Palabras clave
sensor
atmosfera
satélite
forzamiento radiativo
Cómo citar
Resumen
Describimos los resultados del estudio del espesor óptico de aerosol (EOA) y el Forzamiento Radiativo Directo (FRD) en la cima de la atmósfera (TOA), obtenidos en el periodo 2004 utilizando el sensor MODIS del satélite TERRA para Perú. Donde se observa que el valor del EOA puede tomar valores máximos alrededor de 0.5, obteniéndose como resultado el FRD de aerosol en la parte superior de la atmósfera. Los resultados indican que, la FRD está entre [-5 0] W / m2.
Citas
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Esta obra está bajo una licencia internacional Creative Commons Atribución 4.0.
Derechos de autor 2022 Roberto Julio Angeles Vasquez, Julio Miguel Angeles Suazo, Nataly Angeles Suazo, Arlitt Lozano, Jose Flores Rojas