609320ee-d495-47f6-b55c-62484c32e956 11 6 9 decimal

&[DATE] &[TIME] - &[FILENAME]

vx vy char size color plotG n vx length : plot vx 1 el vy 1 el char size color augment : i 2 n range plot plot vx i el vy i el char size color augment stack : for plot 41 line :

Altimetric pressure => km => kPa

XY 0.5 - 107.477 0 101.325 0.5 95.461 1 89.876 1.5 84.559 2 79.501 2.5 74.691 3 70.121 3.5 65.78 4 61.66 4.5 57.752 5 54.048 5.5 50.539 6 47.217 6.5 44.075 7 41.105 7.5 38.299 8 35.651 8.5 33.154 9 30.8 9.5 28.584 10 26.499 10.5 24.54 11 22.699 11.5 20.984 12 19.399 12.5 17.933 13 16.579 13.5 15.327 14 14.17 14.5 13.1 15 12.111 15.5 11.197 16 10.352 16.5 9.571 17 8.849 17.5 8.182 18 7.565 18.5 6.994 19 6.467 19.5 5.979 20 5.529 422 mat :

X XY 1 col : Y XY 2 col : Pts X Y . 12 black plotG : 31 line

x kPa11 66.316994 3988.071258 x 2.403022 + 1379.737008 x 28.965069 + 539.638243 x 13.217861 + / - / + / - :

β 0.02264 127.8954 6.35874 31 mat :

x β kPa20 β 1 el β 2 el x β 3 el / - exp * + :

Pressure [kPa] @ geopotential x = [km]

x kPa11 x β kPa20 11 50 11 0 2 2 mat 20 50 20 0 2 2 mat Pts 5 1 sys

Altimetric Pressure kPa @ Geopotential km

x kPa11 x β kPa20 21 mat 1 - x ≤ (x 11 ≤ (& 11 x ≤ (x 20 ≤ (& 21 mat ≡

Above your head is not homogeneous. The first layer up to 11 km is rational. The next layer is expDecay. It was so recognized by experimenters and so reproduced for 'ρ & kPa' from agreed samples. The two segments are declared exact.