twenty times more powerful than CO2 when talking about it’s ability to warm the Earth’s atmosphere.

This is global warming in a nut shell, however there are of course far more complex issues involved as global warming will not affect the whole planet in the same way at the same time. Some parts will experience more drought, some parts more rainfall, and some parts more extreme weather such as floods and heatwaves.

One thing is for sure,as the world warms, we will all know about it…

For more information on the subject check out THE A-Z OF GLOBAL WARMING. Or visit my website SIROSSERTHRILLERS.