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Víctor M. Mendoza,Blanca Mendoza,René Garduño,Guadalupe Cordero,Marni Pazos,Sandro Cervantes,Karina E. Cervantes
Pág. 1 - 23
We present a thermodynamic model to simulate the atmospheric temperature and pressure, the regolith temperature and the polar CO2 ice caps vertical thickness and horizontal extent of Mars. This is done using the temperatures of the atmosphere and regolit...
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Francisco Estrada,Carlos Gay-García,René Garduño-López
Pág. i - ii
Environmental problems are typically produced by the interactions of complex natural and human systems and can entail far-reaching and sometimes irreversible consequences. Their study is characterized by the existence of incomplete knowledge and high lev...
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Víctor Manuel Mendoza Castro,René Garduño,Elba E. Villanueva,Blanca Mendoza
Pág. 219 - 227
The IPCC (2013) gives simplified formulas to compute the radiative forcing (RF) resulting from the increase in anthropogenic greenhouse gases (AGG): carbon dioxide (CO2), methane (CH4), nitrous oxide (N2O) and halocarbons. These formulas allow to compute...
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JULIAN ADEM,V. MANUEL MENDOZA,A. RUÍZ,E. E. VILLANUEVA URRUTIA,RENÉ GARDUÑO
The Adem thermodynamic climate model (ATCM) has been adapted to carry out three-month extended and seasonal numerical weather predictions. The model uses the Northern Hemisphere NMC polar stereographic grid with 1977 points and a grid distance of 408....
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JULIAN ADEM,ALFREDO RUÍZ,V. MANUEL MENDOZA,RENÉ GARDUÑO,VÍCTOR BARRADAS
A revised version of the Adem Thermodynamic Model is used to make mean monthly predictions of temperature and precipitation anomalies in the Northern Hemisphere. The initialization data are the sea surface and 700 mb temperatures in the previous month...
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RENE GARDUNO,ADEM JULIAN
Smith's (1969) analytical absorption spectrum of the atmosphere is incorporated in a thermodynamic model. This radiative formulation is applied to the infrared region. It computes separately the absorptivity by carbon dioxide and by water vapor, with ...
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