Leaf area index

The impact of vegetation on interception of rainfall and on solar radiation is modelled by a Leaf Area Index (LAI).  It is one of the parameters in the model that describes land surface vegetation.

The leaf area index is derived from climatological data.  This takes into account seasonality (growing, mature, growing old, and dormant phases) of four types of forest vegetation (evergreen trees, deciduous trees, mixed forest/woodland, and interrupted forest).  It is also calculated daily from satellite data.  The leaf area index has a value of 0 over bare ground or where there are no leaves.  

The leaf area index is a non-dimensional number representing the square metres of leaf area per square metre of the earth's surface.  It determines the degree of evapotranspiration or interception of rain by vegetation.  

In IFS, leaf area index varies only with climatology, month by month.  Separation of HTESSEL "tiles" into high and low vegetation gives a more accurate seasonal variability of vegetation.  Anomalous weather (e.g. winds stripping trees of leaf), widespread fire damage (e.g. major change of albedo), etc are not taken into account.

The Leaf Area Index for each grid box is computed as:

Total leaf area index = (Leaf area index of high vegetation) x (cover in grid box of high vegetation) +  (Leaf area index of low vegetation) x (cover in grid box of low vegetation).


Considerations

Users need to be aware of the potential effect of any day-to-day anomalies.

  • Widespread storm damage or defoliation will reduce evapotranspiration from model predictions.
  • Vegetation growth and decay is climatologically variable but there is currently no interactive biology in the model.  Anomalously early extensive vegetation growth in spring or widespread wilting in heatwaves are not modelled. 
  • Transitory local but significant variations in surface characteristics (e.g. extensive burnt vegetation, seasonal variation in lake extent) are not represented.
  • Plant extraction of water and consequent leafiness varies with soil moisture.  This can be important especially in relatively dry conditions.  In turn this can affect the surface specific humidity.

Additional sources of information

(Note: In older material there may be references to issues that have subsequently been addressed)


Fig2A.1.4.7-1: Example leaf area index (LAI) as shown in the surface parameters charts. The LAI is taken from climatological data.  Anomalous weather has not had an effect.  Higher values mean more evapotranspiration, and therefore greater fluxes of moisture into the atmosphere.  An additional contributor to these moisture fluxes is bare-ground evaporation - this is not represented here.  HTESSEL deals with these aspects in more detail.  See the current leaf area index chart.



(FUG associated with Cy50r1)