Chlorophyll remote measureement

ESTIMATING S0 STRESS BY CHLOROPHYLL FLUORESCENCE MEASUREMENTS WITH ACTIVE SYSTEM USED IN THE REMOTE SENSING MODE... 

Karabashev [469] devised a method to estimate the influence of dissolved oxygen on remote sensing measurements of chlorophyll a in seawater. The relationship between fluorescence and absorption was studied in this investigation. 

Indeed, Dachs et al. (2002) demonstrated, using a combination of field measurements of atmospheric PCBs, PCDDs, and PCDFs, and remote sensing data of ocean temperatirre, wind speed and chlorophyll, that deposition in mid-high latitudes is driven by sinking marine particulate matter, rather than by cold condensation. However, the relative contribution of this process is highly dependent on the physical chemical properties of the POPs under consideration. 

By measuring the chlorophyll fluorescence induction kinetics and the fluorescence spectrum of an intact leaf or plant the condition and potential activity of the photosynthetic apparatus can be estimated (1, ed. H.K. Lichtenthaler). Solely two parameters namely the chlorophyll fluorescence ratio F685/F730 and the fluorescence life time are reliable to measure by remote sensing (2). 

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