Dependencia del Índice UV con el ozono y la turbiedad

1. M. J. Marín
2. A. R. Esteve
3. Fernando Tena Sangüesa
4. María Pilar Utrillas Esteban
5. José Antonio Martínez Lozano

Export

Export

×

MLA

modern-language-association

APA

apa

Chicago

chicago-fullnote-bibliography

Harvard

harvard-cite-them-right

Vancouver

vancouver-author-date

---

RIS BibTex

Export

×

This document cannot be exported because it belongs to another portal.

Full text

lock_openFull text externo

DIALNET GOOGLE SCHOLAR lock_openOpen access editor

More publications in: Óptica pura y aplicada

Abstract

The ultraviolet index (UVI) forecast reports people on the erythemal UV radiation level at the Earth’s surface. Prediction of the solar UV Index is achieved with a radiative transfer model that requires the inputs of total ozone and turbidity. The erythemal UV irradiance and the UVI are calculated to study the influence of the inputs for the equinoxes and solstices in Valencia. The ozone values are within the range 150-500 DU and the aerosol optical depth equal to 0.1, 0.3 and 0.5

Data source: Dialnet