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Jōsō, Ibaraki Prefecture, Japan, occupies a strategically important position within the Kanto Plain, a vast sedimentary basin that stretches across central Honshu. Located approximately 80 kilometers northeast of Tokyo, Jōsō’s geography is characterized by gently undulating terrain, a legacy of alluvial deposits from the Kuji River and its tributaries. The city’s elevation averages around 20-30 meters above sea level, contributing to a relatively flat landscape that facilitates agricultural activity and urban expansion. The surrounding landscape is a mosaic of rice paddies, vegetable farms, and increasingly, suburban residential areas reflecting the urban sprawl from Tokyo. To the east, the landscape gradually rises towards the hills of the Hitachi Plateau, influencing local wind patterns. The Kuji River, a vital waterway, flows through the city, providing irrigation and influencing local humidity. Jōsō sits on the edge of a significant agricultural belt, with extensive cultivation of rice, vegetables, and fruits. This proximity to agricultural land, while economically beneficial, can contribute to localized air quality issues related to pesticide use and ammonia emissions. The urban–rural gradient is noticeable, with denser residential areas concentrated closer to the railway line connecting Jōsō to Tokyo, and more rural character prevailing further away. The city’s location within the Kanto Plain, a major industrial and population hub, means it is susceptible to pollutants transported from larger urban centers, particularly during periods of stagnant air. The relatively open nature of the plain allows for both dispersal and accumulation of pollutants, depending on meteorological conditions.

Jōsō’s air quality experiences a distinct seasonal cycle heavily influenced by regional weather patterns. Spring (March-May) often brings a period of increased particulate matter, stemming from agricultural activities like field burning and the resuspension of dust from dry soil. The prevailing westerlies can carry pollutants from industrial areas further west, exacerbating the situation. Summer (June-August) typically sees improved air quality due to increased rainfall and higher temperatures, which promote atmospheric mixing and pollutant dispersion. However, periods of intense heat and humidity can lead to the formation of ground-level ozone, a respiratory irritant. Autumn (September-November) presents a mixed picture. While cooler temperatures and increased rainfall can initially improve air quality, the return of westerlies and the potential for temperature inversions, particularly in October and November, can trap pollutants near the ground, leading to localized episodes of poor air quality. Winter (December-February) is often the most challenging season. Cold, stable air masses frequently lead to temperature inversions, where a layer of warm air sits above cooler air near the surface, preventing vertical mixing. This traps pollutants, including those from residential heating and industrial emissions. Fog, common during winter mornings, further concentrates pollutants. Sensitive groups, including children, the elderly, and individuals with respiratory conditions, should limit outdoor exertion during periods of stagnant air and temperature inversions, particularly in autumn and winter. Monitoring local weather forecasts and air quality reports is crucial for informed decision-making regarding outdoor activities.