Saturday, November 03, 2007

Indtryk efter 4 dage

Børnene og jeg har været på Cayman i 4 dage.

Vi har endnu ikke set så meget af øen, da vi lige har skulle vænne os til tidsforskellen. Ungerne eller især Christoffer har svært ved at omstille sig. Han vågnede kl. halv 2 i forgårs og imorges kl. halv 5, så der er da fremgang.

Igår var vi ude og se skolen hvor Tobias skal gå. Det er almindeligt at skoler og institutioner er tilknyttet en kirke. Ifølge Jasper, som har været rundt at se en del af dem, var der kun en institution, som ikke lagde vægt på religion (kristendommen) og den var der ikke plads i. Det er svært at vænne sig til at religion, er så almindelig en del af samfundet og det at tale om gud osv. er som man taler om pædagogik. I den forbindelse kan jeg fortælle, at den første jeg har mødt her (Patricia) er barnepige og rengøringsdame for underboen. Hun er fra Jamaica og har 4 børn (som stadigvæk er på Jamaica). Hun beundre vores underboer meget for deres stærke tilknytning til kirken og deres store kærlighed til guds hus osv.

Mit umiddelbare indtryk med kun 4 dage på øen er, at det ville være svært at bosætte sig med en anden religiøs baggrund, ikke fordi folk ikke er tolerante, men fordi folk med anden religiøs baggrund måske ikke ville være interesseret i at deres børn igennem skolen bliver opdraget i den kristne tro. Jeg har lige siddet og læst skolens håndbog som bl.a. i forordet skriver:

....becoming totally committed to Christ and His way, ...will help each child to develop his/her full potential, and fulfill his/her God-given pupose.
Skolens motto er:

To grow..in wisdom, and stature, an din favor with god and man.

Ja, det er lidt en anden stil end i DK.

Tuesday, October 23, 2007

High School Physics

This made me laugh and reminded me of Physics in high school (not that I provided any creative solutions).

Saturday, October 20, 2007

The healthy alternative?

A couple of days ago the Freakonomics blog posted on bicycling safety:

Per kilometer, cyclists are 12 times more likely than car drivers to suffer a fatal accident, according to Rutgers University urban planner John Pucher and Lewis Dijkstra of the European Commission (the same study found traveling by foot to be 23 times more dangerous than driving, per kilometer). To put this finding in perspective, there were 785 bicycling fatalities on American roadways in 2005, compared to 4,881 pedestrian and 43,443 automotive fatalities that same year.

On the other hand, a Danish study found that people who do not bike to work suffer a 39 percent higher mortality rate than those who do. So, assuming you can avoid a fatal accident on the road, biking to work may actually help you live longer.

The risks associated with cycling decrease dramatically when more cyclists are on the road, and especially when those cyclists obey traffic laws...

I cycle often here in Cayman, and I can tell you, it is not for everyone. There are no cycle paths and roads are sometimes very narrow. Many of the local cyclists are also fairly reckless and often don't follow normal traffic rules. My experience, however, is that signaling and taking care to obey traffic laws, earns respect from the motorists, making it much less of a hazardous experience. Had it not been for the heat and humidity, I am sure far more people would cycle to work. The distances here in Cayman are relatively short. But most people prefer their air-conditioned SUVs. Go figure.

To read the Freakonomics post, click here. It contains links to the studies mentioned above.

Monday, October 15, 2007

Build Up #1

Sunday I got early for a build up triathlon event - not to participate (still lacking my tri bike), but to help out and meet some of the people from the Cayman Islands Triathlon Association.

See some pictures from the event here and get an impression of what it was like. There are not many picture of me, but if you do manage to find me you will see I am wearing a white cap, black shorts and a grey t-shirt (and holding a water bottle). There will be two more build up events before the olympic distance triathlon late November.

Wednesday, October 10, 2007

Ironman Triathlon World Championships

Lately, I have been giving some thought to triathlon training and my goals. One event I am very keen on doing is the Ironman World Championships in Kona Hawaii. The race encompasses a 2.4 mile (3.86 km) ocean swim in Kailua-Kona Bay, followed by a 112 mile (180.2 km) bike ride in the Hawaiian lava desert and ending with a marathon (42.195 km) along the coast. The event is coming-up this weekend so keep your eye out for media coverage.

Hawaii was host to the first Ironman Triathlon in 1978. If you have triathlon ambitions, Kona is definitely on the list of races you want to participate in. Entrance to Kona is on a qualification only basis. Here there are two main options, a lottery or to participate in a race that allocates slots to Kona.

Of course you could rely on pot luck, but since you want to complete the damn thing and do so in a reasonable time, you might as well try and estimate what the qualification requirements might be. This turns out to be a difficult task because of the way the system works. Luckily there are people out there like Neil Hammond who posted his analysis of qualification times on the internet. Now, Hammond's analysis is far from perfect, but it gives results that seem plausible to me. Indeed by using his analysis I cross-checked my initial thinking and came to more or less the same result.

Without making things too complicated these are the type of times I would need to qualify in the 35-39 age group (+/- 5%). 1:15 for the swim, 5:20 for the bike ride and 3:40 for the run. This adds up to 10:15, add to that 10 minutes in transition and my qualifying time is just under 10.5 hours. +/- 5% gives me a qualifying interval of roughly 10 - 11 hours. Is that possible? I certainly believe it is. Swimming 3.8 km in 1:15 should be fairly easy not least because it is in the beginning of the race. 180 km in 5:20 is just under 34 km/h. While my legs would not be able to cope with that currently, because I haven’t trained on the distance, that can be rectified with purposeful training. The part of the race that causes me most worry is the marathon. I am not sure how my legs or indeed body will react. I got a taste during the Brisbane marathon, but that was without more than 6 hours psychical exertion prior to start. However, as long as I can keep my legs running 3:40 should be possible.

Here are some stats from Kona for a comparison:

2006 WINNERS:
Normann Stadler - S 54:05, B 4:18:23, R 2:55:03, Total 8:11:56
Michellie Jones - S 54:29, B 5:06:09, R 3:13:08, Total 9:18:31

COURSE RECORDS:
1996 – Luc Van Lierde (BEL) 8:04:08
1992 – Paula Newby-Fraser (ZIM) 8:55:28

FASTEST COURSE TIMES:
Swim
1998 – Lars Jorgensen (USA) – 46:41
1999 – Jodi Jackson (USA) – 48:43
Bike
2006 – Normann Stadler (GER) – 4:18:23
1993 – Paula Newby-Fraser (ZIM) – 4:48:30
Run
1989 – Mark Allen (USA) – 2:40:04
1999 – Lori Bowden (CAN) – 2:59:16

I would of course not compete with the elite but in the age groups. The men’s division records are:

Age Record Name Age Year
18-24 8:55:02 Vassilis Krommidas 24 1994
25-29 8:41:02 Maximilian Longree 25 2006
30-34 8:45:59 Igor Kogoj 34 1993
35-39 8:47:02 Jim Beuselinck 39 2006
40-44 8:58:55 Bent Andersen 42 2006
45-49 9:11:56 Brian Keast 45 2005
50-54 9:26:23 Kevin Moats 51 2006
55-59 9:47:29 Reinhold Humbold 57 2005
60-64 10:40:49 Takahisa Mitsumori 62 2005
65-69 11:29:45 Milos Kostic 65 2006
70-74 12:59:02 Bob Scott 71 2001
75-79 13:27:50 Bob Scott 75 2005
80+ 16:21:55 Robert McKeague 80 2005

Robert McKeague is amazing. 80 years old and doing an Ironman. I wonder if Bob Scott will try to beat his record in 2010.

First things first though. Step one is to successfully complete the distance, if that can result in qualification to Kona that would be exceptional, but more likely a second attempt will be necessary. My timeframe is 3 years.

Anyway, you don’t get any faster writing blogs. Better to do some training instead! This video provides some good motivation.

Friday, October 05, 2007

Map of Internet

Ever seen a map of the internet? The Chris Harrison project has created a series of maps that show the geographical structure and distribution of the Internet.

Thursday, October 04, 2007

South Sound Run

In a previous post I mentioned MapMyRun.com. The website enables users are to visualize their training progress through the use of maps, workout logs, fitness calculators/tools etc. Personally, I just use it to set distance markers and because it gives me a good overview of the course.

I have added my latest run to the webiste, click here. Note that you will have to turn on the satellite image to better appreciate the run. Google does not have road maps covering Grand Cayman. The run starts and ends at where we live.

Negative feedback

This issue of melting ice caps and global warming continues to worry me. Recent changes to the Artic and ices of Greenland are of particular concern. It seems to me that changes to our planet induced by melting ice might be one of most costly and yet still underappreciated factors in the global warming debate. A recent report in the NY times, emphasizing the role of vicious circles or negative feedback, provides some more food for thought:

Each summer over the past six years, global warming has trimmed this ice’s total area a little more, and each winter the ice’s recovery has been a little less robust. These trends alarmed climate scientists, but most thought that sea ice wouldn’t disappear completely in the Arctic summer before 2040 at the earliest.

But this past summer sent scientists scrambling to redo their estimates. Week by week, the National Snow and Ice Data Center in Boulder, Colo., reported the trend: from 2.23 million square miles of ice remaining on Aug. 8 to 1.6 million square miles on Sept. 16, an astonishing drop from the previous low of 2.05 million square miles, reached in 2005.

The loss of Arctic sea ice won’t be the last abrupt change in earth’s climate, because of feedbacks. One of the climate’s most important destabilizing feedbacks involves Arctic ice. It works like this: our release of carbon dioxide and other greenhouse gases around the planet causes some initial warming that melts some ice. Melting ice leaves behind open ocean water that has a much lower reflectivity (or albedo) than that of ice. Open ocean water absorbs about 80 percent more solar radiation than sea ice does. And so as the sun warms the ocean, even more ice melts, in a vicious circle. This ice-albedo feedback is one of the main reasons warming is happening far faster in the high north, where there are vast stretches of sea ice, than anywhere else on Earth.

There are other destabilizing feedbacks in the carbon cycle that involve the oceans. Each year, the oceans absorb about half the carbon dioxide that humans emit into the atmosphere. But as oceans warm, they will absorb less carbon dioxide, partly because the gas dissolves less readily in warmer water, and partly because warming will reduce the mixing between deep and surface waters that provides nutrients to plankton that absorb carbon dioxide. And when oceans take up less carbon dioxide, warming worsens.

Scientists have done a good job incorporating some feedbacks into their climate models, especially those, like the ice-albedo feedback, that operate directly on the temperature of air or water. But they haven’t incorporated as well feedbacks that operate on the atmosphere’s concentrations of greenhouse gases or that affect the cycle of carbon among air, land, oceans and organisms. Yet these may be the most important feedbacks of all.

Read the rest of the article here.

Saturday, September 29, 2007

Hazards

The other day at work a colleague mentioned in passing the possibility of earthquakes here in the Caymans. What ?!! was my reaction. But he asserted me we live in an area prone to volcanic activity. That made me ponder what kind natural hazards I was exposing myself and my family to, by living in this region of the world. Based on a look at various websites, I came up with the following four major hazards: earthquakes, volcanoes, tsunamis and hurricanes.

Earthquakes, volcanoes and tsunamis enjoy a common father: the movement of tectonic plates. Grand Cayman lies on the plate boundary between the North American and Caribbean plates (see image), next to the Cayman Trough (or Trench).

The tectonic plates in Cayman’s region are in continuous lateral movement against each other, with the Caribbean plate traveling east at approx. 20 mm a year. The lateral movement limits the size of earthquakes in this area. However, in December 2004 a quake of 6.8 magnitude rocked Grand Cayman - there was no major damage though.

The following image shows the Cayman Trough together with an indication of Caribbean plate boundaries. The Trough has a maximum depth of 7,686 meters.

The depth of the Trough is more easily seen in the image below. It provides a perspective view of the sea floor of the Atlantic Ocean and the Caribbean Sea. Florida is on the upper right. The purple sea floor at the bottom center of the view is the Puerto Rico trench, the deepest part of the Atlantic Ocean. At the top of the image and to the left of Cuba you can see the Cayman Trench and what looks like small mountains. The top of the mountains are the Cayman islands - the realisation that we are on top of massive underwater mountains in the middle of nowhere made me feel small and vulnerable.

Along the northern east part of the Caribbean plate, including areas in the vicinity of Jamaica and the Virgin Islands, moderate earthquakes of shallow depth are generated. In the Eastern Caribbean seismic events are common and principally associated with a subduction zone at the junction of the Caribbean Plate and the North American Plate. The North American Plate slides underneath the Caribbean Plate along a north-south line just east of the arc of Caribbean islands.

Several of the islands of the Eastern Caribbean are volcanic in origin. Grenada even has a submarine volcano called Kick 'em Jenny. Studies dating back to 1972 indicate that minor eruptions have been occurring on a fairly regular basis and that the summit of the volcano is growing at a rate of approximately 4 metres per annum.

To conclude, on a hazard rating of 1 to 10 for Cayman: volcanoes = 0, earthquakes = 2.

So what about the possibility of a tsunami? The majority of tsunamis are related to tectonic displacements associated with earthquakes at plate boundaries. However, tsunamis can also be generated by erupting volcanos, landslides or underwater explosions (and meteorites). For islands in the vicinity of Kick’em Jenny that is bad news.

Grand Cayman has large boulders on its south coast that geologists believe were moved from the seabed to land by a tsunami. Carbon-dating of dead sea-plants on the rocks put the event in 1662 plus-or-minus 25 years. That time-period comes close to including the 1692 earthquake and the event-generated tsunami and landslide that killed over 2,000 in Port Royal, Jamaica. However geologists believe that Grand Cayman's rocks were moved by an even greater event.

For us in the Cayman, I doubt tsunamis pose a significant threat. It seems to me that possible movements in the Cayman trench are at a depth and of a type (horizontal not vertical movement) that would be unlikely to create a tsunami. My hazard rating: tsunami = 1.

Finally, we have hurricanes which name is derived from the Mayan storm god Hunraken and the Arawak (Amerindians encountered by the Spanish explorers) word hurican, which meant the devil wind. As I noted in a previous post one of the greatest of all recorded hurricanes occurred in October 1780. Nearly 20,000 people perished. Warmer waters also increase their intensity.

Here in Grand Cayman, hurricane Ivan (two years ago) caused massive damage. Damage which is still evident today. Apart from strong winds and flying debris, one of the major contributors to damage was the surge of water, flooding almost all parts of the low-lying island. I would say the likelihood a direct hit by a hurricane is substantial. My hazard rating: hurricane = 8.

Writing about hurricanes reminds me of an article I read in the local newspaper a few weeks ago. It was on the (economic) cost of hurricanes. It is pretty obvious that people who live in hurricane prone areas must expect to incur additional costs to protect themselves. Building construction needs to be of a higher grade, insurance is more expensive, etc. However, one thing I had not thought about (which in retrospect seems obvious) is the cost to businesses of having emergency hurricane disaster plans in place and the cost of acting upon these plans in the event of a possible hurricane event. Think of staff evacuation, additional back-up options for data, standby office space off shore etc. When hurricane Dean passed south of Cayman with no consequence whatsoever a month ago, most firms engaged their pre-hurricane disaster plans. While some incurred little cost, some sent all staff off island at considerable expense.

Monday, September 24, 2007

Sting rays miles apart

Below is the Stingray Nebula captured by the Hubble Space Telescope (image from NASA). The bright central star is in the middle of the green ring of gas. Its companion star is diagonally above it at 10 o'clock. The colors shown are actual colors emitted by nitrogen (red), oxygen (green) and hydrogen (blue). The nebula is as large as 130 solar systems and at a distance of 18,000 light-years.
Much closer is Stingray City here in Grand Cayman. It is located in the shallow waters east of the northwest corner of Grand Cayman. According to local legend stingrays began gathering in the area many years ago when fisherman would clean their catch in the calm water of the shallows and sand bar area. Over time the stingrays began to associate the sound of a boat engine with a free meal. Not unsurpringly: friendly sting rays = major tourist attraction.
I should note that sting rays can be seen all around Grand Cayman. The other day while swimming just 20 meters off shore and no more than 200 meters from where we live, a sting ray passed under me.

Friday, September 21, 2007

RS800 Polar

A couple of days ago I received a product update from Polar (the company that makes heart rate monitors). Around two years ago I upgraded to a new polar heart rate monitor. At the time I did some research into the different options. It was clear that GPS was finding its way into distance and speed measurement. But the units were a bit too bulky for my liking. There was also the issue that I had an Ipod shuffle strapped to my left arm when running and the thought of having a device on the other arm simply didn't appeal to me (nowadays the Ipod is hidden in my back short pocket). When I read that Polar had added what they called a G3 GPS sensor to their RS800 training system I was hoping for a cool new innovation.


Nope... Polar has opted for the arm strap solution. Disappointing. Had they produced a heart rate monitor with in-built GPS, instead of a separate unit, I would have been first in line to buy one. See the RS 800 here. I am guessing it is still too costly or difficult to add a GPS unit to a wristwatch without changing size and appearance siginificantly.

Tuesday, September 18, 2007

NW Passage

In a previous post I mentioned the Artic Northwest passage being open. Today I came across an article from the ESA (click here). Apparently the area covered by sea ice in the Arctic has shrunk to its lowest level this week since satellite measurements began nearly 30 years ago.


The ESA has created a mosaic using radar equipment aboard their Envisat satellite. The image is created from nearly 200 images acquired in early September 2007. The Northwest Passage is the orange line and the Northeast passage (partially blocked) is the blue line. The dark gray colour represents the ice-free areas, while green represents areas with sea ice.
UPDATE: Below is a picture from the NASA observatory which more clearly shows what is going on. The graph of sea ice melt shows the five-day mean sea ice extent for June through September. It compares values from 2007 with those from 2005 and the average (1979-2000).

Sunday, September 16, 2007

A devine morning

Today I went to church!

Those who know me may be surprised, because this not something I do very often. The people who live downstairs had invited to me to go along to see the school that is affiliated with the church.

I am currently trying to find a school for Tobias. Here in Cayman every school I have seen so far has an affiliation of some kind to a Christian church or a Christian movement. In this case it was a Baptist church. Other denomination of the Christianity on the island include Anglican, Catholicism, Church of God and Presbyterian.

Arriving there at 9.15 am, I was taken on a brief tour of the school. Nothing much to say about the school grounds - everything looked fine. Then I was placed in discussion class. The subject: the Book of Daniel (chapter 3). For more devoted Christians this is probably a well-known story, but for me it was all new. I guess I could have heard the story as a child, but it is certainly not something I remember. Anyway it is the story of three Hebrews Shadrach, Meshach and Abednego who defy King Nebuchadnezzar's order to bow down and worship a huge golden idol (9 stories high). As a result Nebuchadnezzar throws them into a fiery furnace (likely used when building the idol), but they are miraculously unharmed by the flames. Nebuchadnezzar sees them walking around in the furnace along with an unnamed fourth figure. When they emerge, Nebuchadnezzar orders everyone to worship their god instead of the idol. The fourth figure (who did not emerge) was the Son of God or a least that's who Nebuchadnezzar thought it was.

The story was discussed for a hour. I kept my quite, only listening. Suffice to say, discussion of Christianity is not something I do very often and I felt very much like an outsider. There was some interesting discussion though, some of which I could relate not to Christianity but to game theory and strategic interaction on the part of the Hebrews and the king.

After discussion class it was time for church. Compared to the church on Ærø where I would normally go Christmas eve, this was all high tech. Power-point presentations running lyrics to the hymns on two huge screens and top of the line sound equipment. Compare this with hymns idenified by a number listed on boards. There was a band consisting of keyboard player, drummer and guitarist. Compare with a mechanical organ. Cushioned seats vs. antic wooden benches… you get the picture. However, once the initial fascination with the physical elements subsided, it was frankly not a service that appealed very much to me. But the same is often the case in Danish churches.

Churches seem to play an extremely significant role in Caymanian society. It is evident when walking the streets on Sunday. Many native Caymanians are churchgoers. Indeed it would appear that the churches are more than religious centres - they are also community centers serving as a basis for a variety of activities.

On http://www.caymanchurches.com/ I counted 35 churches - a pretty significant amount for a population of about 45,000, of which just under half are Caymanian residents and the rest expatriates.

By the way, I met the Principal of the school after church and she me invited me for a tour on a normal everyday school day. No doubt a much better way to evaluate the school than on a Sunday morning.

Wednesday, September 12, 2007

48 years ago today....

...the Soviet Union launched The Sputnik-like probe "Luna 2" from the Baikonur Cosmodrome. It took 33.5 hours to reach its destination the moon. The first man-made object to hit the lunar satellite. More info on the Luna Missions here.

UPDATE: Of course, also a very appropriate day for Google to launch the Lunar X Prize, a competition that will award US$20 million to the first team that lands a private unmanned spacecraft on the moon and broadcasts high-definition video back to earth.

Sunday, September 09, 2007

Summer Games

This summer Tobias has been playing with new games and toys. Two in particular have dominated: Bionicle and Yu-Gi-Oh. While Bionicle are a series of robotic monsters that need assembly upon purchase (in typical Lego fashion), Yu-Gi-Oh is a card game. While they don’t at first sight seem to have anything in common, they both make use of myths and legends and involve battles of good against evil. In my opinion, Tobias is still a little young to play with them, but he seems to enjoy both nonetheless.

Both have complicated storyboards that (at least for adults) require study to appreciate. I myself have not taken the time to understand the different worlds these games or toys develop. However, with some time to spare, I decided to spend a few hours taking a closer look. Here is the result - basically a summary of publicly available sources on the internet spiced-up with my own experience playing with Tobias. Note that I feel like I have only scratched the surface.

Let’s start with Bionicle.

My initial searches on the Lego website were rather confusing. However, in retrospect this confusion was derived from my lack of knowledge of the Bionicle background. To start at square one, the storyline begins as follows….

In the time before time, the island of Mata Nui was a tropical paradise. The villagers, called Matoran, and their elders who lead the villages, the Turaga, lived in peace. That was before the Makuta came. Dark brother of the spirit Mata Nui, the Makuta quickly engulfed the island in evil. Matoran and Turaga inhabitants had almost lost hope in the legends handed down over the years.... legends that told of the coming of six mighty heroes, the Toa, who would free the island of terror. And then, on one unsuspecting day six large canisters washed up on the shores of Mata Nui. Inside the canisters lay the saviors of the island, the Toa.

Each of the six Toa had a special ability to control an element of nature. Tahu was the unspoken leader of the Toa who controlled the element of fire. The solitary Kopaka controlled ice. Clumsy footed Lewa was Toa of the air. Gali the Toa of water was the only female Toa. Onua, Toa of Earth, was as wise as he was strong. And the sluggish Toa of stone Pohatu used his large feet to kick boulders great distances.The Toa knew what was required of them: defeat the evil that terrorized the island. They also knew that they could not tackle that quest without the aid of six Great Masks of Power, called Kanohi.

And so begins the adventures of the Toa (the Māori word for "champion"), their first quest, to search for the Kanohi masks. This was all back in 2001, when Bionicle was first introduced. In their latest adventure (at the time of writing) the Toa (now called Toa Mahri) are undersea warriors. The Great Spirit Mata Nui is dying (remember this was the also the name of the island - not sure why the island and spirit have the same name), and only the so called Mask of Life can save the spirit and the universe. The Toa’s quest is therefore to find the mask which is beneath the sea.

Beneath the waves, the Toa discover the sunken city of Mahri Nui and its Matoran inhabitants. The villagers are caught up in a desperate battle for survival against the mutated Barraki and their armies of sea creatures. Of course the Barraki have the Mask of Life in their possession. It is the Barraki and Toa Mahri that Tobias has collected.

Building the Bionicle characters is straightforward for adults, but a challenge for children Tobias age. Tobias and his cousin Niels (both 5) managed to build one the characters almost entirely by themselves. They are also great for different poses. All major joints (ankle, knee, hip, arm, head etc.) are movable.

Lego has come far since I was a kid. Although the good old fashioned Lego is still, in my opinion, superior to these new "biomechanical" beings.

Now for a look at Yu-Gi-Oh.

As mentioned earlier Yu-Gi-Oh is a card game. It is based around a boy named Yugi who learns of an ancient Egyptian card fighting game called "Duel Monsters". Playing the game Yugi solves the secret of an ancient puzzle (the Millennium Puzzle) and releases the spirit of an Egyptian King, Yami Yugi. With help from the King's spirit, Yugi sets out to become King of the Duelists (or Yu-Gi-Oh! - King of Games).

The game is played with three types of cards: Monster Cards, Trap Cards and Magic Cards. Monster cards are used to attack or defend. Each monster has an attribute indicated by a symbol on the top right corner of its card. There are 6 attributes in all (earth, water, fire, wind, light, dark). The type of monster and its attribute determine its ability to attack or defend. Each monster has a predetermined number of Attack and Defend points. Magic Cards have a wide range of magical abilities. Some make monsters stronger or weaker while others may alter the conditions of the battle field. Trap cards are literally traps that can be activated after your opponents turn.

Tobias is especially fascinated by three cards: The Egyptian Gods: Slifer the Sky Dragon, Obelisk the Tormentor and Winged Dragon of Ra. The three Egyptian Gods combine to form the omnipotent Creator of Light - Harakhti.

We haven’t actually played with the original Yu-Gi-Oh cards. Tobias has drawn 30 different cards each with different abilities. As creator of his own game, playing with him can at times be very difficult as he has a tendency to manipulate the cards and monsters to his liking and to detriment of his opponent. If he continues to find these card games interesting we might have to buy him a real set.

Thursday, September 06, 2007

Storm of 1780

I am currently reading a book on the history of the Caribbean. To follow-up from the previous post where I briefly mentioned hurricanes, there is an account in the book of a hurricane that passed over the region in October 1780. During its passage, it killed well over 22,000 people and totally destroyed large British and French naval fleets as well as hundreds of merchant ships. Back then there were no instruments to measure the force of the hurricane, but maximum wind gusts are thought have exceeded 300 km per hour since raindrops stripped the trees of their bark!

Tuesday, September 04, 2007

Back in the Caymans

I am back in the Caymans, having accepted the job offer from the Information, Communications and Technology Authority (ICTA). I have been given a week to sought out all tasks related to a move abroad: accommodation, schools, banking etc. So far I have opened a bank account and found a place to live. The apartment is located in the George Town area close to schools and work. It has a sea view and direct access to the sea and a beach half a block away. The Google Earth coordinates are: lat=19.2784135251, lon=-81.3917586815

As I write this post there is a thunder storm passing overhead. The last couple of days I have been watching the developments of hurricane Felix. It passed way south of Cayman as expected. The people here didn’t make any fuss at all. With hurricane Dean a few weeks ago, however, it is my understanding that some areas were vacated and people prepared themselves for a hit.

The potential for a hurricane passing over the Caymans has influenced me in some of my tasks this week. For example, when renting a house, a two story is recommended. During hurricane Ivan (three years ago), the island was nearly covered in sea water. A quarter or more of the buildings on the islands were reported to be uninhabitable, with 85% damaged to some extent. A second story can keep you dry. Another example, is my choice of car. During Ivan almost all cars were covered in sea water, ruining car engines. Obviously, I don’t intend to buy an amphibious vehicle, but through private purchase there is a risk of buying an Ivan infected car. As a person with very little understanding of car mechanics, this has narrowed my car search efforts to car dealers.

The prospects of a hurricane passing over the island both scares and fascinates me. Currently, we in the midst of the Atlantic hurricane season. The figure below illustrates the Atlantic hurricane season with over 97% of tropical activity within the period of 1 June to 30 November.
There is evidence that the global warming might be making the storms stronger (not increasing their number). In addition, global warming may also be causing sea levels to rise. The Northwest Passage is now open (connecting the Atlantic and Pacific Oceans) and melting polar ice and glaciers may cause a rise in global sea levels - something that should be a major concern for Caymanians. Cayman Islands is very low lying and I suspect a rise of only a few meters could have disastrous effects.

Sunday, July 08, 2007

Flying and Delays

As I write this post I am in Heathrow Airport waiting for my final connection to Copenhagen. It is currently 1 hour and 10 minutes delayed. I need to catch a train with a connection to Ærø at 4.40 pm. Expected arrival in Copenhagen is presently 4.25 pm. The alternative is a three hour wait for the next scheduled ferry.

There have been several delays during my roundtrip to Cayman - more than I’m normally accustomed too. My flight out of Copenhagen (to London) was delayed an hour. Add to that an hour to find our luggage which had mysteriously disappeared. With the shuttle service closed for the day, a taxi was the only transportation option. However, with a massive queue outside Terminal 3 and one taxi arriving every 2-3 minutes, I faced the prospect of waiting more than an hour. I decided to try Terminal 2. Luckily, the queue there was much smaller and within 10 minutes I was on my way to the hotel. I arrived a quarter past midnight - delayed two and half hours and utterly wasted.

It is surprising that a large international airport like Heathrow is not better equipped to deal with transport issues late at night. The Heathrow express does operate at this hour, but is not very helpful if you are going to hotel in the vicinity of Heathrow. The key lesson to learn is either to avoid Heathrow after 10.30 pm or find a hotel at the end of the Heathrow Express line. And if you find yourself in a massive taxi queue try one of the other terminals.

The flight out of Heathrow the next morning to Cayman (via Nassau) was also delayed, although with no real consequence as Cayman was my final destination. Leaving Cayman yesterday morning, however, was different story. I was still trying to check-in when my flight was scheduled to depart. Technical difficulties at the check-in counter made turnaround impossibly slow. Nevertheless, we managed to make up most of the time before our arrival at Heathrow. With an ongoing connection to Copenhagen I was of course very pleased with this development. However, my excitement was short lived. Upon landing at Heathrow we were unable to taxi to our gate because of traffic on the ground. By the time I stepped out of the plane I only had 25 minutes to reach my Copenhagen flight. Sprinting to Terminal 4, I managed to make the gate 10 minutes prior to scheduled departure, only to find, as noted above, that the plane was delayed.

All in all, you can’t claim I have been lucky in my travels this time around (although I did travel on the 7th of the 7th month of 2007).

UPDATE: To add further dissatisfaction, my luggage did not arrive at Copenhagen airport. I will have to wait a few days before they find it (I hope) and send it to me. In addition, the plane did not land before 5 pm, so I am forced to take the last ferry arriving at midnight instead of 9 pm.

Saturday, July 07, 2007

To Hell and Back

Today I went for a walk up the north-west side of Cayman Island. There are two attractions: Turtle Farm and Hell.

Turtle farm breeds turtles - predominately the green sea specifies. Christopher Columbus who discovered the Cayman Islands in 1503 also named them Las Tortugas. It was the presence of the marine crocodile, however, that gave the islands their name, after the Carib word caymanas.
About 60% of each year's turtle hatchlings are raised to 3 - 4 years of age before they are processed for food that is sold locally. A national delicacy apparently and not one I have managed to taste. The remaining 40% are released into the ocean when they are around one year old. Out of these, a few are kept as future breeders.

Hell is an altogether different attraction. Rock formations that supposedly resemble the charred remains of a hell fire. A rock named ironshore makes up the rock formation. Ironshore is common on the island and is essentially limestone although it bears resemblance to volcanic rock. The grayish-black colour is product of algae secreting acid that also erodes the ironshore to create the hellish shapes.

On my way back to the hotel I got a lift from an old lady who was one of the original Caymanians with surname Ebanks. She was able to trace her decedents back to the first official population count in the eighteenth century. The count at that stage was around 900. By the time got back from Hell, the recruitment consultant ad left a message on my hotel phone advising that I had been offered the job. We have until Tuesday to accept. More will follow…..

Some facts about Cayman:
  • Discovered by Christopher Columbus on 10 May 1503 when his ships were blown off course by strong winds. Consists of three islands Grand Cayman, Little Cayman, and Cayman Brac
  • The capital, George Town, is named after King George III of England.
  • The islands are formed primarily of limestone.
  • Grand Cayman is the largest island and approximately 35 km long and 13 km widePopulation of approx. 50,000 English is the official language.
  • The national flower is the wild banana orchid, the national tree is the silver thatch palm, and the national bird is the Cayman parrot.
  • Pirates used the islands as a hideout well into the eighteenth century.
  • The country has the highest per capita income in the Caribbean.
  • The economy is based largely on tourism and the islands' status as an offshore financial center.
  • There is no business or personal income tax
  • Major sources of government revenue include import duties, a tax of 7.5–10 percent on land or property transfers, a 10 percent tax on tourist accommodations, airport and cruise ship passenger departure fees, company registration fees, work permits, and business licenses.
  • More than six hundred banks are registered, with assets in excess of $500 billion, making the islands the fifth largest financial center in the world.
  • The governor is appointed by the British Crown.
  • An eight-member Executive Council advises the governor. Five of the council members (called ministers) are elected from the fifteen Legislative Assembly representatives.

Thursday, July 05, 2007

From Brisbane to Cayman

So it has been a while since I posted anything. It has been a few very busy months. As I write this post I am sitting in The Courtyard Marriot Hotel on the Cayman Islands in the Caribbean waiting for a response to a job interview. The previous post was submitted from our apartment in Brisbane.

Having left Brisbane on 10 June (Tobias birthday) we made our way to Thailand. Here we spent three weeks doing pretty much nothing. The majority of time we were at the Holiday Inn Resort on Koh Phi Phi Don (about 8 x 2.5 km and the shape of an H), a fantastic island paradise off the southern coast of Thailand.
The resort had all the essentials for the making of a relaxing vacation. Staying within the bounds of the resort you could be forgiven for thinking that this was an island of perfection. However, just outside the resort was the island’s sea gypsy population and other less exclusive resorts giving a more realistic picture of the status of the island. In addition, every morning from around 6 an army of workers would clean the beach allocated to the Holiday Inn resort visitors. Upstream from the resort various rubbish would drift downstream during the night littering the otherwise beautiful beach. Litter in the water seems to be a general problem in the island region. According to Majken who visited the area 11 years ago, it was also problem back then. No matter where you are in the island region you find rubbish. The tsunami may have played a role, but it is unfortunate that locals (and tourists) are not more concerned with this development and have been educated in environmental protection.

During our stay we also managed to visit Phi Phi Don’s sister island Phi Phi Lei. Lei is uninhabited except for the Viking Cave which is guarded to protect the nests of the cave swift.
They are renowned for building nests with a unique chemical mix needed to produce the Chinese delicacy - Bird's Nest Soup. It is also on this island you find the world famous beaches Loh Samah and Maya Bay. The Beach was filmed here.

While the beaches in Thailand are fantastic the main Beach here on Cayman, seven mile beach, is just as impressive and impeccably clean. Despite its name it is only about 5.5 miles long. The stretch of land making up seven mile beach is the most developed and expensive area of Cayman and houses most of the island's luxury resorts and hotels.

I think the job interview went well. Cayman Island could prove to be a good place to live.