Refroidissement de la stratosphère : Détection réussie mais quantification encore incertaine

Keckhut, Philippe; Hauchecorne, Alain; Claud, Chantal; Funatsu, Beatriz M.; Angot, Guillaume

doi:10.4267/2042/51479

Météorologie

2013

DOI: 10.4267/2042/51479

|View full text |Cite

Refroidissement de la stratosphère : Détection réussie mais quantification encore incertaine

Philippe Keckhut¹,

Alain Hauchecorne²,

Chantal Claud³

et al.

Abstract: Figure 1. Profil vertical des variations de température associées à l'augmentation des gaz à effet de serre et des chlorofluorocarbones, gaz réduisant la c o n c e n t r a t i o n d'ozone stratosphérique (Ramanathan et al., 1987).

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...

Citation Types

Supporting

Mentioning

Contrasting

Year Published

2024

Publication Types

Select...

Article1

Relationship

Self Cite0

Independent1

Authors

Journals

Cited by 1 publication

References 16 publications

Supporting

Mentioning

Contrasting

Order By: Relevance

Numerical Models and Methods of Atmospheric Parameters Originating in the Formation of the Earth&#8217;s Climatic Cycle

Ilboudo,

Yamba,

Koumbem

et al. 2024

ACS

View full text Add to dashboard Cite

Atmospheric models are physical equations based on the ideal gas law. Applied to the atmosphere, this law yields equations for water, vapor (gas), ice, air, humidity, dryness, fire, and heat, thus defining the model of key atmospheric parameters. The distribution of these parameters across the entire planet Earth is the origin of the formation of the climatic cycle, which is a normal climatic variation. To do this, the Earth is divided into eight (8) parts according to the number of key parameters to be defined in a physical representation of the model. Following this distribution, numerical models calculate the constants for the formation of water, vapor, ice, dryness, thermal energy (fire), heat, air, and humidity. These models vary in complexity depending on the indirect trigonometric direction and simplicity in the sum of neighboring models. Note that the constants obtained from the equations yield 275.156˚K (2.006˚C) for water, 273.1596˚K (0.00963˚C) for vapor, 273.1633˚K (0.0133˚C) for ice, 0.00365 in/s for atmospheric dryness, 1.996 in 2 /s for humidity, 2.993 in 2 /s for air, 1 J for thermal energy of fire, and 0.9963 J for heat. In summary, this study aims to define the main parameters and natural phenomena contributing to the modification of planetary climate.

show abstract

Numerical Models and Methods of Atmospheric Parameters Originating in the Formation of the Earth&#8217;s Climatic Cycle

Ilboudo,

Yamba,

Koumbem

et al. 2024

ACS

View full text Add to dashboard Cite

show abstract

scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.

Contact Info

hi@scite.ai

10624 S. Eastern Ave., Ste. A-614

Henderson, NV 89052, USA

Blog Terms and Conditions API Terms Privacy Policy Contact Cookie Preferences Do Not Sell or Share My Personal Information

Made with 💙 for researchers

Part of the Research Solutions Family.

Refroidissement de la stratosphère : Détection réussie mais quantification encore incertaine

Abstract: Figure 1. Profil vertical des variations de température associées à l'augmentation des gaz à effet de serre et des chlorofluorocarbones, gaz réduisant la c o n c e n t r a t i o n d'ozone stratosphérique (Ramanathan et al., 1987).

Cited by 1 publication

References 16 publications

Numerical Models and Methods of Atmospheric Parameters Originating in the Formation of the Earth&#8217;s Climatic Cycle

Numerical Models and Methods of Atmospheric Parameters Originating in the Formation of the Earth&#8217;s Climatic Cycle

Contact Info

Product

Resources

About

Refroidissement de la stratosphère : Détection réussie mais quantification encore incertaine

Abstract: Figure 1. Profil vertical des variations de température associées à l'augmentation des gaz à effet de serre et des chlorofluorocarbones, gaz réduisant la c o n c e n t r a t i o n d'ozone stratosphérique (Ramanathan et al., 1987).

Cited by 1 publication

References 16 publications

Numerical Models and Methods of Atmospheric Parameters Originating in the Formation of the Earth&amp;#8217;s Climatic Cycle

Numerical Models and Methods of Atmospheric Parameters Originating in the Formation of the Earth&amp;#8217;s Climatic Cycle

Contact Info

Product

Resources

About

Numerical Models and Methods of Atmospheric Parameters Originating in the Formation of the Earth’s Climatic Cycle

Numerical Models and Methods of Atmospheric Parameters Originating in the Formation of the Earth’s Climatic Cycle