prd | R Documentation |
Convert mean and seasonal index of primary production and export depth to export POC flux
prd(npp_svi)
rld(npp_svi)
prr(npp_svi)
p.ratio(prd, z_ex, rld, prr)
lutz_p_flux(npp_mean, npp_svi, z_ex)
npp_svi |
A numeric vector of Seasonal variation index of production (SVI; annual standard deviation divided by average) |
z_ex |
A numeric vector of eport depth = water depth (z) - euphotic depth (z_eu) |
npp_mean |
A numeric vector of nnual mean surface production |
Export POC flux in the same unit as input primary production
prd()
: the labile fraction of export
rld()
: remineralization length scale
prr()
: rapidly sinking fraction of export
p.ratio()
: Annual Particulate Organic Carbon Flux to Depth Normalized to Overlying Production
Chih-Lin Wei <chihlinwei@gmail.com>
Lutz MJ, Caldeira K, Dunbar RB, Behrenfeld MJ (2007) Seasonal rhythms of net primary production and particulate organic carbon flux to depth describe the efficiency of biological pump in the global ocean. Journal of Geophysical Research: Oceans 112:C10011
# Seasonal variation index of NPP (SD/mean)
npp_svi <- 0.2789988
# Mean NPP (mgC/m2/day)
npp_mean <- 294.2888
# Mean chlorophyll concentrations (mg/m3)
chl_mean <- 0.123846
# Euphotic depth (m)
z_eu <- case1_z_eu(chl_mean)
# Water depth (m)
z <- 3115.12
# Export depth (m)
z_ex <- z-z_eu
# Lutz et al. (2007) POC flux (mgC/m2/day)
lutz_p_flux(npp_mean, npp_svi, z_ex)
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