Abstract
The aim of this study is to analyze the effect of the water vapor content on the downward irradiance measured at the Earth's surface. For that purpose, downward irradiance values have been estimated with the radiative transfer model libRadtran in different spectral ranges: shortwave (SW: 285-2800 nm) and longwave (LW: 3500-50000 nm), and with different water vapor content in the column. These simulations have been made for Évora, Portugal, the August 4, 2012, a cloud-free day and with low aerosol optical depth.The comparison between the simulated irradiance with different water vapor contents shows differences in both spectral ranges. For SW, the irradiance reaching the surface increases when the water vapor content decreases, obtaining an increase of up to 4%, 2% and 1%, corresponding the largest increases to the smallest values of water vapor. For LW, the behaviour is the opposite, the irradiance decreases when the water vapor content decreases, obtaining a decrease of up to 10%, 4% and 2%, corresponding the largest decreases to the smallest values of water vapor. The effect of water vapor in the aerosol radiative forcing (ARF) has also been analyzed, obtaining relative difference values of up to 2.5% for SW and 35% for LW.
Highlights
Water vapor is an important atmospheric component, influencing the Earth’s climate in many ways
Estimations of downward irradiance provided by a reliable radiative transfer code, as libRadtran model [1], using different water vapor contents in the column are of great interest in order to analyze the water vapor effects in the irradiance and in the radiative balance of the Climate System
The aim of this study is to analyze the effect of different water vapor contents in the simulated downward irradiance values at the surface in different spectral ranges: shortwave and longwave
Summary
Water vapor is an important atmospheric component, influencing the Earth’s climate in many ways. Estimations of downward irradiance provided by a reliable radiative transfer code, as libRadtran model [1], using different water vapor contents in the column are of great interest in order to analyze the water vapor effects in the irradiance and in the radiative balance of the Climate System.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have