Aerosol intelligence

The atmosphere,
under observation.

Investigating atmospheric optical depth, UV absorption, seasonal variability, and Earth system relationships across Punjab.

describes how strongly particles absorb ultraviolet light. It is different from AOD, which measures how much sunlight all particles block together.
Punjab · extraction-area observations
Sen trend / decade
+0.04744
Sen confidence interval not supplied
Estimated total change
—
Total change not supplied
Seasonal Mann–Kendall p
0.0892
Not significant at p < 0.05
Valid observations
252
252 / 252 months · 100.0% coverage

Aerosol index is increasing over the selected record. This is an area-averaged satellite signal, not a measurement of ground-level pollution or proof of a cause.

Aerosol index through time

Aura OMI · OMAERUVd v003 · Punjab study box; exact coordinates not supplied in CSV

Trend: 0.0474 per decade (p = 0.0892, not significant)

Area-averaged monthly retrievals. Annual values use available months; coverage is listed below.

Season-adjusted trend and 95% confidence band

Supplied OLS fit, deseasonalized monthly values and pointwise 95% confidence band

Monsoon versus winter

Winter Dec–Feb · monsoon Jun–Sep · means of valid selected months

Monsoon mean
0.626047
Winter mean
0.584971

Two instruments, one winter signal

AOD (MODIS) and Aerosol Index (OMI) both rise significantly in winter, and neither changes significantly in the monsoon. Supplied monthly correlation: r = 0.34.

Consistent with growing smoke and pollution in winter; satellite data alone can't prove the source.

Monthly climatology

Annual means & data coverage

YearMean aerosol indexMonthsCoverage
2005-01-010.58454412/12Eligible annual mean
2006-01-010.61567212/12Eligible annual mean
2007-01-010.48933912/12Eligible annual mean
2008-01-010.60605812/12Eligible annual mean
2009-01-010.57398612/12Eligible annual mean
2010-01-010.63379312/12Eligible annual mean
2011-01-010.49088212/12Eligible annual mean
2012-01-010.62522412/12Eligible annual mean
2013-01-010.51950412/12Eligible annual mean
2014-01-010.62121912/12Eligible annual mean
2015-01-010.57160012/12Eligible annual mean
2016-01-010.69556612/12Eligible annual mean
2017-01-010.75053412/12Eligible annual mean
2018-01-010.90381312/12Eligible annual mean
2019-01-010.59622412/12Eligible annual mean
2020-01-010.56703012/12Eligible annual mean
2021-01-010.78704112/12Eligible annual mean
2022-01-010.64065712/12Eligible annual mean
2023-01-010.55272312/12Eligible annual mean
2024-01-010.57753712/12Eligible annual mean
2025-01-010.61743812/12Eligible annual mean
UV Aerosol Index · supplied seasonal findings and cleaning notes

The UV Aerosol Index detects particles that absorb sunlight, mainly smoke and desert dust. Higher = more absorbing haze. It helps separate smoke and dust from other pollution.

OMI on NASA's Aura satellite · OMAERUVd v003 · daily, 1° · area-averaged over the supplied Punjab study box · NASA Giovanni. Exact box coordinates were not included in these CSVs.

Winter absorbing haze is rising.

Supplied findings cover January 2005–December 2025, regardless of chart date filters. Whole year: no significant trend.

Winter Sen slope / decade
+0.218
p = 0.0004
Significant
Whole-year seasonal Sen / decade
+0.047
p = 0.089
Not significant
OLS anomalies / decade
+0.045
p = 0.065
Not significant
Yearly averages / decade
+0.030
p = 0.291
Not significant

OLS 95% slope CI: −0.003 to +0.093 per decade. Autocorrelation-adjusted OLS p = 0.248. Winter also passes the stricter four-season threshold, 0.05 ÷ 4 = 0.0125.

UV Aerosol Index through time

252 selected months · baseline 2005–2025

Highest month: Nov 2020 (1.622). Lowest: Mar 2005 (0.083). Rolling values require 12 consecutive months. Anomalies, fitted lines and confidence bounds are read directly from the supplied CSV.

Yearly averages

Seasonal cycle · 2005–2025 normal

Season by season

SeasonMeanSen / decadepSeasonal meansEvidence (four-season correction)
Winter (Dec-Feb)0.586+0.2180.000420Significant
Pre-monsoon (Mar-May)0.514-0.0520.45021Not significant
Monsoon (Jun-Sep)0.626-0.0880.05721Not significant
Post-monsoon (Oct-Nov)0.819+0.1270.04321Weak evidence

Post-monsoon: weak evidence (+0.127 per decade, p = 0.043); it does not pass the stricter threshold. Monsoon and pre-monsoon: no significant trend. Winter uses complete December–February seasons, 2006–2025.

Two instruments, one winter signal

AOD (MODIS) and Aerosol Index (OMI) both rise significantly in winter, and neither changes significantly in the monsoon. Supplied monthly correlation: r = 0.34.

Consistent with growing smoke and pollution in winter; satellite data alone can't prove the source.

How we cleaned the data

450 days were missing (NASA fill values). We removed 239 more days (3%) that were sensor artifacts: values up to 34, jumping on alternate days in a repeating pattern linked to OMI's known 'row anomaly'. We used a Hampel filter (more than 4 robust standard deviations from the 15-day median) plus a cap at 5. Every month keeps at least 18 valid days.

Cleaning sensitivityWhole-year p
None0.0003
Cap only0.050
Hampel 15-day (k=3)0.074
Hampel 31-day (k=3)0.119

The winter rise is significant under every method; the whole-year trend is not robust.

Sensitivity runs use k=3; the supplied primary clean series uses k=4. Findings are supplied statistics, not recalculated here.

Download daily raw & clean data

Download data

Relationships, not assumptions.Albedo and AOD extraction extents differ. UV Aerosol Index uses supplied cleaned OMI observations and supplied 2005–2025 findings. No environmental values are inferred between variables.