Calculation of Vegetation Indices with PAR and Solar Radiation Measurements David R. Cook Argonne National Laboratory.

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Presentation transcript:

Calculation of Vegetation Indices with PAR and Solar Radiation Measurements David R. Cook Argonne National Laboratory

2 Vegetation Indices NDVI – Normalized Difference Vegetation Index – indicator of vegetation health and carbon sink strength. LAI – Leaf Area Index – indicator of reflectance, density of vegetation, estimate soil surface heat flux. Fg – Green Vegetation Fraction – indicator of plant health and “greeness”. Normally used during growing season. Also exhibit seasonal trends throughout the year.

3 NDVI NDVI = (NIR-RED)/(NIR+RED) NIR ( nm; MODIS) RED ( nm; MODIS) NIR (760 and 810 nm) RED (660 and 710 nm) Fermi MSR Plants reflect well in the NIR to keep cool and absorb in visible wavelengths useful for photosynthesis.

4 NDVI from PAR and Solar Wilson and Meyers (2007) – upwelling, downwelling PAR ( nm) to determine visible radiation ratio (R VIS ); partitioned downwelling global (SOLR in ) into visible (VIS in ) and near infrared (NIR in ) R VIS = PAR out /PAR in VIS in = 0.45 * SOLR in NIR in = 0.55 * SOLR in (Weiss and Norman 1985) VIS out = R VIS * VIS in ) NIR out = SOLR out – VIS out R NIR = NIR out /NIR in NDVI = (R NIR – R VIS )/(R NIR + R VIS )

5 Estimation of R VIS No PAR measurements at ARM sites presently. Figure 3 in Wilson and Meyers (2007) little variation of the reflectance of visible radiation RVIS during a year for a grassland and that RVIS is very similar for grasslands in different climatic areas. Measurements for plain and temperate grasslands in Wilson and Meyers (2007) were used to determine the seasonal variation of RVIS for the SGP CF grassland.

6 Fg Fg = (NDVI – NDVI min ) / (NDVI max – NDVI min ), NDVI min - minimum mid-day NDVI measured during winter for bare soil and/or dead vegetation. NDVI max - maximum mid-day NDVI measured during the height of the summer growing season.

7 LAI LAI = LAI max x Fg, LAI max - maximum mid-day LAI during the growing season. LAI max is normally determined from at least one full year of data.

8 R VIS, NDVI, LAI, Fg - Fermi Ameriflux Prairie (PAR, SOLAR) 2005 a minor drought year 2006 fast growing invasive clover plant, Melilotus alba 2007 normal year

9 NDVI, LAI, and Fg - Fermi Ameriflux Prairie (MSR/ceptometer and PAR, Solar) MSR/ ceptometer five locations PAR/Solar one location NDVI, Fg agreement LAI worse

10 SGP CF NDVI, LAI, Fg, R VIS Very similar to Fermi prairie values Typical of temperate grasslands Agree with MODIS values (Wilson and Meyers 2007)

11 Differences – Fermi and SGP CF NDVI max, NDVI min - SGP CF grassland 0.69 and 0.07 Fermi prairie and 0.04 LAI max - SGP CF grassland 3.69 Fermi prairie – 2.8 SGP CF grassland denser; Fermi prairie more diverse

12 NDVI, H, LE, CO2 Flux, CO2 Concentration Fermi Prairie LE and CO 2 flux track with NDVI during middle of growing season Poor NDVI prediction in the early part and latter part of the growing season. NDVI underpredicts LE during the peak part of the Melilotus growing season in Significant decrease in CO 2 concentration in 2006 corresponding to the rapidly growing Melilotus alba

13 Evaporative Fractions EF = LE/(Rn-G) ES = LE/solar shortwave EPAR = LE/APAR APAR = net PAR ES better than EF long-term LE trends Satellites measure solar better than RN-G

14 NDVI, EF, and EPAR Fermi Prairie NDVI is a better predictor of EF through most of the growing season than of just LE NDVI does not do as well at predicting EPAR EF ratio is best predicted by vegetation indices calculated from surface measurements.

15 Conclusion The inclusion of upwelling and downwelling PAR measurements in conjunction with SIRS measurements of upwelling and downwelling solar radiation would enable valuable site specific vegetation indices to be determined with great confidence and employed for land use applications in computer models. Recommend Satlantic PAR 600LIN – $1200 each high quality filter delrin body excellent spectral response