2018
DOI: 10.1590/0102-7786332015
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Evaluación de la Estabilidad Atmosférica Bajo Condiciones Físicas y Meteorólogicas del Altiplano Ecuatoriano

Abstract: Resumo La estabilidad atmosférica en la capa superficial, influye en muchos de los procesos dinámicos que se dan en la atmósfera, afectan los fenómenos de difusión y transporte de energía y materia, razón por lo que se ha estudiado ampliamente en latitudes medias; sin embargo, existen muy pocos trabajos en condiciones típicas del altiplano ecuatoriano (latitud cero y altura media respecto al nivel del mar de alrededor de 2500 m). En el presente trabajo se desarrolla un estudio de la variación de la estabilidad… Show more

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Cited by 2 publications
(3 citation statements)
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“…where ρ is the density of dry air (1.2 kgÁm −3 ), T (K) is the temperature, C p (1,010 JÁkg −1 ÁK −1 ) is the specific heat of air at constant pressure, k (0.4) is the Von Karman constant, and g (9.81 mÁs −2 ) is the gravitational acceleration (Bonan, 2015;Haro Velasteguí et al, 2018). The temperature and sensible heat flux (Q H ) were obtained from the meteorological station of II_UABC (Figure 1).…”
Section: Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…where ρ is the density of dry air (1.2 kgÁm −3 ), T (K) is the temperature, C p (1,010 JÁkg −1 ÁK −1 ) is the specific heat of air at constant pressure, k (0.4) is the Von Karman constant, and g (9.81 mÁs −2 ) is the gravitational acceleration (Bonan, 2015;Haro Velasteguí et al, 2018). The temperature and sensible heat flux (Q H ) were obtained from the meteorological station of II_UABC (Figure 1).…”
Section: Methodsmentioning
confidence: 99%
“…In the Pasquill‐Gifford classification, net radiation and wind speed values are considered (Asharafi and Hoshyaripour, 2010). In the Monin‐Obukhov classification, the length L was estimated as follows: L=ρCpTu·3italickgQH where ρ is the density of dry air (1.2 kg·m −3 ), T (K) is the temperature, C p (1,010 J·kg −1 ·K −1 ) is the specific heat of air at constant pressure, k (0.4) is the Von Karman constant, and g (9.81 m·s −2 ) is the gravitational acceleration (Bonan, 2015; Haro Velasteguí et al ., 2018). The temperature and sensible heat flux ( Q H ) were obtained from the meteorological station of II_UABC (Figure 1).…”
Section: Methodsmentioning
confidence: 99%
“…In areas with valley topography, temperature inversions at night limit the dispersion of pollutants from sources of terrestrial origin (Allen et al 2011). At night, atmospheric stability varies from neutral to moderately stable, with an ambient temperature gradient smaller than the adiabatic dry temperature gradient (De Nevers 1998, Haro et al 2018. This situation generates that these VOCs.…”
Section: Introductionmentioning
confidence: 99%