Monday, January 14, 2008

Weather Break: Snow Where You'd Least Expect It

The following is a transcript of the Weather Break radio show for Monday, January 14, 2008. The episode was written by Dr. Jon Schrage.


Last week, a series of low pressure systems called “cyclones” dumped snow across much of the western United States. In some cases, it was a LOT of snow, with Kirkwood, CA reporting over 11 FEET of snow during these storms. Now, when most people think about CA, they are picturing warm beaches and deserts, but Kirkwood is northeast of San Francisco, just south of Lake Tahoe. It’s mountainous there, and as the moist air from the Pacific flows over the lee side of the mountains, the air is forced to rise, producing condensation that falls to the ground as snow at these high altitudes. In fact, the snowiest city in the US is Truckee, CA, which averages over 203 inches of snowfall a year—that’s almost 17 FEET of snow! Some of the ski resorts in CA actually have trouble staying open in particularly wet years because the snow gets so deep that chairs on the ski lift have to be dug out of the snowdrifts!

Of course, snowfall generally does become less common the farther south you go, simply because the average temperatures are increasing. However, snow can fall at high altitudes in the tropics, and along the equator itself there are even some examples of glaciers, where the snowpack doesn’t even melt in the summer!

In the tropics, just like other parts of the world, one of the major factors that control the climate is the altitude of a location. In general, the higher a location is, the colder its climate tends to be. The reason why this happens has to due with the fact that the heat and light from the sun tend to pass THROUGH the atmosphere without heating it. The light and heat from the sun reach the ground, heating the ground. In meteorology courses, we professors always need to remind our students that the sun heats the ground, not the atmosphere. The air is then heated by the ground, either by conduction or by radiation. On a mountain top, the sun can and does heat the ground itself, but the mountaintop is surrounded by air that may be thousands of heat above the ground in the valleys. Therefore, the mountain tops remain cold. In contrast, the valleys and the lower elevations have warm ground around them on all sides, heating the surrounding air. The results are warmer temperatures at the lower elevations.

A few tropical mountains receive considerable snowfall—sometimes enough snowfall that it doesn’t melt in the cool summer season, creating glaciers. Fans of Hemmingway will immediately think of his short story The Snows of Kilimanjaro. Mt. Kilimanjaro is a volcano and it’s the highest point in Africa. At over 19,000 feet, it’s one of the highest mountains in the world. It’s also just a few degrees south of the equator in the east African nation of Tanzania. Since that’s obviously a very tropical location, you might be surprised to realize that there are glaciers on Mt. Kilimanjaro. These glaciers, however, are rapidly receding, and they will probably be completely gone in the next few decades, according to researchers. The reasons for the retreating glaciers on Mt. Kilimanjaro are not completely clear, but it could be due to either warming temperatures or decreasing precipitation in the region.

Mt. Chimborazo is the highest point in the South American nation of Ecuador, rising to over 20,500 feet. At just more than 1° south of the equator, Mt. Chimborazo is covered with glaciers, whose annual meltwater is an important source of fresh drinking water in the relatively dry provinces of Ecuador. Just like in Africa, the glaciers of Mt. Chimborazo are retreating, although the reasons why are complex and include Global Warming, El Nino, and ashfall from nearby volcanoes.

Indonesia is the nation made up of over 17,000 islands north of Australia. While most of these islands are very small, the island of New Guinea is the world’s second largest island, with about twice the area of the state of California. New Guinea is extremely tropical, with lush rain forests at low elevations. However, some of the mountains on New Guinea are more than 16,000 feet high, and they receive enough snow to form permanent glaciers as well.

Whether tropical or from a higher latitude, almost all glaciers on earth are currently retreating. It’s a matter of some debate in scientific communities about whether or not this is attributable to Global Warming. A delicate balance of precipitation and melting is necessary to maintain a glacier, and studying these factors and their role in climate is the work of a branch of earth science known as glaciology.

Friday, January 4, 2008

Getting Ready for ATS 113!

Hello, ATS 113 students!

As you may know, the ATS 113 course uses a lot of electronic resources, like websites and course CD. Rather than spend a bunch of time on the first day of class trying to make sure that everyone understands what's going on, it seems like a better idea to do this using the course blog this year.

Course CD. I'm currently putting the final touches on the course CD, so it will definitely be ready by the first day of class. Every student is required to have a copy of the course CD. However, you are under no obligation to BUY the CD; you can borrow a friend's copy, or you can check the CD out from the library. If you choose to buy the CD, I'll bring a bunch of copies to class on the first day and they are $5 each. (The proceeds from the sale of the CD go to Weather Break, Creighton's daily radio program about weather, climate and the environment.) You can run the CD directly, or there are installation instructions with the CD that will help you copy the disk to your hard drive, which will result in much smoother performance.

What kind of stuff is on the course CD?
  • Outlines of every lecture. (These are not NOTES; they are outlines.)
  • Many of the figures and handouts for each lecture.
  • A daily video called the "Reading Coach". On each Reading Coach video, I walk you through that day's assigned readings, pointing out the most important (and least important) parts of the reading.
  • Several dozen short videos produced here at Creighton for use in ATS 113.
  • Many PowerPoint files and related materials.
  • And much more!

Course Website. This course has a website that is maintained in two convenient locations. You can either access the course at ats113.com, or you can use Blueline. The same content is available on both sites, although grades are only available on Blueline this year.

What kind of stuff is available on the course websites?
  • All of the daily outlines and the Reading Coach videos.
  • Most of the PowerPoint files and related materials.
  • All "news" and "announcements".
In other words, the course websites have largely the same content as the course CD. However, because of possible copyright conflicts, many of the images on the website have been disabled; those resources are only available on the course CD.

Course Wiki. Electronic participation is a small but important part of your total grade in ATS 113. One of the ways in which many students choose to participate electronically in the course is to add to the course wiki. I'm guessing that most of you know what a wiki is; wikis are made of web pages that users can modify. We maintain two kinds of course wikis in this class:
  • "Group Lecture Notes Wikis" are written by students based on their notes from the lecture.
  • "Group Reading Notes Wikis" are similar, but they are based on the readings from each day.
Now, maybe YOU will NEVER contribute to the Wikis, and that's okay (maybe you'll get your participation points some other way, as we'll discuss in class). But even if you don't ADD to the wikis, you'll want to be able to ACCESS them, because they will be a good source of notes and information before each test.

Blueline has the ability to make wikis, but they don't work very well, so we are going to be using a different piece of software called "Moodle". Our "Moodle Server" is called "stratocumul.us". If you navigate to http://stratocumul.us, you'll be able to create an account there. Play-by-play instructions about how to create this account are available by watching this video.

Online Participation. A total of 5% of your grade comes from your "online participation" in the course. There are a number of ways to participate online. Probably the best way for you to learn about this is to watch this video.

Okay, I hope that I haven't "overwhelmed" you! I think that you'll find that this stuff turns out to be a lot of fun. See you on the 10th!

Monday, October 9, 2006

Folies Bergere Continues To Be A Must-See: Old Vegas So Retro It Is New Again

Local Review-Journal writer Mike Weatherford writes in
this article:

You can't pump significant money into the Strip's longest-running show because the casino is widely acknowledged to be on borrowed time after a bidding war for owner Aztar Corp. Either an implosion or a significant remodeling could drop the curtain on the classic showgirl revue that has been around since 1959.

But you can't just let it go either. Customers can sense when a show has been allowed to slide into stagnation. Note last Saturday's closing of the 21-year-old "Splash, which offered too little too late with a sketchy overhaul last year.

So what do you do?

What you do is simply go see this show. A little bit classic Las Vegas, sexy topless production numbers with beautiful Las Vegas showgirls, and a reasonable price in a day that $100-plus tickets are the norm make this a fun time. And one that might not be around much longer.

When you think of Las Vegas entertainment, what do you think of? Lasers and tigers? No. You think of showgirls. They are in our movies, commercials, and surround the winners here whether it be a golf tournament, NASCAR race, or big jackpot winner. Folies Bergere has been presenting some of the best before James Bond or Elvis became synonymous with Las Vegas.

Folies is a true celebration of the showgirls and dance throughout the ages with a stunning display of fantasy and light. Opening scenes highlight the entire cast in song and dance with bits of real feathers flying around in the air.

Still undecided? Check out these Folies Bergere Las Vegas photos then check out Folis Bergere ticket info.

Recent Las Vegas related blog posts by Ted Newkirk: