Summary:

## Sensible and Latent Heat Fluxes and Temperature for Vegetated Surfaces

In the case of a vegetated surface, the sensible heat (H) and water vapor flux (E) are partitioned into vegetation and ground fluxes. This partitioning depends on the vegetation temperature (Tv) and ground temperature (Tg), in addition to the surface temperature (Ts) and specific humidity (qs).

Due to the coupling between vegetation temperature and fluxes, a Newton-Raphson iteration is used to simultaneously solve for the vegetation temperature and the sensible heat and water vapor fluxes from the vegetation.

The article covers the following:

### Theory (Section 2.5.3.1)
- The equations used in the iteration scheme are derived.

### Numerical Implementation (Section 2.5.3.2)
- Details on the numerical scheme are provided.

The key points are the partitioning of heat and moisture fluxes between vegetation and ground, and the use of an iterative method to solve for the coupled vegetation temperature and fluxes.