Compound urban extremes weaken the cooling efficacy of super cool broadband materials in cities
Delhi, one of the fastest-warming megacities globally, frequently experiences compound urban extremes. This study evaluates the radiative–dynamic performance of super cool broadband materials under compound urban extremes. During peak heat episodes, super cool broadband materials can reduce surface temperature by up to 6.3 °C, roof temperature to 34.8 °C, and ambient air temperature by 3.2 °C, with an urban-average cooling of 2.9 °C. Reduced net radiation limits sensible heat flux, weakens buoyant turbulence, and suppresses vertical momentum exchange, resulting in enhanced mesoscale stabilization following surface cooling. Additionally, convective fluxes decline, lowering wind speed by 3.2 m s −1 and planetary boundary-layer height by 752.6 m. Under high-humidity conditions (>75 %), elevated atmospheric water vapor narrows the radiative window and increases downward longwave flux, while enhanced latent heat flux reduces sensible heat release. Net radiation decreases by 276 W m −2 , surface temperature falls by 5.2 °C, roof temperature reaches 30.4 °C, and ambient air cools by 2.4 °C, accompanied by a 9.6 % rise in relative humidity and reductions in wind speed and boundary-layer height to 2.7 m s −1 and 677.1 m. During severe PM₂.₅ pollution (>100 μg m −3 ), aerosol scattering and absorption further reduce insolation, lowering net radiation by 265 W m −2 and causing 4.7 °C surface and 2.2 °C ambient cooling. The optical design of super cool broadband materials sustains reflectivity and emissivity under heat, humidity, and aerosol-laden skies, maintaining a net radiative deficit and converting urban surfaces from heat sources into radiative sinks, enabling robust, condition-sensitive cooling under Delhi’s combined extremes. • Aerosol–heat–humidity interactions alter urban surface radiative forcing and convection. • Super-cool broadband materials cooled surface 6.3 °C and ambient 3.2 °C under dry heat. • High humidity and aerosols curtailed infrared emission and solar reflection, reducing cooling. • Reduced surface cooling weakened turbulence and boundary-layer ventilation in cities. • Radiative–convective feedbacks govern cooling efficacy and climatic trade-offs of materials.
Authors
- Deepak Amaripadath (ORCID: https://orcid.org/0000-0003-2822-5749)
- Rafiq Hamdi
- Jyotirmoy Mandal (ORCID: https://orcid.org/0000-0001-8124-5234)
- Hashem Akbari (ORCID: https://orcid.org/0000-0001-8808-8112)
- Samiran Khorat (ORCID: https://orcid.org/0000-0002-6276-9005)
- Thanh-Hung Nguyen (ORCID: https://orcid.org/0000-0001-6290-2841)
- Dev Niyogi (ORCID: https://orcid.org/0000-0002-1848-5080)
- Mattheos Santamouris
- Asfa Siddiqui
- Ansar Khan
- Rupali Khatun
Institutions
- University of Calcutta (IN)
- Royal Meteorological Institute of Belgium (BE)
- Planetary Science Institute (US)
- National University of Singapore (SG)
- Jadavpur University (IN)
- Princeton University (US)
- UNSW Sydney (AU)
- Indian Institute of Remote Sensing (IN)
- Arizona State University (US)
- Concordia University (CA)
- The University of Texas at Austin (US)
Publication Details
- Journal
- Urban Climate
- Published
- 2026-01-05
- DOI
- https://doi.org/10.1016/j.uclim.2025.102761
- Primary Topic
- Urban Heat Island Mitigation
- Type
- article
- Field-Weighted Citation Impact
- 0.00