Exploiting the MODIS albedos with the Two‐stream Inversion Package (JRC‐TIP): 2. Fractions of transmitted and absorbed fluxes
in the vegetation and soil layers
The two-stream model parameters and associated uncertainties retrieved by inversion against
MODIS broadband visible and near-infrared white sky surface albedos were discussed in a
companion paper (Pinty et al., 2010). The present paper concentrates
on the partitioning of the solar radiation fluxes delivered by the Joint Research Centre
Two-stream Inversion Package (JRC-TIP). The estimation of the various flux fractions related
to the vegetation and the background layers separately capitalizes on the PDFs of the model
parameters discussed in the companion paper. The propagation of uncertainties from the
observations to the model parameters is achieved via the Hessian of the cost function and
yields a covariance matrix of posterior parameter uncertainties. This matrix is propagated to
the radiation fluxes via the model's Jacobian matrix of first derivatives. Results exhibit a
rather good spatio-temporal consistency given that the prior values on the model parameters
are not specified as a function of land cover type and/or vegetation phenological states. A
specific investigation based on a scenario imposing stringent conditions of leaf absorbing
and scattering properties highlights the impact of such constraints that are, as a matter of
fact, currently adopted in vegetation index approaches. Special attention is also given to
snow covered and snow contaminated areas since these regions encompass significant
reflectance changes that strongly affect land surface processes. A definite asset of the
JRC-TIP lies in its capability to control and ultimately relax a number of assumptions that
are often implicit in traditional approaches. These features greatly help us understand the
discrepancies between the different data sets of land surface properties and fluxes that are
currently available. Through a series of selected examples, the inverse
procedure implemented in the JRC-TIP is shown to be robust, reliable and compliant with large
scale processing requirements. Furthermore, this package ensures the physical consistency
between the set of observations, the two-stream model parameters and radiation fluxes. It
also documents the retrieval of associated uncertainties.
PINTY Bernard;
CLERICI Marco;
ANDREDAKIS Ioannis;
KAMINSKI Thomas;
TABERNER Malcolm;
VERSTRAETE Michel;
GOBRON Nadine;
PLUMMER Stephen;
WIDLOWSKI Jean-Luc;
2011-12-09
AMER GEOPHYSICAL UNION
JRC64306
0148-0227,
http://www.agu.org/pubs/crossref/2011/2010JD015373.shtml,
https://publications.jrc.ec.europa.eu/repository/handle/JRC64306,
10.1029/2010JD015373,
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