El Asintal Weather
Loading current temperature, humidity, wind, and air quality context for El Asintal, Retalhuleu, Guatemala.
Loading current temperature, humidity, wind, and air quality context for El Asintal, Retalhuleu, Guatemala.
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El Asintal, nestled within the Retalhuleu Department of Guatemala, occupies a geographically significant position within the southern highlands. Located at approximately 14.6000° N, -91.7333° W, the city sits at an elevation of roughly 1,500 meters (4,921 feet) above sea level, contributing to a cooler climate compared to lower-lying regions of Guatemala. The surrounding landscape is characterized by a mix of rolling hills, agricultural land, and patches of remnant cloud forest, typical of the Sierra Madre de Gualán-Zacapa volcanic chain. This terrain influences local wind patterns, often creating localized areas of stagnant air, particularly within the valley where El Asintal is situated. The city’s proximity to the Suchitepéquez Department creates a gradual urban-rural gradient, with agricultural activities – primarily coffee, sugarcane, and maize cultivation – dominating the surrounding areas. While not directly adjacent to a major river, the region receives substantial rainfall, contributing to humidity levels and influencing atmospheric stability. The absence of large-scale industrial zones within El Asintal itself is notable; however, the region’s agricultural practices, including the use of fertilizers and occasional burning of fields, can contribute to localized air pollution episodes. The valley setting, combined with the elevation and surrounding hills, can trap pollutants, especially during periods of reduced wind activity, impacting air quality within the city limits. The urban character is primarily residential, with a developing commercial sector, meaning vehicle emissions are a growing concern.
El Asintal’s tropical highland climate dictates a distinct wet and dry season pattern, significantly impacting air quality throughout the year. The dry season, typically spanning November to April, often sees a build-up of particulate matter. Reduced rainfall means less natural cleansing of the atmosphere, and the lack of strong winds can lead to temperature inversions, trapping pollutants closer to the ground. Agricultural burning, a common practice for land clearing and crop residue disposal, intensifies during this period, releasing significant amounts of smoke and particulate matter. February and March are often the months with the most noticeable impact from these practices. Conversely, the wet season (May to October) brings frequent rainfall, which naturally washes pollutants from the air, leading to improved air quality. However, periods of prolonged fog, common during the transition months (May and November), can temporarily reduce visibility and trap moisture-borne pollutants. The increased humidity during the wet season can also exacerbate respiratory issues for sensitive individuals. During the wettest months (September and October), while overall air quality improves, the prevalence of mold and mildew can trigger allergic reactions. Sensitive groups, including children, the elderly, and individuals with pre-existing respiratory conditions, should exercise caution during the dry season, limiting outdoor activities during peak burning periods and monitoring for respiratory discomfort. The increased humidity during the wet season necessitates vigilance regarding mold exposure within homes.
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