|
Eliassen-Palm (E-P) Flux
SEPTEMBER 2012
FIGURE S7.
Daily vertical component of EP flux (which is proportional to the poleward
transport of heat or upward transport of potential energy by planetary wave) at
100 hPa averaged over (top) 30N-90N and (bottom) 30S-90S. The EP flux
unit (kg m-1s-2) has been scaled by multiplying
a factor of the Brunt Vaisala frequency divided by the
Coriolis parameter and the radius of the earth. The letter 'M' indicates
the current monthly mean value and the letter 'C' indicates the climatological
mean value. Additionally, the normalized departures from the monthly
climatological EP flux values are shown.
|
|