Refinement of a Database of Spectral Surface Reflectivity in the Range 335-772 nm Derived from 5.5 Years of GOME Observations

By N. Fournier, R. Koelemeijer, M. Eisinger, J. D. Haan, Piet Stammes. 2003

320 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/31ab4ccf6748058f0421720c3dc9075f20f5ba2e

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

In Global and Planetary Change

Citations in the corpus

Multi-model ensemble simulations of tropospheric NO2 compared with GOME retrievals for the year 2000 (2006, unknown): “…and associated radiative forcings (Stevenson et al., 2006); a detailed analysis of surface ozone, including impacts on human health and vegetation (Ellingsen et al., 20062); an analysis and validation of nitrogen and sulfur deposition budgets (Dentener et al., 2006b); and a comparison of…”
Global inventory of nitrogen oxide emissions constrained by space‐based observations of NO2 columns (2003, unknown): “Our inventory integrates information from bottom-up inventories and the top-down GOME observations, weighted by their respective errors, to optimize the use of the GOME data for constraining NO x emissions.”
Effective cloud fractions from the Ozone Monitoring Instrument: Theoretical framework and validation (2008, methodology): “The surface albedo in the retrieval is taken from the GOME albedo database [Koelemeijer et al., 2003], in combination with the TOMS albedo database [Herman and Celarier, 1997].”
Ozone profile and tropospheric ozone retrievals from the Global Ozone Monitoring Experiment: Algorithm description and validation (2005, background): “We find large differences in surface albedo of up to 50% between TOMS [Herman and Celarier, 1997] and GOME [Koelemeijer et al., 2003] databases at polar regions, supporting that large errors of surface albedo exist.”
Aerosol properties over bright-reflecting source regions (2004, methodology): “To obtain the surface reflectance information required by our aerosol retrieval algorithm, we generated a database of surface reflectivity using the minimum reflectivity technique [9], [24].”
Cloud pressure retrieval using the O2‐O2 absorption band at 477 nm (2004, methodology): “The surface albedo is taken in this paper from a ground reflectance database derived from GOME data [Koelemeijer et al., 2003], interpolating to the wavelength 475 nm.”