Low Profile Box Spring Dust Ruffle

Iceland and Antarctica

Well that's a headline! Who do you have to write so much, it's not the easiest to write. What was I not restore all things out for great stories. Iceland for three weeks with all the trimmings! There is one email I received during an exciting bus ride to my phone if I join the ANT-XXVI / 2.
Thanks to modern technology Iceland so it was possible that I got in the middle of the remoteness of the Icelandic highlands of this mail. Iceland provided a Handyabdeckeung, even in places where you need it or not very much either. The Icelandic highlands is legendary. Stories of outlaws who were exiled there mixed with stories of tragedies and modern control. Iceland is practically the only offshore. In Germany, is nothing, garnix. What if I did not answer it can?
Then someone else would be traveling in the course of the ANT-XXVI / 2 of Polarstern expedition from Punta Arenas in Chile to Wellington in New Zealand. Endurance and annoying to pay off, according to cancel dozens I received a confirmation. One is enough, yes. It is not easy to get to the North Star. Many want to, but even though the Ship over 110 meters long drive only about 45 people with the AWI, the rest is part of the crew. Of the 45, some of Hawaii, Korea, Chile, New Zealand and elsewhere. So there are few places for PhD students or graduates that are sought after by its very nature. So I was lucky enough that someone can not ride because of the great thorough German bureaucracy. My job will be so with the equipment, the sediment cores from the seabed drag on deck to work.


Wolfram Distance: approx 8000nm
Weather
Harsh weather conditions are expected. Sea-ice may be present in the Ross Sea. Please be prepared against sea thickness. ha! Looking forward. Hopefully I can take the waves again as then before the Hakon Mosby Spitsbergen.

PS: The little problems are not solved! But tomorrow could be an important day ...

Photos of Iceland will soon be there.

Pokemon Purple Ti-84 Plus

hiccups

program and work-dipom is basically no different than running little problems to solve. Plays little more time. This month was marked by two larger ones. The first problem was to make it very difficult to locate. Fortunately
now the whole code in a version control system called Subversion. Many people use open source Subversion Kham

so that multiple people can work and do not come in your way. Very practical.
The second problem which I have now is not technical but mathematical programming. This point is probably in every major work ahead of time? Was all for nothing I have done? No! At least that is my opinion.
heard It is so simple. I must find out where a particle was previously a time-step. I know where it is now, and I know the 3D velocity field. So it's all there, right? But just the beginning of the story.

The goal is to extend the model that I have the whole history of particles in the ice record. Sounds very simple, since I already have the ice sheet, which gives me speeds etc. So just define a variable where the whole is stored, ready. It's just a simple Advection

, it happens no chemical transformation and no diffusion. But that is precisely the problem.
You think you could just carry the particles that fall on the ice. Just at the temperature formula which omitted? But no, there is no diffusion, there are sharp transitions from one property to another. For example, if two glaciers flow together, that's an ice and thus the particle is 2000 years old and the other 40000th At one point I then got a transfer of 2,000 to 4,000 Exactly at the interface I have on a jump. This leads to some problems. At the temperature there is something not because it is no matter how old the ice, the temperature there has not cracked. To detect the gene-history of the particles, such jumps should be possible. The origin and the time where it has landed on the ice must be maintained. It is the simplest formula, like this: The change is 0! The problem was solved until 2002 was the first time for ice sheet. The idea was to make it so so in 2002. See the picture below. It basically
two ways how to implement a model. It shares its entire area so as to Greenland in a grid, say 20x20 km and 100 in the high layers. In the Euler method one has a fixed grid and looking at what happened. In the Lagrange model you look at a particle and it follows all the time. In this case, as it were, then bends the bars. Both options have advantages and disadvantages. My
ice sheet has a fixed grid. So now it comes: there is the semi-Lagrangian method. This is a mixture of both. One uses a fixed grid and tracked in each time step, only the particle that hits a lattice point as the endpoint. Because change is not with me so the property should it enough if I know where the particles come and how the property was there the previous time step.
The difficulty is now to know where it was PRIOR particles. In a 3D grid with a different velocity at every point within a grid cell! And an ever-changing speed. Yes when that does not work then the whole method does not, or will the inaccurate, so inaccurate and everything becomes less accurate with each time step. If we accurately compute time just 400,000 years then add up the deviations.
is unfortunately nothing in the article about accurate extreeeem only a simple formula: the place where it was before the same is the place where it's gone now minus the back down ....
So I searched more articles the semi-lagrange use and after a day I also found some where it is described in more detail, with all the numerical odds and ends you have to consider too. So I'm confident it will work and I will meet again on Monday with my supervisor.

We think that is more complex and the more complicated it is. Make a simple task at first is evolving into an interesting and complex problem. We lost very quickly to details. To every detail, there are dozens of articles and sometimes you just think everything is too complicated and it is no longer the easiest things safe. So it was good that I've written here once so I know what itself the original objective was.

but then starts to really, because then you can make virtual ice cores and compare them with real! About isotopes and for which one uses it I'll write something later.

Well, now, a slightly longer post but then I want if I am then in a week in Graz not always explain what I make. I'm looking forward to daham, so until then.

PS In August I'll go to Iceland! The hike, etc., not from the AWI.

Help Installing Mount And Blade Vista From Disk

diseases

your machine manufacturer knows the safe at the very beginning where you get used to the 40 hour week, and the whole day sitting in front of the PC and records, and zooms out and new items will zoom, zoom, and again a Stichleim there and then.
Then you sit at home watching television and in a careless moment, one will be even closer Zooming when something interesting in the picture is ... Yes
as modelers and programmers that are so similar, one wonders sometimes briefly about the brilliant implementation of the graphics at the waves in the lake. Or amused at
Surge
the sauce from the potatoes.

long time now I had to struggle with a problem, there were not getting results, but completely wrong. Everything was right, and yet not. Usually you can find errors immediately, as upset the compiler. If he was not upset, then Not on the man and the man, and in general, and in any case.

But we're up again as it should, the virtual glacier flows nicely in front of him and I can simulate thousands of funny.
But the real work is thus obviously a little behind schedule, some things are working now and I am confident that I have until July first results.
On Friday I go to visit the world-famous or not Polarstern
! The output label of the AWI. I've already tried some on a long ride exit so far without success, but I'm working on it ...

Why Can't I Have A Pet Platypus?

Norge

am now yes again some time back from Norway. Fjord, snow, mountains, mountains, meet old friends, must be a holiday. Bergen has the dubious reputation of the city so in Europe with the most rainy days to be. Not true. According to my extrapolation of 5 days, it is the sunniest city in Europe. So yes, some argue Klimaskepitker. Perfect conditions for my wanderlust

to breastfeed. So it was a mountain that I climbed twice on the same day, as Jule just behind it lives on a lake. Should live one, 15min to the center but in the middle of the wilderness.
In Oslo, I visited with Peter, who is doing a semester abroad in Bergen, two friends of Spitsbergen. So I could study their behavior in their natural habitat. They're two marked the City Girls is thought not necessarily in Spitsbergen. On the first evening we were grateful to a party-wise in the 12th floor overlooking Oslo towed. The train ride alone was worth the trip already. Although only 300 km between Oslo and Bergen are driving man 7 hours over the mountains and the highest railway station in northern Europe. The second weekend we were headed for Stavanger Pulpit Rock said. It immediately in the top 3 on the list of the most beautiful places I have visited make it. A stone's 600 projects over the fjord with spectacular views of the surrounding mountains. Were some very nice days and also important to complete with Spitsbergen. This can be in Bremerhaven for the time and live very well, am just from the beach in the middle of the city back. Including holiday feeling. Yesterday I had my first visitor and he has also fallen quite well. Visitors who want to wade around in the Wadden Sea, however, may have no fear of worms ....