Vegetation
Optional
vegetation
listdictionaryThe optional vegetation
argument is a listdictionary of properties for vegetation and the soil. There must be one or more vegetation pools and there must be one or more soil pools. The values that can be set within the vegetation
listdictionary are:
Cvegpi
: A vectorlist of preindustrial carbon stocks, in GtC, for each of the vegetation pools. Default isc(100,475,40)
.tauveg
: A vectorlist, of the same length asCvegpi
, of timescales, in yr, for the flows of carbon out of the vegetation pools (to the first soil pool). The default isc(100,25,1)
. Combined with the defaultCvegpi
, this gives a preindustrial NPP of 100/100 + 475/25 + 40/1 = 60 GtC/yr.NPPmax
: The maximum NPP, in GtC/yr, when the atmospheric CO2 concentration is no longer a limiting factor. This value must be greater than the sum ofCvegpi
. Default is80
.albedo_forcing
: The shortwave radiative forcing per deviation in the total amount of vegetative carbon (not including soil carbon) from the preindustrial value, in units of W/m2/GtC. Default is0.002
.tausoil
: A vectorlist, of length equal to the number of desired soil pools, of timescales, in yr, for the flows of carbon out of the soil pools (a fractionsoiloxi
of which goes to the atmosphere and1-soiloxi
of which goes to the next soil pool). Default isc(10,1000)
.soiloxi
: A vectorlist, of the same length astausoil
, of fractions of the flows of carbon out of the soil pools that are oxidized and sent to the atmosphere. The last element of this vectorlist must equal1
. Default isc(59/60,1)
. With a preindustrial NPP of 60 GtC/yr (see the note ontauveg
above) and the defaulttausoil
values (given above), this gives preindustrial soil carbon stocks of 60 x 10 = 600 GtC in the fast (10-yr) pool and 60 x (1-59/60) x 1000 = 1000 GtC in the slow (1000-yr) pool.soilQ10
: The Q10 value for the soil decay rate, i.e., the factor by which the timescale of soil decay decreases for a 10-K temperature in surface temperature. Default is1.5
.