Abstract
The quasigeostrophic equations formulated using the Charney–Phillips vertical staggering of variables are well known to possess an analog of the form of conservation of potential vorticity. It is shown that a similar analog is enjoyed by the quasigeostrophic equations formulated using the modified Lorenz staggering of variables.
Corresponding author address: Dr. Michael J. Bell, FOAM Research and Development, Met Office, London Rd., Bracknell, Berkshire RG12 2SZ, United Kingdom. Email: mike.bell@metoffice.com