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91̽»¨
von Kármán vortex street over Canary Islands
Credit: NASA

Philip Stier

Professor of Atmospheric Physics

Research theme

  • Climate physics

Sub department

  • Atmospheric, Oceanic and Planetary Physics

Research groups

  • Climate processes
philip.stier@physics.ox.ac.uk
Telephone: 01865 (2)72887
Atmospheric Physics Clarendon Laboratory, room 103
  • About
  • Research
  • Teaching
  • CV
  • Publications

The effect of harmonized emissions on aerosol properties in global models – an AeroCom experiment

Authors:

C Textor, M Schulz, S Guibert, S Kinne, Y Balkanski, S Bauer, T Berntsen, T Berglen, O Boucher, M Chin, F Dentener, T Diehl, J Feichter, D Fillmore, P Ginoux, S Gong, A Grini, J Hendricks, L Horowitz, P Huang, ISA Isaksen, T Iversen, S Kloster, D Koch, A Kirkevåg, JE Kristjansson, M Krol, A Lauer, JF Lamarque, X Liu, V Montanaro, G Myhre, JE Penner, G Pitari, S Reddy, Ø Seland, P Stier, T Takemura, X Tie

The evolution of the global aerosol system in a transient climate simulation from 1860 to 2100

Authors:

P Stier, J Feichter, E Roeckner, S Kloster, M Esch

The global aerosol-climate model ECHAM-HAM, version 2: sensitivity to improvements in process representations

Authors:

K Zhang, D O'Donnell, J Kazil, P Stier, S Kinne, U Lohmann, S Ferrachat, B Croft, J Quaas, H Wan, S Rast, J Feichter

The impact of a land-sea contrast on convective aggregation in radiative-convective equilibrium

Authors:

Beth Dingley, Guy Dagan, Philip Stier, Ross James Herbert

The importance of temporal collocation for the evaluation of aerosol models with observations

Copernicus GmbH

Authors:

Naj Schutgens, Dg Partridge, P Stier

Abstract:

<jats:p>Abstract. It is often implicitly assumed that over suitably long periods the mean of observations and models should be comparable, even if they have different temporal sampling. We assess the errors incurred due to ignoring temporal sampling and show they are of similar magnitude as (but smaller than) actual model errors (20–60 %). Using temporal sampling from remote sensing datasets (the satellite imager MODIS and the ground-based sun photometer network AERONET) and three different global aerosol models, we compare annual and monthly averages of full model data to sampled model data. Our results show that sampling errors as large as 100 % in AOT (Aerosol Optical Thickness), 0.4 in AE (Ångström Exponent) and 0.05 in SSA (Single Scattering Albedo) are possible. Even in daily averages, sampling errors can be significant. More-over these sampling errors are often correlated over long distances giving rise to artificial contrasts between pristine and polluted events and regions. Additionally, we provide evidence that suggests that models will underestimate these errors. To prevent sampling errors, model data should be temporally collocated to the observations before any analysis is made. We also discuss how this work has consequences for in-situ measurements (e.g. aircraft campaigns or surface measurements) in model evaluation. </jats:p>

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