Satellite Measurements of Atmospheric Aerosols

From Federation of Earth Science Information Partners
Jump to: navigation, search

< GEO User Requirements for Air Quality | Report | Documents | Resources | Edit with Form
Doc #: warning.png" " is not a number. Title: Satellite Measurements of Atmospheric Aerosols | Document Link
Organization/Author: R. Husar
Type: Other
Year: 2009
Region: {{{DocRegion}}}warning.png"{{{DocRegion}}}" is not in the list of possible values (International, Africa, Asia, Non-Southeast , Asia, Southeast, Europe, North America, Oceania/Australia, Polar Region, South America) for this property.
Observation Type: {{{ObservationType}}}warning.png"{{{ObservationType}}}" cannot be used as a page name in this wiki.
Observation Needs: {{{ObservationNeedType}}}warning.png"{{{ObservationNeedType}}}" cannot be used as a page name in this wiki.
Document Status: Unsubmitted, 2009/11/00warning.pngThe date "2009/11/00" was not understood.
Parameters: {{{Parameters}}}warning.png"{{{Parameters}}}" cannot be used as a page name in this wiki.


Description of Document: Book chapter for Aerosol Measurement

Contents

Chapter Table of Contents: Satellite Measurements of Atmospheric Aerosols

Introduction

  • Two fields not clear at the start - 2 fields are atmospheric aerosols and remote sensing
  • Inverse problem of deriving atmospheric aerosol properties from measured optical effects at the top of the atmosphere is difficult because it requires the knowledge of those aerosol properties.
  • Aerosols are described by matching models and observations - uncertainty comes from divergence between model/uncertainty
  • Two fields complement each other not replace - surface measurements provide aerosol characteristics and properties; satellites provide transport and spatio/temporal patterns

Aerosol Physical and Optical Properties

Aerosol Dimensions

  • Space
  • Time
  • Diameter
  • Composition
  • Shape
  • Mixing (internal/external)

Key point is that diameter, composition, shape and mixing are all integral from satellite perspective not just height

signal at TOA is weak compared to surface reflectance

Regularities allow simplify the  :

  1. Multi-modal simplifies size distribution if you know total mass
    1. Each mode can be treated separately b/c particles of different size are governed by diff. mechanisms of formation, transport.
    2. Coarse particles originate from primary emission, are chemically stable, irregular shape do not interact with themselves or fine particles - therefore easier to model?
    3. Fine particles size changes in response to environment, form as product of reactions, internally mixed, multi-modal? more difficult to model?
  2. Mass median diameter increases in Urban area increases concentration. Find mass median using spectral and angular scattering.
  3. For region there is a high correlation between total light scattering and mass concentration of fine particles
  4. aerosol types are in layers
  • P = scattering phase function = energy scattered in given direction/average energy in all directions
  • Extinction Coefficient (Bext) = bscat + babs = fraction of light scattered and absorbed by particle per unit length.
    • if atmosphere is mixture of particles b is the sum of contributions for each source (SDH)
    • B also changes with vary with space/time.
    • AOT = integral of Bext between L1 and L2 (surface to satellite?) (SDH)
  • Fig. 4b - If higher bext more pronounced phase function therefore larger characteristic size therefore higher concentration?
  • aerosol types have same forward scattering, satellite measures the backscatter, therefore total scattering can be calculated and then correlated to pm2.5 conc. for a region.

Satellite Orbits

GEO - Geostationary orbits; 36,000 km up. high temporal res, low spatial res Polar orbit - low temporal (pass 1x a day); high spatial res

Principles of Satellite Aerosol Detection

Two competing effects of aerosols are that the light scattering particles tend to add reflectance to the surface brightness and at the same time they act as a filter which exponentially diminishes the total upwelling radiation

The ratio P/R0 determines whether aerosols will increase or decrease the apparent reflectance

  • R0=Surface reflectance function

AOT retrieval is not possible either when aerosol system reaches radiative equilibrium or when Phase function approximately matches surface reflectance function(which occur over bright surfaces)

Challenges of Satellite Aerosol Remote Sensing

  • Clouds obscure the detection of both underlying surface and atmospheric aerosols. Cloud shadows also can complicate aerosol retrieval.
  • Sensors has to work in transmission windows to avoid the influence of molecular absorption on aerosol retrieval
  • Uncertainties in Bidirectional Diffuse Reflectance Function (BDRF)cause uncertainties in retrievals

Aerosol Retrievals: Past, Present and Future

Earliest quantitative retrievals of aerosols was the byproduct from "aerosol correction algorithms"

A wide array of "dedicated" sensors were available by 1990's for the characterization of aerosols, each providing specific characteristics of aerosols

These sensors measure total aerosol burden (as AOT) in multiple wavelength channels which can give a clue on size composition of aerosol column

Performance of aerosol sensors are evaluated against observations by AERONET. Disparities are observed between sensors at pixel level as well as between temporal and spatial averaged aerosol properties.

In future,

  • Replacing static aerosol models with dynamic aerosol models would be desirable
  • Co-retrieval of surface and aerosol reflectance would be ideal
  • Aerosol retrievals could be expanded by multi-sensor data fusion

Satellite Information Systems

Applications

Personal tools
Namespaces

Variants
Actions
Navigation
Toolbox