[-] jadelord@discuss.tchncs.de 6 points 4 months ago

What is dead may never die.

[-] jadelord@discuss.tchncs.de 5 points 4 months ago* (last edited 4 months ago)

Time to let go, NASA. We had a good run. She needs to move on to another Solar System.

[-] jadelord@discuss.tchncs.de 5 points 5 months ago

Voice to Text system for Linux.

After Sayboard for Android, it seems plausible to get a local voice recongnition system for PC too.

[-] jadelord@discuss.tchncs.de 4 points 5 months ago* (last edited 5 months ago)

That math does not check out. There are only 8.1 billion humans alive. How can there be trillions of companies?

[-] jadelord@discuss.tchncs.de 4 points 8 months ago

The theme is FAIR and open-science and more specifically Research Software management.

[-] jadelord@discuss.tchncs.de 8 points 8 months ago

uBO > Preferences > Filter lists > Annoyances > uBlock filters - Annoyannces / AdGuard Annoyanaces

[-] jadelord@discuss.tchncs.de 8 points 8 months ago

Eww de Elon

[-] jadelord@discuss.tchncs.de 6 points 10 months ago

We need more tips like this to fool the next ChatGPT.

[-] jadelord@discuss.tchncs.de 5 points 10 months ago

If you press . while browsing github.com, it redirects to github.dev, which is a web VSCode too. Same thing in Gitlab.

[-] jadelord@discuss.tchncs.de 5 points 11 months ago

If everyone is dropping in market shares, who's gaining?

[-] jadelord@discuss.tchncs.de 4 points 11 months ago

Every orifice adds some drag into the flow, decreasing the flow rate. However if you would go for a descending size of orifices you would introduce a Venturi effect, increasing the velocity for a given flow rate. Think what happens when you squeeze the end of a gardening water hose; or what happens when you blow air out of your mouth.

[-] jadelord@discuss.tchncs.de 7 points 11 months ago

To me personally, the field is fun because it gives me a perspective on all the processes which drives the weather and climate. I like watching the skies and the seas.

Scientifically the most exciting areas right would be:

  • mixing efficiency: The ocean has a layered structure and it takes 1000s of years for the deep ocean to rise up. Many are trying to understand at what limits the turbulence in ocean currents drives the cold saline deep ocean to starts mixing with warmer fresher waters on the top more effectively. An important question in our changing climate.
  • convection: a classic problem where the heated walls drive convective motion. People are still trying to understand different parameters and how it affects the kind of convection we get. Convection is everywhere: ocean currents transporting heat between the latitudes and, atmosphere which determine where the deserts and rainforests are etc.
view more: ‹ prev next ›

jadelord

joined 1 year ago