Henry Charnock Explained

Henry Charnock [1] (25 December 1920  - 28 November 1997) was a British meteorologist.[2] He is well known for his work on surface roughness and wind stress over water surfaces. The now named "Charnock's relationship" describes the aerodynamic roughness length,

z0

, over a water surface by:[3]

z0=C

2/g
u
*

where

u*

is the friction velocity and

g

is the acceleration due to gravity (typically the Standard gravity).

C

is Charnock's proportionality constant.

Charnock was President of the International Union of Geodesy and Geophysics (IUGG) from 1971 to 1975.

Bibliography

Notes and References

  1. Cartwright . D. E. . 10.1098/rsbm.1999.0004 . Henry Charnock, C.B.E. 25 December 1920 -- 27 November 1997: Elected F.R.S. 1976 . . 45 . 35 . 1999 . 140594865 .
  2. The Oxford Dictionary of National Biography . 10.1093/ref:odnb/68802 . 2004 . Cartwright . D. E. .
  3. Book: Stull . R. B. . 1988 . "An Introduction to Boundary Layer Meteorology" . 978-94-009-3027-8 . Kluwer Academic Publishers.