Remote Sensing (Dec 2018)

Satellite and In Situ Observations for Advancing Global Earth Surface Modelling: A Review

  • Gianpaolo Balsamo,
  • Anna Agustì-Parareda,
  • Clément Albergel,
  • Gabriele Arduini,
  • Anton Beljaars,
  • Jean Bidlot,
  • Nicolas Bousserez,
  • Souhail Boussetta,
  • Andy Brown,
  • Roberto Buizza,
  • Carlo Buontempo,
  • Frédéric Chevallier,
  • Margarita Choulga,
  • Hannah Cloke,
  • Meghan F. Cronin,
  • Mohamed Dahoui,
  • Patricia De Rosnay,
  • Paul A. Dirmeyer,
  • Matthias Drusch,
  • Emanuel Dutra,
  • Michael B. Ek,
  • Pierre Gentine,
  • Helene Hewitt,
  • Sarah P. E. Keeley,
  • Yann Kerr,
  • Sujay Kumar,
  • Cristina Lupu,
  • Jean-François Mahfouf,
  • Joe McNorton,
  • Susanne Mecklenburg,
  • Kristian Mogensen,
  • Joaquín Muñoz-Sabater,
  • Rene Orth,
  • Florence Rabier,
  • Rolf Reichle,
  • Ben Ruston,
  • Florian Pappenberger,
  • Irina Sandu,
  • Sonia I. Seneviratne,
  • Steffen Tietsche,
  • Isabel F. Trigo,
  • Remko Uijlenhoet,
  • Nils Wedi,
  • R. Iestyn Woolway,
  • Xubin Zeng

DOI
https://doi.org/10.3390/rs10122038
Journal volume & issue
Vol. 10, no. 12
p. 2038

Abstract

Read online

In this paper, we review the use of satellite-based remote sensing in combination with in situ data to inform Earth surface modelling. This involves verification and optimization methods that can handle both random and systematic errors and result in effective model improvement for both surface monitoring and prediction applications. The reasons for diverse remote sensing data and products include (i) their complementary areal and temporal coverage, (ii) their diverse and covariant information content, and (iii) their ability to complement in situ observations, which are often sparse and only locally representative. To improve our understanding of the complex behavior of the Earth system at the surface and sub-surface, we need large volumes of data from high-resolution modelling and remote sensing, since the Earth surface exhibits a high degree of heterogeneity and discontinuities in space and time. The spatial and temporal variability of the biosphere, hydrosphere, cryosphere and anthroposphere calls for an increased use of Earth observation (EO) data attaining volumes previously considered prohibitive. We review data availability and discuss recent examples where satellite remote sensing is used to infer observable surface quantities directly or indirectly, with particular emphasis on key parameters necessary for weather and climate prediction. Coordinated high-resolution remote-sensing and modelling/assimilation capabilities for the Earth surface are required to support an international application-focused effort.

Keywords