![](v3_space.gif) |
![](v3_space.gif) |
![](v3_space.gif) |
![](v3_space.gif) |
![](v3_space.gif) |
![](v3_space.gif) |
![](v3_space.gif) |
![](v3_space.gif) |
![](v3_space.gif) |
![](v3_space.gif) |
![](v3_space.gif) |
![](v3_space.gif) |
![](v3_space.gif) |
![](v3_space.gif) |
![](v3_space.gif) |
![](v3_space.gif) |
![](v3_space.gif) |
|
|
Polarward Energy Transport
|
|
|
|
|
Annual-Mean
Radiative Energy
|
|
|
|
|
|
|
![](v3_slide0012_image022.gif) |
|
![](v3_slide0012_image023.gif) |
|
|
|
|
|
![](v3_space.gif) |
![](v3_space.gif) |
![](v3_space.gif) |
![](v3_space.gif) |
The atmosphere dominates the
|
|
polarward heat transport at
|
|
middle and high latitudes. The
|
|
ocean dominates the transport at
|
|
lower
latitudes.
|
|
|
|
|
![](v3_space.gif) |
![](v3_space.gif) |
Polarward heat flux is needed to
|
|
transport radiative energy from
|
|
the
tropics to higher latitudes
|
|
|
|
|
|
|
|
|
|
|
|
|
![](v3_slide0012_image024.gif) |
|
|