Atmospheric Model Applications

Abstract

He received his PhD in Hydrology from the University of Arizona in 2001 and during his career has done research in regional atmosphere modeling, hydrometeorological system modeling (coupled system of atmosphere, land-surface, and hydrological models), remote sensing and data assimilation. Since 2009, Dr. Yucel has been a member of the International Association of Hydrological Sciences (IAHS). Other than being an experienced lecturer, Dr. Yucel has also published extensively in numerous journals.

Contribution of Satellite Measurements to the Modeling and Monitoring of the Quality of Coastal Seawater

“…ρ λ is the coefficient of reflectance, G λ is the total radiation which reaches the ground, it represents the sum of a direct radiation and a radiation diffused by the air molecules and the aerosols towards the ground; T λ (θ v ) is the function of the radiation transmission into upper atmosphere; ω is the spherical albedo for the atmosphere which explains the multiple reflexions between the surface of the ground and the atmosphere; θ S is the solar angle of zenith in degrees and θ v is the angle of sight of the sensor at the time of while taking the images. (Houma and Bachari, 2012) Since the reflectivity of water is low, the equation 1can be roughly linear as in equation 1b:…”

Perspectives in Water Pollution

“…ρ λ is the coefficient of reflectance, G λ is the total radiation which reaches the ground, it represents the sum of a direct radiation and a radiation diffused by the air molecules and the aerosols towards the ground; T λ (θ v ) is the function of the radiation transmission into upper atmosphere; ω is the spherical albedo for the atmosphere which explains the multiple reflexions between the surface of the ground and the atmosphere; θ S is the solar angle of zenith in degrees and θ v is the angle of sight of the sensor at the time of while taking the images. (Houma and Bachari, 2012) Since the reflectivity of water is low, the equation ( 1) can be roughly linear as in equation ( 1b):…”