192 karma · joined July 26, 2015
https://www.gla.ac.uk/research/beacons/nanoquantum/wee-gglas...
One important distinction is between measuring gravity (generally, acceleration in the vertical direction) and the gravity gradient. The latter is generally easier and more useful for navigation.
https://ieeexplore.ieee.org/document/4215058
Basically you can image anything if there is a density contrast, it's "just" a matter of how good your sensor and inversion algorithm is.
I spend my day-to-day working on measuring gravitational changes to determine groundwater storage change. There's a huge difference between demonstrating something in the lab vs. building an actual field instrument you can use in the real world.
https://www.usgs.gov/mission-areas/water-resources/science/s...
(he's a Cornell prof with dubious research/PR tactics)
https://groundwaterwatch.usgs.gov/default.asp
With some obvious large gaps. There are more collected by state agencies, consultants, etc. In most places there are probably more wells than you'd think.
In addition to measuring gravity from space to monitor groundwater it can be measured at the land surface, with better spatial resolution and worse accuracy. A 1x10-8 m/s^2 change in gravity is 2.4 cm of groundwater!
It's unclear what the other advantages over PyInstaller are. Does @cached_property provide a performance benefit?
http://enormocast.com/episode-90-peter-metcalf-big-peaks-and...