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Paper Information

Journal:   INTERNATIONAL JOURNAL OF ENERGY AND ENVIRONMENTAL ENGINEERING   2019 , Volume 10 , Number 2; Page(s) 147 To 156.
 
Paper: 

Effect of 21 August 2017 solar eclipse on surface‑ level irradiance and ambient temperature

 
 
Author(s):  Calamas David M.*, Nutter Christopher, Guajardo Dianna Nicole
 
* Department of Mechanical Engineering, Georgia Southern University, Statesboro, GA 30460, USA
 
Abstract: 
The temporal variation in the direct normal irradiance, diffuse horizontal irradiance, global horizontal irradiance, and ambient temperature was quantified during the 21 August 2017 solar eclipse. The magnitude and obscuration of the eclipse at the observation location were 0. 97 and 96. 94%, respectively. A two-axis sun tracker equipped with a pyrheliometer, a shaded pyranometer, an unshaded pyranometer, and a pyrgeometer were utilized to obtain the solar irradiance measurements. Thermistors contained within the pyrheliometer and the pyrgeometer were used to quantify changes in temperature. Unfortunately, on the day of the eclipse, the weather conditions were not ideal and periodic cloud coverage impacted measurements of the direct normal irradiance. As such, solar irradiance and temperature data from 2 days prior, when the weather conditions were near-ideal, are presented for comparison. The temperature of the air as measured by the thermistors enclosed within the pyrheliometer and pyrgeometer recorded an average temperature drop of 8. 49 ° C. The minimum temperature was recorded approximately 47 min after totality. The diffuse horizontal irradiance reached a maximum value of 495. 9 W/m2 shortly after the start of partial eclipse and dropped to a minimum value of 0 W/m2 near totality. Similarly, the global horizontal irradiance reached a maximum value of 1138 W/m2 and dropped to a minimum value of 1. 54 W/m2 near totality. For reference, at the same time of day, but 2 days prior, the diffuse horizontal irradiance and global horizontal irradiance were at values of 89. 2 W/m2 and 962 W/m2, respectively, under clear sky conditions. The rate of decrease in the temperature of the air as well as in the diffuse and global horizontal irradiances after first contact and before totality was greater than the rate of increase in these parameters after totality. The difference in the magnitude of these gradients before and after totality is largely attributed to normal diurnal variations as the solar eclipse occurred in the afternoon.
 
Keyword(s): Solar irradiance,Solar eclipse,Total eclipse,Temperature
 
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