Economic-boom-driven electricity demand linked to urban air pollution and health in India
Nature Cities Springer Nature (2026) 1-16
Abstract:
Rapid economic growth in India since 2000 has been accompanied by rising electricity demand and worsening urban air pollution. Here we show that a threefold increase in GDP per capita was associated with a nearly fourfold rise in electricity demand, with coal supplying approximately 76% of total generation. This coal-dependent expansion increased energy-sector SO2 emissions and contributed to a twofold increase in urban aerosol loading, with sulfate accounting for approximately 46% of the urban aerosol burden. Urban PM2.5-attributable deaths increased from approximately 0.7 million in 2000 to 0.9 million in 2020, with increasing contributions from power-sector emissions. Meanwhile, rising incomes increased clean-cooking access from approximately 25% to 75%, accompanied by declining household air-pollution deaths but increasing outdoor air-pollution deaths. These findings highlight contrasting indoor and outdoor air-pollution health consequences of coal-dependent economic growth. This underscores the urgency of decarbonizing electricity generation to improve urban air quality and public health as well as maintaining sustainable economic growth.Coal plants persist as a large barrier to the global solar energy transition
Nature Sustainability Springer Nature 9:7 (2026) 1-12
Abstract:
The global energy transition depends on solar photovoltaic (PV) power displacing fossil fuels to deliver projected climate and air quality benefits. However, aerosol pollution from co-located coal plants actively suppresses PV energy production. Here a global, facility-level dataset shows that aerosols reduced global PV generation by 5.8% in 2023 (111 TWh). From 2017 to 2023, annual aerosol-induced PV energy losses from existing systems were, on average, equivalent to one-third of the energy added by new PV installations. In China, aerosols caused the largest PV energy losses worldwide, reducing national PV generation by 7.7% in 2023. The corresponding annual loss-to-growth ratio averaged 38% and frequently exceeded 50%. Despite continued coal expansion, PV energy losses have declined by 1.4% yr−1 since 2017 owing to stricter emission controls. By contrast, the USA, where co-location of solar and coal plants is limited, experienced only 3.1% aerosol-induced PV loss. Given the slow pace of global coal phase-out, these results reveal a constraint on solar performance that, if unaccounted for, could lead to a systematic overestimation of the transition’s contribution to climate and air quality goals.Characterizing the Saharan dust transported to the UK through lidar ratio, particle depolarization, and spectroscopic measurements
Atmospheric Environment Elsevier 363 (2025) 121613
Abstract:
On 1 May 2024, a Saharan dust plume was observed over Hatfield, UK, and analyzed using a novel spectroscopic lidar system (LITES) developed at the University of Hertfordshire. To the best of our knowledge, this represents the first coordinated study over the UK combining lidar optical properties at 532 nm with a spectrally resolved analysis of a long-range transported Saharan dust event. A distinct dust layer was observed between 2–5 km, with lidar-derived optical thickness values ranging from 0.19 to 0.26 at 532 nm, indicating a low-to-moderate Saharan dust intrusion. Within this layer, the lidar ratio was 53 ± 14 sr and the particle linear depolarization ratio was 0.27 ± 0.02, confirming the presence of non-spherical dust particles. After 4 h, despite the reduction in dust loading, the lidar ratios (mean: 51 ± 11 sr) and particle linear depolarization ratios (0.28 ± 0.01) remained characteristic of Saharan dust. Complementary AERONET observations, collected approximately 10 km from the lidar site, recorded low Å ngström exponent values (0.05–0.2 at 440–870 nm) and a high total AOD of 0.5, with coarse-mode AOD contributing 0.37 (74%) at 500 nm, further confirming the dominance of coarse-mode Saharan dust. Spectrally resolved lidar signals revealed distinct Raman-shifted features near 571.0 nm ± 1.3 nm (1284 ± 40 cm−1) and higher backscatter signals in the 542.9–554.4 nm (377-759 cm−1) range, using a primary emission wavelength of 532 nm. These spectral features persisted throughout the dust layer but were absent in the Raman spectrum of a low-level cloud that was embedded in the dust layer during the lidar observation time. These dust spectral features furthermore disappeared above the dust layer, confirming their attribution to Saharan dust. The spectrally resolved observations are consistent with the Raman spectra of dust samples, which were measured in the LITES laboratory using Raman spectroscopy for direct comparison.Analyzing the observational capabilities of a Moon-based platform for monitoring Earth’s outgoing radiation
Geo-spatial Information Science Taylor & Francis ahead-of-print:ahead-of-print (2025) 1-16
Characterization of dust aerosols from ALADIN and CALIOP measurements
Atmospheric Measurement Techniques European Geosciences Union 17:8 (2024) 2521-2538