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Professor Roy Grainger

Reader in Atmospheric Physics

Research theme

  • Climate physics

Sub department

  • Atmospheric, Oceanic and Planetary Physics

Research groups

  • Earth Observation Data Group
Don.Grainger@physics.ox.ac.uk
Telephone: 01865 (2)72888
Robert Hooke Building, room S47
  • About
  • Publications

A study on the sensitivities of simulated aerosol optical properties to composition and size distribution using airborne measurements

Atmospheric Environment Elsevier 89 (2014) 517-524

Authors:

AR Esteve, EJ Highwood, WT Morgan, G Allen, H Coe, RG Grainger, P Brown, K Szpek
More details from the publisher

Simplifying the calculation of light scattering properties for black carbon fractal aggregates

Copernicus Publications 14:3 (2014) 3537-3562

Authors:

AJA Smith, RG Grainger
More details from the publisher

Supplementary material to "Simplifying the calculation of light scattering properties for black carbon fractal aggregates"

(2014)

Authors:

AJA Smith, RG Grainger
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Systematic satellite observations of the impact of aerosols from passive volcanic degassing on local cloud properties

Copernicus Publications 14:2 (2014) 2675-2716

Authors:

SK Ebmeier, AM Sayer, RG Grainger, TA Mather, E Carboni
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Retrieval of aerosol backscatter, extinction, and lidar ratio from Raman lidar with optimal estimation

Atmospheric Measurement Techniques European Geosciences Union 7:3 (2014) 757-776

Authors:

Adam Povey, Roy Grainger, Dan Peters, Judith L Agnew

Abstract:

Optimal estimation retrieval is a form of nonlinear regression which determines the most probable circumstances that produced a given observation, weighted against any prior knowledge of the system. This paper applies the technique to the estimation of aerosol backscatter and extinction (or lidar ratio) from two-channel Raman lidar observations. It produces results from simulated and real data consistent with existing Raman lidar analyses and additionally returns a more rigorous estimate of its uncertainties while automatically selecting an appropriate resolution without the imposition of artificial constraints. Backscatter is retrieved at the instrument’s native resolution with an uncertainty between 2 and 20 %. Extinction is less well constrained, retrieved at a resolution of 0.1–1km depending on the quality of the data. The uncertainty in extinction is >15 %, in part due to the consideration of short 1 min integrations, but is comparable to fair estimates of the error when using the standard Raman lidar technique. The retrieval is then applied to several hours of observation on 19 April 2010 of ash from the Eyjafjallajökull eruption. A depolarising ash layer is found with a lidar ratio of 20– 30 sr, much lower values than observed by previous studies. This potentially indicates a growth of the particles after 12– 24 h within the planetary boundary layer. A lower concentration of ash within a residual layer exhibited a backscatter of 10Mm−1 sr−1 and lidar ratio of 40 sr.
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