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AGU: Journal of Geophysical Research, Atmospheres

 

Keywords

  • PAR
  • MODIS
  • carbon cycle

Index Terms

  • Biogeosciences: Remote sensing
  • Biogeosciences: Carbon cycling
  • Atmospheric Processes: Clouds and aerosols
  • Biogeosciences: Data sets
  • Atmospheric Composition and Structure: Cloud/radiation interaction
Abstract
Cited By (18)
 

Abstract

JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 111, D15208, 13 PP., 2006
doi:10.1029/2005JD006730

Estimation of incident photosynthetically active radiation from Moderate Resolution Imaging Spectrometer data

Shunlin Liang

Department of Geography, University of Maryland, College Park, Maryland, USA

Tao Zheng

Department of Geography, University of Maryland, College Park, Maryland, USA

Ronggao Liu

Institute for Geographical Science and Natural Resources Research, Chinese Academy of Sciences, Beijing, China

Hongliang Fang

Department of Geography, University of Maryland, College Park, Maryland, USA

Si-Chee Tsay

Climate and Radiation Branch, NASA/Goddard Space Flight Center, Greenbelt, Maryland, USA

Steven Running

School of Forestry, University of Montana, Missoula, Montana, USA

Incident photosynthetically active radiation (PAR) is a key variable needed by almost all terrestrial ecosystem models. Unfortunately, the current incident PAR products estimated from remotely sensed data at spatial and temporal resolutions are not sufficient for carbon cycle modeling and various applications. In this study, the authors develop a new method based on the look-up table approach for estimating instantaneous incident PAR from the polar-orbiting Moderate Resolution Imaging Spectrometer (MODIS) data. Since the top-of-atmosphere (TOA) radiance depends on both surface reflectance and atmospheric properties that largely determine the incident PAR, our first step is to estimate surface reflectance. The approach assumes known aerosol properties for the observations with minimum blue reflectance from a temporal window of each pixel. Their inverted surface reflectance is then interpolated to determine the surface reflectance of other observations. The second step is to calculate PAR by matching the computed TOA reflectance from the look-up table with the TOA values of the satellite observations. Both the direct and diffuse PAR components, as well as the total shortwave radiation, are determined in exactly the same fashion. The calculation of a daily average PAR value from one or two instantaneous PAR values is also explored. Ground measurements from seven FLUXNET sites are used for validating the algorithm. The results indicate that this approach can produce reasonable PAR product at 1 km resolution and is suitable for global applications, although more quantitative validation activities are still needed.

Received 3 October 2005; accepted 28 April 2006; published 8 August 2006.

Citation: Liang, S., T. Zheng, R. Liu, H. Fang, S.-C. Tsay, and S. Running (2006), Estimation of incident photosynthetically active radiation from Moderate Resolution Imaging Spectrometer data, J. Geophys. Res., 111, D15208, doi:10.1029/2005JD006730.

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