Autonomous marine hyperspectral radiometers for determining solar irradiances and aerosol optical properties

作者:Wood John; Smyth Tim J*; Estelles Victor
来源:Atmospheric Measurement Techniques, 2017, 10(5): 1723-1737.
DOI:10.5194/amt-10-1723-2017

摘要

We have developed two hyperspectral radiometer systems which require no moving parts, shade rings or motorised tracking, making them ideally suited for autonomous use in the inhospitable remote marine environment. Both systems are able to measure direct and diffuse hyperspectral irradiance in the wavelength range 350-1050 nm at 6 nm (Spectrometer 1) or 3.5 nm (Spectrometer 2) resolution. Marine field trials along a 100 degrees transect (between 50 degrees N and 50 degrees S) of the Atlantic Ocean resulted in close agreement with existing commercially available instruments in measuring (1) photo-synthetically available radiation (PAR), with both spectrometers giving regression slopes close to unity (Spectrometer 1: 0.960; Spectrometer 2: 1.006) and R-2 similar to 0.96; (2) irradiant energy, with R-2 similar to 0.98 and a regression slope of 0.75 which can be accounted for by the difference in wavelength integration range; and (3) hyperspectral irradiance where the agreement on average was between 2 and 5 %. Two long duration land-based field campaigns of up to 18 months allowed both spectrometers to be well calibrated. This was also invaluable for empirically correcting for the wider field of view (FOV) of the spectrometers in comparison with the current generation of sun photometers (similar to 7.5 degrees compared with similar to 1 degrees). The need for this correction was also confirmed and independently quantified by atmospheric radiative transfer modelling and found to be a function of aerosol optical depth (AOD) and solar zenith angle. Once Spectrometer 2 was well calibrated and the FOV effect corrected for, the RMSE in retrievals of AOD when compared with a CIMEL sun photometer were reduced to similar to 0.02-0.03 with R-2 > 0.95 at wavelengths 440, 500, 670 and 870 nm. Corrections for the FOV as well as ship motion were applied to the data from the marine field trials. This resulted in AOD(500 nm) ranging between 0.05 in the clear background marine aerosol regions and similar to 0.5 within the Saharan dust plume. The RMSE between the handheld Microtops sun photometer and Spectrometer 2 was between 0.047 and 0.057 with R-2 > 0.94.

  • 出版日期2017-5-9