Understanding the Land Carbon Cycle with Space Data: Current Status and Prospects

Geophysical surveys - Tập 40 - Trang 735-755 - 2019
Jean-François Exbrayat1, A. Anthony Bloom2, Nuno Carvalhais3,4, Rico Fischer5, Andreas Huth5,6,7, Natasha MacBean8, Mathew Williams1
1National Centre for Earth Observation and School of GeoSciences, University of Edinburgh, Edinburgh, UK
2Jet Propulsion Laboratory, California Institute of Technology, Pasadena, USA
3Max Planck Institute for Biogeochemistry, Department Biogeochemical Integration, Jena, Germany
4CENSE, Departamento de Ciências e Engenharia do Ambiente, Faculdade de Ciências e Tecnologia, Universidade NOVA de Lisboa, Campus de Caparica, Caparica, Portugal
5Helmholtz Centre for Environmental Research–UFZ, Department of Ecological Modelling, Leipzig, Germany
6Institute of Environmental Systems Research, University of Osnabrück, Osnabrück, Germany
7German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-Leipzig, Leipzig, Germany
8Department of Geography, Indiana University, Bloomington, USA

Tóm tắt

Our understanding of the terrestrial carbon cycle has been greatly enhanced since satellite observations of the land surface started. The advantage of remote sensing is that it provides wall-to-wall observations including in regions where in situ monitoring is challenging. This paper reviews how satellite observations of the biosphere have helped improve our understanding of the terrestrial carbon cycle. First, it details how remotely sensed information of the land surface has provided new means to monitor vegetation dynamics and estimate carbon fluxes and stocks. Second, we present examples of studies which have used satellite products to evaluate and improve simulations from global vegetation models. Third, we focus on model data integration approaches ranging from bottom-up extrapolation of single variables to carbon cycle data assimilation system able to ingest multiple types of observations. Finally, we present an overview of upcoming satellite missions which are likely to further improve our understanding of the terrestrial carbon cycle and its response to climate change and extremes.

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