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Moḩammadābād sits within the rugged, semi-arid landscape of the Kermān Province, positioned on the high-altitude fringes of the Iranian plateau. The geography is defined by a stark transition between the undulating, rocky foothills and the vast, unforgiving expanse of the surrounding desert ecosystems. This specific regional position, characterized by significant elevation and relatively low humidity, creates a unique atmospheric environment. The city acts as a transitional node between local agricultural pockets and the more desolate, wind-swept plains that characterize much of southeastern Iran. Because the terrain is marked by depressions and surrounding hills, the local topography plays a critical role in how air masses move through the urban fabric. The absence of large, cooling bodies of water means that the local microclimate is heavily dictated by solar radiation and thermal shifts. Furthermore, the proximity to arid, unshielded land makes the area susceptible to the transport of fine particulate matter. As the urban–rural gradient shifts from the concentrated settlement of Moḩammadābād to the sparsely populated outskirts, the primary source of airborne matter transitions from localized anthropogenic activities to natural aeolian processes. The landscape's openness allows for rapid wind-driven transport of dust, yet the surrounding topographical features can also facilitate stagnant air conditions. Consequently, the city’s air quality is a complex interplay between the regional desert dynamics and the localized thermal behavior of the high-altitude Kermān plateau, influencing everything from visual clarity to long-term respiratory health for the local population living within this environment.

The atmospheric cycle in Moḩammadābād is dictated by the harsh transitions of the Iranian interior. During the spring and early summer, the air quality often faces challenges from increased wind activity. As temperatures rise, thermal turbulence can lift fine desert dust into the breathing zone, leading to periods of reduced visibility and heightened particulate concentrations. These seasonal dust events are particularly prevalent when dry winds sweep across the nearby arid basins. Conversely, the summer months bring intense heat, which can exacerbate the presence of ground-level ozone through photochemical reactions, though the primary concern remains particulate matter. As autumn transitions into winter, the meteorological narrative shifts significantly. The onset of cooler temperatures often brings about temperature inversions, where a layer of warm air traps cooler, denser air near the ground. This phenomenon is most common during the late evening and early morning hours in the winter months, causing local emissions from heating and transport to accumulate within the valley-like depressions of the landscape. To maintain optimal health, residents should favor outdoor activities during the mid-day period in winter when the inversion layer might be less stable, or during the calmer, post-storm periods in spring. Sensitive groups, including children and the elderly, should monitor local conditions closely during the winter months and high-wind spring days. Wearing high-filtration masks during dust events is highly recommended to mitigate the inhalation of fine desert silicates and protect overall health. This cyclical pattern requires constant vigilance from all residents living in this unique and arid environment.