Astara Weather
Loading current temperature, humidity, wind, and air quality context for Astara, Astara, Azerbaijan.
Loading current temperature, humidity, wind, and air quality context for Astara, Astara, Azerbaijan.
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Astara, a small city nestled in Azerbaijan’s southeastern corner, occupies a unique geographic position where the Talysh Mountains meet the Caspian Sea plain. Situated at approximately 38.44° N, 48.875° E, and with an elevation of around 180 meters (590 feet), Astara benefits from a relatively mild climate influenced by both the mountains and the sea. The city’s terrain is gently undulating, transitioning from the foothills of the Talysh range to the flat, fertile lands bordering the Khoshchoban River, a significant tributary of the Alinja River. This riverine system contributes to the region’s agricultural productivity, with surrounding areas dedicated to tea plantations, citrus groves, and rice paddies – all potential sources of localized emissions. Astara’s location on the border with Iran creates a complex interplay of influences, including potential transboundary pollution. The urban character is primarily residential and agricultural, with limited heavy industry within the city itself. However, the broader Astara region experiences a gradual urban-rural gradient, with smaller villages and agricultural settlements extending outwards. The proximity to Iran, and the potential for industrial activity in adjacent regions, means that Astara’s air quality can be affected by regional pollution events. Prevailing winds generally flow from the Caspian Sea towards the mountains, potentially carrying pollutants inland, while the mountains themselves can create localized areas of stagnant air, particularly during periods of calm weather. The surrounding landscape is a mix of dense forests, agricultural fields, and scattered settlements, all contributing to the overall atmospheric conditions.
Astara’s air quality exhibits a distinct seasonal pattern dictated by its subtropical climate and regional weather systems. The warmer months, from May to September, are generally characterized by higher temperatures and increased solar radiation, which can exacerbate ground-level ozone formation, a secondary pollutant. Agricultural activities, including irrigation and fertilizer application, also contribute to emissions during this period. The summer months often experience periods of calm winds, leading to stagnant air and the potential for pollutant accumulation. Conversely, the cooler, wetter months (October to April) typically see improved air quality due to increased rainfall, which helps to wash pollutants from the atmosphere, and more frequent wind events that disperse them. Fog, common during the autumn and winter, can trap pollutants near the ground, creating localized episodes of reduced visibility and potentially impacting air quality. The transition seasons, spring and autumn, are generally the most pleasant in terms of air quality, with moderate temperatures and sufficient wind to prevent significant pollutant buildup. Sensitive groups, such as children, the elderly, and individuals with respiratory conditions, should exercise caution during the warmer months, particularly on days with high temperatures and stagnant air. Outdoor activities are generally more favorable during the cooler, wetter months, although periods of fog can still pose a risk. Agricultural burning, a traditional practice in the region, can occasionally contribute to short-term spikes in particulate matter, particularly during the harvest season.
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