Hi Everybody!!

Hi Everybody!!
Welcome to my Hometown!!

Saturday, December 14, 2013

SHARING MY SNOW PHOTOS (A REAL OR IMAGINED PHOTO BLOG)



Hi Everybody!!
I am so excited with the Snow we are having this winter on this Blog. It is not cold as it is not real. In an old editing program on Picasa, I could add snow (and I did). That option is gone now. However, a new option has come in for the season. If you have your G+ Photo Albums set up, there is a new feature called G+Awesome AutoBackup. They copy some of your pics, add snow, twinkling lights or make quick clips as you have seen here. (If you do not like this, just x them out as your original is still intact). I just love having Snow because I have never had snow for real in this part of Texas.
 I am enjoying the Google Joy for the season and sharing the Google Joy with You!!!!!












link to photostudy:
https://plus.google.com/u/0/photos/117645114459863049265/albums/5685557805960719153/5685557812240089378?pid=5685557812240089378&oid=117645114459863049265




****NEW THIS SEASON FROM G+ AWESOME AUTO BACKUP:    SNOW!

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Let it Snow


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Let it Snow


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Let it Snow!

https://en.wikipedia.org/wiki/Snow


Snow

From Wikipedia, the free encyclopedia


Snow is precipitation in the form of flakes of crystalline water ice that falls from clouds. Since snow is composed of small ice particles, it is a granular material. It has an open and therefore soft structure, unless subjected to external pressureSnowflakes come in a variety of sizes and shapes. Types that fall in the form of a ball due to melting and refreezing, rather than a flake, are known as hailice pellets or snow grains.
The process of precipitating snow is called snowfall. Snowfall tends to form within regions of upward movement of air around a type of low-pressure system known as anextratropical cyclone. Snow can fall poleward of these systems' associated warm fronts and within their comma head precipitation patterns (called such due to the comma-like shape of the cloud and precipitation pattern around the poleward and west sides of extratropical cyclones). Where relatively warm water bodies are present, for example because of water evaporation from lakes, lake-effect snowfall becomes a concern downwind of the warm lakes within the cold cyclonic flow around the backside of extratropical cyclones. Lake-effect snowfall can be heavy locally. Thundersnow is possible within a cyclone's comma head and within lake effect precipitation bands. In mountainous areas, heavy snow is possible where upslope flow is maximized withinwindward sides of the terrain at elevation, if the atmosphere is cold enough. Snowfall amount and its related liquid equivalent precipitation amount are measured using a variety of different rain gauges.
See link for complete Article

Many Thanks to Google+ Awesome Auto Backup for adding twinkle lights to the Christmas Decorations!
A nice Glow-

Happy Holidays Everybody!
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From a couple of years ago! My edits in Picasa:











...this is brendasue signing off from Rainbow Creek.  See You next time! 
Keep on Snowing and Glowing!

https://plus.google.com/u/0/photos/117645114459863049265/albums/5677979690024516321

ps- yes I fell asleep and No-I do not work for Google (They work for Me!)
O+O