A31C-0065
Theoretical Variation of Solar Radiation in a Tropical Mountain Valley

Wednesday, 16 December 2015
Poster Hall (Moscone South)
Laura Zulima Flórez Botero, Universidad Nacional de Colombia, Bogota, Colombia
Abstract:
Solar radiation over the earth's surface varies in response to global factors such as the atmosphere and the relative movement of Earth around the sun, and local factors related to the earth's surface features and topography. The aim of this study is to know the effect of local factors in spatial and temporal variability of solar radiation in a tropical mountain valley in Colombia. We estimated the potential solar radiation on simplified schemes of valleys by the means of theoretical exercises with different slopes and aspects for further analysis. Despite the closeness of the studied area to the line of Ecuador where the annual variation of radiation is almost zero we detected some differences. Changes were found in solar radiation on different valley schemes in terms of hours of sunshine and total energy that reaches the surface depending on the slope, the orientation of the slopes and the diurnal variation of the solar altitude angle. Results suggest that different aspects lead changes in the annual insolation up to 4 MJ / m2 on June and a lag of about two hours in the diurnal cycle of insolation in the southeast (135°) and northwest (315°) facing peaks with the highest radiation around 8 hours after sunrise. The annual variation cycle, related to the slope, does not show major changes, but the diurnal cycle of the cells with the major slope has the lower insolation with a maximum of about one hour before the other cells. Finally, a better understanding of the real dynamics of sunshine in the Valley of Aburrá - Colombia is possible knowing the variation of the annual cycle and the diurnal cycle of insolation in a synthetic valley reliant on the different aspects and slopes allows. This represents an opportunity to improve urban planning and rural productive activities that depends directly on the availability of energy.