Abstract Aerosols produced by fire burns can have marked impacts on PV power production. Here we take advantage of an isolated, short-lived but well monitored fire burn event during an otherwise clear sky day – a case of a serendipitous ‘earth experiment’ – to study its impact on both solar irradiance and solar power recorded at the nearby solar lab. The local council controlled burns happened at Black Mountain in Canberra, Australia. Evidence from the solar lab sky-camera images was used to confirm that the sky was clear of clouds during the late afternoon of 4th March 2014 so that the effect of the smoke plume could be isolated, and to observe the development of the plume. Global and direct irradiance observations were compared with those from analogous clear days, as well as with values obtained from a clear sky model, in order to estimate the reduction in irradiance due to the smoke plume. The results showed that global irradiance was reduced by 6.5% and direct irradiance by 9% during a 140 min afternoon period, with one-minute reductions of up to 26% and 32% respectively. The spectral global irradiance showed that the smoke had the greatest impact in the wavelength range from 400 to 500 nm. A spectral analysis of the impact of smoke on six different PV technologies revealed that the least impact was on the mono-silicon cells used in this study. The resulting effect of solar power output was an overall reduction of 7% during the study period and a peak reduction of 27%.
[1]
I. Mokhov,et al.
The radiative and thermal effects of smoke aerosol over the region of Moscow during the summer fires of 2010
,
2012,
Izvestiya, Atmospheric and Oceanic Physics.
[2]
R. M. Mitchell,et al.
Characteristics and radiative impact of the aerosol generated by the Canberra firestorm of January 2003
,
2006
.
[3]
Alexander Smirnov,et al.
Cloud-Screening and Quality Control Algorithms for the AERONET Database
,
2000
.
[4]
T. Eck,et al.
Assessment of smoke aerosol impact on surface solar irradiance measured in the Rondônia region of Brazil during Smoke, Clouds, and Radiation ‐ Brazil
,
1999
.
[5]
G. Anderson,et al.
Radiative impact of boreal smoke in the Arctic: Observed and modeled
,
2008
.
[6]
S. M. Shaahid,et al.
Effect of Kuwait's oil-fire smoke cloud on global horizontal irradiance at Dhahran, Saudi Arabia
,
1994
.
[7]
E. Skoplaki,et al.
ON THE TEMPERATURE DEPENDENCE OF PHOTOVOLTAIC MODULE ELECTRICAL PERFORMANCE: A REVIEW OF EFFICIENCY/ POWER CORRELATIONS
,
2009
.
[8]
T. Stoffel,et al.
Some effects of the yellowstone fire smoke cloud on incident solar irradiance
,
1990
.
[9]
P. Ineichen,et al.
A new airmass independent formulation for the Linke turbidity coefficient
,
2002
.