the company i work for decided that its switching from the german formal "You"(Sie) to the informal "you" (Du) in all of our websites so now we have to scour the entire database to change it and i quite frankly hate that, not just bc the unecessary extra work but especially bc its such a weird and unecessary change
i bet its bc everything here is getting englishfied (both literally and culturally it feels like, when my new boss talks its half in english bc every second german word is just replaced by an english one despite there being perfectly fine words for it in german too, its so annoying) and bc they want to sound more personal in hopes of getting more clients bc 'company is your fwiend uwu!!', i know this here is the amercian tm site so you wouldnt understand really but i do not want to be greeted with 'du' by companies, no, thats too personal, you dont know me and im not giving you my data, stay away!!
i guess thats how i would describe it .. the formal you is like a polite distance, like someone you dont know staying outside your personal space, but when its the informal 'you' it feels invasive unless i told you you can call me that, and that goes double for companies
maybe its a small thing that doesnt seem important but i cant stand it, im just a little part time worker doing data work so i got no say in it but the companies founder also announced hes giving his post to his kids some time ago so ...... since then theres been alot of changes and new projects that solely aim to imitate whats popular and whats done by other companies, despite ours being one that is, or used to be, intentionally different, like, that was the POINT, but i guess chasing trends is just too appealing for CEOs
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Hmm, I am looking through endless Ultimania translations to find a bit of information on a Crisis Core scene that will help me finish a post but as usual I became distracted.
(From the Crisis Core guide).
I was thinking about this fusion pod that Hojo lets Zack enter. Hojo can also apparently use it to physically enhance subjects?
Somehow Zack is infused to become stronger and then….
Hmmm.
Too much enhancement leads to degradation for SOLDIERs.
Alas, they all have their limits.
Well. Except one…
“You do not have the ability to copy unto others. Your DNA cannot be spread. Thus your body cannot deteriorate.”
Sephiroth’s cells have no limitations. How proud Hojo must have been, to discover that his first-rate science experiment, could not degrade or reach the limit of his cells.
He could enhance Sephiroth endlessly, making him stronger and stronger. Always superior to Hollander’s experiments. Never reaching a limit to what Project S could endure.
There was no threshold, was there?
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FOB: I only think in the form of crunching numbers
Me, a Data Engineer: Is... is he talking about me... 🤓
FOB: In hotel rooms, collecting Page Six lovers
Me, a Data Engineer in a monogamous relationship: Ah, nvmd 🥴
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Have you ever wondered how scientists know what earth's climate was like in the past? Thousands of years ago, long before humans started to measure and record these things?
It's a really fascinating question with a VERY cool answer! Ice cores! Basically, they go to someplace cold, like the Arctic or Antarctic, and drill really deep into the ice to take a vertical section of it.
[ID:A cylinder of ice, about an inch in diameter and perhaps a little over a foot long (that's around 2.5 centimeters in diameter and over 30cm long, for those of you sensibly using the metric system), held in thickly-gloved hands. End ID.]
Here's what they look like. Kind of - they're a lot bigger when they come out of a glacier, but they get broken down into smaller pieces for transportation and study.
The US National Oceanic and Atmospheric Administration has a cool article on it here, but I'll go over the basics because tumblr science communication has a uniquely fun dialect, and I much prefer to learn things that way. I'm also putting it under a read-more because it got long.
If you've ever taken a geology class, you probably know that rock gets deposited vertically over time, with the newest at the top and the oldest at the bottom. In places where ice stays frozen for a long time, it's basically the same principle - year after year of snow and ice layered on top of each other. Ice cores can include stuff that's been frozen for perhaps thousands of years - including air bubbles, dust, sea salt, volcanic ash, etc. Both those and the ancient ice itself can tell us things about what earth's climate was like when they were first frozen.
The water in the ice cores contains, just like water from today, varying ratios of oxygen isotopes: oxygen-16 and oxygen-18. Remember, the difference between isotopes is the number of neutrons in each atom - oxygen-16, with 16 neutrons, is the 'normal' one, which makes up over 99% of oxygen atoms. It's also lighter than oxygen-18, which has two extra neutrons, and that means that it's slightly more difficult to get out of the atmosphere via precipitation - and this is easier at colder temperatures. So, as global climate gets cooler, the ratio of oxygen-16 to 18 increases, and as global climate cools, it decreases. We can measure those ratios in ice cores to figure out what Earth's climate was like in the past - as far back as we can find ice. How far is that? Up to 800,000 years. Yeah, that's some fucking old ice.
That's a lot of ice, I can hear you thinking. You're right - the deepest ice core ever collected was 3769m - 3.7 kilometers of ice (for my fellow Americans, that's over 2 and a quarter miles). That is a stupidly long piece of ice. Now you know why they have to break it up to analyze it.
Also, remember those air bubbles I mentioned? We can measure the concentrations of gases in those to learn about the composition of Earth's atmosphere a long fucking time ago, including the concentration of greenhouse gases like carbon dioxide and methane. (How do you get air bubbles out of ancient ice you ask? NOAA has the answer: crush it under a vacuum hood. That means there's no other gases around to contaminate your sample while you put it in an airtight vial.)
How do we know how old the ice is? Same way we date other ancient stuff - there's two main methods.
Radioactivity and radioisotopes! Mostly naturally occurring, although for recent ice, radioactivity from nuclear testing can also be used. Carbon dioxide can be radiocarbon dated, volcanic material can be argon/argon dated, etc.
Layering! Especially looking for distinctive stuff like volcanic ash from significant geological events. This can be used to synchronize ice cores from different places, or for relative ages (i.e. this section is older than this one).
These are far from the only things ice cores can teach us, but this post is already very long so I'll leave it here. Check out the NOAA article for more details, and a fun anecdote about how no fieldwork project ever goes entirely according to plan - especially when there's polar bears.
Sources: 1, 2
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