Existing photochemical theories of stratospheric ozone are surveyed. Recent modifications to Chapman's 1930 classical model have been focused on the search for additional sinks for stratospheric ozone, while relatively little attention has been given to the uncertainties in its production rate. A critical discussion is presented on the uncertainties involved in the photo-dissociation rate of molecular oxygen which is the determining factor in the ozone production rate. (Author).Research supported by the Air Force Cambridge Research Laboratories, Air Force Systems Command, United States Air Force, L.G. Hanscom Field, Bedford, Massachusetts."Meteorology Laboratory Project 8604."AD0779685 (from http://www.dtic.mil)."12 February 1974."Includes ...
Abstract: For almost half a century it was widely believed that the photochemistry of the stratosphe...
An assessment is made of the ability of current theory to explain the phenomenology of upper atmosph...
International audienceThe stratosphere is the atmospheric layer comprised between 8–18 km for its lo...
A review is given on selected aspects of the reaction mechanisms of current interest in the chemistr...
International audienceThis article describes the validation of a linear parameterization of the ozon...
In the upper stratosphere, an altitude range in which ozone should be in photochemical steady-state,...
Photolysis of vibrationally excited oxygen produced by ultraviolet photolysis of ozone in the upper ...
A simple but computer efficient parameterized ozone chemistry is developed to account for up-dates i...
Part I: This thesis consists of two chapters concerning photochemical processes in the atmosphe...
Diurnal variation of stratospheric short-lived speciesMaryam KhosraviChalmers University of Technolo...
Tropospheric ozone in high concentrations is harmful for mankind and the environment as a whole. As...
Two of the most important chemically reactive tropospheric gases are ozone (O{sub 3}) and the hydrox...
This chapter discusses the future evolution of stratospheric ozone and its return to historical valu...
Simplified models were developed for radiative heating and cooling and for ozone photochemistry in t...
The nature of the minor constituents which may have a controlling effect on the stratospheric ozone ...
Abstract: For almost half a century it was widely believed that the photochemistry of the stratosphe...
An assessment is made of the ability of current theory to explain the phenomenology of upper atmosph...
International audienceThe stratosphere is the atmospheric layer comprised between 8–18 km for its lo...
A review is given on selected aspects of the reaction mechanisms of current interest in the chemistr...
International audienceThis article describes the validation of a linear parameterization of the ozon...
In the upper stratosphere, an altitude range in which ozone should be in photochemical steady-state,...
Photolysis of vibrationally excited oxygen produced by ultraviolet photolysis of ozone in the upper ...
A simple but computer efficient parameterized ozone chemistry is developed to account for up-dates i...
Part I: This thesis consists of two chapters concerning photochemical processes in the atmosphe...
Diurnal variation of stratospheric short-lived speciesMaryam KhosraviChalmers University of Technolo...
Tropospheric ozone in high concentrations is harmful for mankind and the environment as a whole. As...
Two of the most important chemically reactive tropospheric gases are ozone (O{sub 3}) and the hydrox...
This chapter discusses the future evolution of stratospheric ozone and its return to historical valu...
Simplified models were developed for radiative heating and cooling and for ozone photochemistry in t...
The nature of the minor constituents which may have a controlling effect on the stratospheric ozone ...
Abstract: For almost half a century it was widely believed that the photochemistry of the stratosphe...
An assessment is made of the ability of current theory to explain the phenomenology of upper atmosph...
International audienceThe stratosphere is the atmospheric layer comprised between 8–18 km for its lo...