Objectives
The overall objective of ONC is to demonstrate the feasibility of monitoring vegetation-atmosphere
CO2 exchange at the global scale, on daily to seasonal and inter-annual time scales.
In situ meteorological measurements and different satellite remote sensing sources
of information will be integrated by implementing and using assimilation techniques
in global land surface models. At the end of the project ECMWF will be able to
propose a near-operational system analysing land biospheric CO2 fluxes with a
spatial resolution of about 50 km. Global or continental-scale land data assimilation
systems (LDAS) have been developed in the last few years to characterise the surface
energy and water budget, including changes in soil water and snow mass. The pioneering
effort, coordinated by NASA, brings together a large community of meteorologists
and hydrologists and runs currently in real-time, for the globe (GLDAS, at ¼
degree resolution) and North America (NLDAS, at 1/8 degree resolution). In Europe,
ONC will provide a pre-operational global LDAS dealing with carbon accounting
issues. Some ONC partners (ECMWF, KNMI, Météo-France, Alterra) are
involved in the European LDAS (ELDAS) project which has created a daily data set
spanning the year 2000 and the European continent. LDAS systems are able to collect
all available remote sensing and in-situ information to create precipitation and
surface radiative field, together with near-surface meteorology from atmospheric
data assimilation centers. These fields are used to force state-of-the-art land-surface
models, producing as output surface energy and water fluxes, soil water and snow
mass. Uncertainty estimates can be obtained from varying the forcing and/or using
different land-surface models. LDAS outputs document best estimates of the fields
governing the surface-atmosphere interface; in particular, the soil moisture and
snow mass fields can be used as initial conditions for weather prediction and
monthly to seasonal forecasts.
So far, LDAS systems have not addressed carbon fluxes. However, a number of land
surface models used in numerical weather prediction and climate studies now include
photosynthesis and respiration modules coupled with biomass allocation schemes.
For example, ISBA-A-gs at Météo-France (the French weather service)
and ORCHIDEE at LSCE (a French research center of the Commissariat à l’Energie
Atomique and of the Centre National de la Recherche Scientifique) are interactive
vegetation models able to simulate the leaf area index and the vegetation biomass.
Furthermore ORCHIDEE includes the slow carbon reservoirs of the soil and the dynamics
of ecosystems after disturbance.
ONC will build on the modelling expertise of Météo-France and LSCE
to implement a carbon LDAS at ECMWF.
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