Sami Air Quality Index (AQI)

Loading live AQI data...

Loading weather snapshot...

Loading historical AQI trends...

Sami, a small city in Gujarat, India, situated at 23.6872°N, 71.7786°E, occupies a relatively flat terrain within the broader Indo-Gangetic Plain. Its location in the eastern part of Gujarat places it within a region experiencing a gradient between the arid coastal areas and the more fertile inland agricultural zones. The city’s elevation is low, contributing to limited atmospheric dispersion of pollutants. Sami is not directly on the coast, but is influenced by the monsoon winds originating from the Arabian Sea, approximately 100km to the west. Surrounding Sami are predominantly agricultural lands, primarily cotton and groundnut cultivation, with increasing, though currently limited, industrial activity concentrated around nearby larger towns like Himmatnagar. The urban-rural gradient is quite sharp; Sami itself is a relatively small urban centre surrounded by extensive rural farmland. This proximity to agricultural practices introduces potential sources of particulate matter from crop residue burning and fertilizer use. The lack of significant topographical features – hills or valleys – hinders natural ventilation, exacerbating pollution build-up, particularly during calmer weather conditions. The regional climate is semi-arid, with hot, dry summers and mild winters, influencing pollutant behaviour. The city’s air quality is therefore intrinsically linked to both agricultural practices and the prevailing meteorological conditions.

Sami’s air quality follows a distinct seasonal pattern. The post-monsoon period, from October to November, often sees a deterioration in air quality due to the practice of agricultural stubble burning in surrounding fields, releasing significant amounts of particulate matter. Cooler temperatures and calmer winds during these months trap pollutants near the ground. December and January bring relatively cleaner air, benefiting from slightly higher wind speeds and occasional rainfall, though temperature inversions can still occur, trapping pollutants. The pre-monsoon months of March to May are characterised by rising temperatures and dust storms, leading to increased levels of coarse particulate matter. The summer heat creates strong convective currents, offering some dispersion, but also exacerbates ozone formation. The monsoon season, from June to September, generally provides the cleanest air, as rainfall washes away pollutants and high humidity suppresses dust. However, increased cloud cover can also lead to temperature inversions. Sensitive groups – children, the elderly, and those with respiratory conditions – should avoid prolonged outdoor activity during October-November and March-May. Monitoring local weather patterns is crucial, as wind direction significantly impacts pollutant concentration. Staying indoors during peak pollution periods and using air purifiers are recommended.