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Naryāi ka Puri is situated within the expansive plains of Madhya Pradesh, nestled in the regional influence of the Gwalior division. Its geography is defined by the undulating terrain of the Chambal river basin, characterized by a semi-arid landscape where fertile alluvial soils meet rugged ravines. This specific location places the city at a critical intersection of urban expansion and traditional agrarian life, creating a distinct urban-rural gradient. The surrounding landscape is dominated by intensive agriculture, primarily mustard and wheat cultivation, which significantly impacts the local atmospheric composition. Elevation remains relatively low and consistent, allowing for the unimpeded movement of surface-level winds, yet the proximity to the Chambal's drainage system introduces localized humidity fluctuations. The city’s urban character is a blend of dense residential clusters and sprawling peri-urban fringes, where unpaved roads and construction sites contribute to a high baseline of suspended particulate matter. Regionally, the city sits downwind from various small-scale industrial belts, meaning it often inherits secondary pollutants from neighboring hubs. The lack of significant mountain barriers allows for the transport of regional haze, but the flat terrain also makes the city susceptible to dust storms during the pre-monsoon transition. Consequently, the air quality is a complex interplay between anthropogenic emissions from growing traffic and the natural aeolian processes of the Madhya Pradesh plains, where seasonal crop residue burning further complicates the breathable air quality for its residents.

The air quality in Naryāi ka Puri follows a dramatic seasonal rhythm dictated by the Indian monsoon and temperature fluctuations. During the scorching pre-monsoon summer months, the atmosphere is dominated by coarse mineral dust and heat-induced ozone, as dry winds sweep across the parched plains. This period sees high particulate levels, making midday outdoor activity strenuous. The arrival of the southwest monsoon brings a profound atmospheric cleansing; heavy precipitation effectively scrubs the air of pollutants, leading to the cleanest air of the year between July and September. However, as the rains recede in October and November, a dangerous shift occurs. The transition to winter is marked by the widespread practice of agricultural stubble burning in the surrounding fields, which injects massive quantities of PM2.5 into the boundary layer. This coincides with the onset of winter temperature inversions, where a layer of warm air traps pollutants close to the ground, preventing vertical dispersion. December and January are the most critical months, as dense fog often merges with smog, creating hazardous conditions for respiratory health. Sensitive groups, including children and the elderly, should strictly limit outdoor exposure during these winter mornings. To maintain health, residents are encouraged to favor the monsoon window for outdoor exercise and employ air purification or masks during the peak burning season in late autumn, ensuring protection against the stagnant, pollutant-heavy air typical of the region's winter climate.