In a companion paper, the temperature dependence of Raman scattering and its influence on the Raman water vapor signal and the lidar equations was examined. New forms of the lidar equation were developed to account for this temperature sensitivity. Here we use those results to derive the temperature dependent forms of the equations for the aerosol scattering ratio, aerosol backscatter coefficient, extinction to backscatter ratio and water vapor mixing ratio. Pertinent analysis examples are presented to illustrate each calculation
The problem of the increasing global atmospheric temperature has motivated a large interest in study...
Classical and quantum formulations are used to estimate Rayleigh scattering within lidar signals. Wi...
This article presents a study of aerosol optical and microphysical properties under different relati...
Water vapor concentration, expressed as a mass mixing ratio (g kg-1), is conserved in all meteorolog...
Lidar measurements of temperature for the upper troposphere and lower stratosphere are commonly deri...
Lidar measurements of the atmospheric water vapor mixing ratio provide an excellent complement to ra...
The statistical properties of atmospheric water vapor mixing ratio (WVMR) determined as the ratio of...
Aerosol size distribution provides good information for predicting weather changes and understanding...
Abstract:- The affinity of aerosol particles to water, as measured by the relative humidity, plays a...
A new method for independent calibration of water vapor Raman lidar by using additional measurements...
Abstract. A Raman lidar system based on a tripled Nd:YAG laser is used for profiling of water vapor ...
Vibrational Raman scattering from nitrogen is commonly used in Mie-Raman lidars for evaluation of pa...
Model studies have demonstrated that relative humidity has a critical influence on aerosol climate ...
A UV vibrational Raman lidar has been built and used to make quantitative measurements of water vapo...
This is a postprint (author final draft) version of article that has been accepted for publication. ...
The problem of the increasing global atmospheric temperature has motivated a large interest in study...
Classical and quantum formulations are used to estimate Rayleigh scattering within lidar signals. Wi...
This article presents a study of aerosol optical and microphysical properties under different relati...
Water vapor concentration, expressed as a mass mixing ratio (g kg-1), is conserved in all meteorolog...
Lidar measurements of temperature for the upper troposphere and lower stratosphere are commonly deri...
Lidar measurements of the atmospheric water vapor mixing ratio provide an excellent complement to ra...
The statistical properties of atmospheric water vapor mixing ratio (WVMR) determined as the ratio of...
Aerosol size distribution provides good information for predicting weather changes and understanding...
Abstract:- The affinity of aerosol particles to water, as measured by the relative humidity, plays a...
A new method for independent calibration of water vapor Raman lidar by using additional measurements...
Abstract. A Raman lidar system based on a tripled Nd:YAG laser is used for profiling of water vapor ...
Vibrational Raman scattering from nitrogen is commonly used in Mie-Raman lidars for evaluation of pa...
Model studies have demonstrated that relative humidity has a critical influence on aerosol climate ...
A UV vibrational Raman lidar has been built and used to make quantitative measurements of water vapo...
This is a postprint (author final draft) version of article that has been accepted for publication. ...
The problem of the increasing global atmospheric temperature has motivated a large interest in study...
Classical and quantum formulations are used to estimate Rayleigh scattering within lidar signals. Wi...
This article presents a study of aerosol optical and microphysical properties under different relati...