TOPIC:

Hello Brett,
It seems to have gone now, the Met Office promises double figures by new years day, hussar and hurrah!
Kind regards Frank

Brett Hendey wrote: Frank, I watched the SkyNews reports this morning and hoped in vain to see your snow-covered house. (Sky often fails to cater for my expectations.) However, I was thinking of you in your latest tribulation. Here it is another 22 degrees and wet start to the day.

Regards
Brett

Frank

The Natal coast's "green drought" continues. There has been more than enough light rain to keep the vegetation green and growing, but not enough to raise the water tables, fill the rivers, and replenish the dams. Today has again dawned as cool (20 degrees) and wet, but it is still too soon to start building another Ark.

Regards
Brett

A "cool" 20 degrees, what an impossible dream for me at least!

Good Morning Frank......

When I woke up yesterday morning the temp was Minus 34 with wind chill and then a Chinook blew into town and last night when I went to bed it was Plus 6.......

Got to love those Chinooks......

Mike

A "chinook" Mike?

Frank Kelley wrote: A "chinook" Mike?

Here you go Frank......

Chinook

Chinook, warm, dry, gusty, westerly WIND that blows down the Rocky Mountains into the mountains' eastern slopes and the western prairies. The chinook, a native word meaning "snow eater," belongs to a family of winds experienced in many parts of the world where long mountain chains lie more or less at right angles to the prevailing wind.

Examples include the foehn in Europe, the zonda in Argentina and the berg in South Africa.

In Canada, the chinook belt lies almost exclusively within southern and central Alberta. The wind occurs in every season, but it is more distinctive and numerous in the winter, when the unseasonable warming it brings differentiates it from the normal cold winter weather. In southwestern Alberta, one in 3 winter days is a chinook day; its frequency drops to one in 5 in the northeast. The maximum daily temperature anomaly associated with the wind ranges from +13°C in the northwest to +25°C in the southeast.

The temperature rise at the onset of the event is abrupt and steep; an increase of 27°C in 2 minutes has been observed.

The warmth of the chinook is derived primarily from 2 nonmutually exclusive sources. Firstly, the replacement of arctic air (the mean temperature at Calgary's elevation is -24°C) by maritime air (-2°C) improves surface temperatures. Secondly, if the downslope flow occurs following a loss of moisture through precipitation on the windward side of the mountain, the heat used to change the water into vapour (latent heat) is returned to the air parcel and warms it. The downslope flow leeward of the mountain warms the wind further, reducing its relative humidity sometimes down to 25% or less. Wind speed ranges from 16 km/h to 60 km/h, gusting to 100 km/h.

The chinook melts snow, dries soil, desiccates vegetation and is a factor in soil erosion. Most people appreciate the chinook because it is a pleasant break from the frigid winter temperatures characteristic of the region. However, a significant minority complain of discomforts ranging from headaches and earaches to depression and attempted suicide.