K. Huang
NYU Shanghai campus in Pudong, Shanghai

About

I study cities as complex socio-ecological systems, the outcome of interactions between human and natural systems. At New York University Shanghai I lead the CLimate and Urban Environments (CLUEs) Lab. We combine satellite data, climate models, and causal inference across thousands of cities, and ask how the amount, height, and arrangement of what we build shapes who overheats, who floods, and how much material a city consumes.

We have shown that denser neighborhoods need disproportionately less built mass (Nature Cities, 2026), that larger homogeneous building clusters cool daytime heat islands (PNAS, 2026), and that taller, better-protected cities change where flood damage lands (Scientific Reports, 2026).

Before New York University Shanghai, I was an Advanced Study Program Postdoctoral Fellow at NCAR. I earned my PhD at the Yale School of the Environment.

Selected Publications

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  • At the neighborhood scale, doubling population density only increases built mass by about 68% (δ ≈ 0.75) — economies of scale intensify inside the city versus city-level scaling (β ≈ 0.90)
  • Analyzes over 3,000 cities globally to reveal universal sub-linear scaling of built mass with population, with a city-level scaling exponent of β ≈ 0.90 meaning larger cities use less built mass per capita
  • Proposes a theoretical framework showing that city-level sub-linear scaling emerges from the aggregation of within-city neighborhood-level disparities, establishing a nested multi-scale scaling relationship
  • Redefines 'over-built' and 'under-built' conditions as deviations from expected scaling patterns, linking excess built mass to environmental impact and deficient built mass to inadequate living standards
Animation: nested economies of scale in global city mass
urban scaling lawsZipf's lawcity size distributionbuilt massurban allometryurban economics
  • Introduces the Urban Homogeneous Scale (UHS) metric — the spatial scale of functionally homogeneous building clusters — as a novel urban morphology measure for understanding urban heat island effects
  • Analyzes 232,874 observations across 101 global cities using machine learning (XGBoost) building classification and Double Machine Learning causal inference to establish UHS-heat relationships
  • Finds that a 100-metre increase in UHS leads to approximately 5% decrease in daytime urban heat island intensity, with daytime cooling more pronounced in inland, humid, and high-income regions
  • Proposes homogeneous scale planning as a land-use strategy for mitigating urban heat, with implications for mixed-use zoning and urban design guidelines
urban heat islandUrban Homogeneous Scaleurban morphologyclimate adaptationurban planningcausal inferencemachine learning
  • Across the 1,000 largest global cities (2003–2020), declining urban population density attenuates the rise in population-weighted surface urban heat island extremes by approximately 0.5 K per decade per 1,000 persons/km²/year decrease in density
  • Cities undergoing densification face disproportionately greater increases in population-weighted exposure to surface heat extremes compared to area-average trends
  • Vegetation changes show a moderate association with population-weighted heat exposure (R² = 0.56), while variations in surface albedo exhibit a negligible relationship (R² = 0.03)
  • Highlights the need for strategic urban planning that balances compact development co-benefits against amplified heat exposure risks in rapidly densifying cities
urban densityheat exposuresurface urban heat islandurban sprawlclimate equitysatellite land-surface temperature
  • Integrating building height and protection standards shifts the global flood damage distribution: Southeast Asia accounts for 42% of damages versus only 15% under conventional flood-depth-only assessments
  • Sole reliance on flood depth overestimates risk in regions with resilient vertical urban forms and robust protection (e.g., Europe, East Asia) while underestimating it in areas with low-rise, unprotected development
  • Chinese cities show strong dependence on protection systems that can reduce potential flood damages by over 90%, as illustrated by Wuhan where damages drop to 0.12%–0.17% after accounting for its 100-year protection standard
  • Countries such as Vietnam, Cambodia, Bangladesh, Thailand, and Pakistan show high vulnerability, with more than 30% of building footprints located within floodplains
urban flood risk3D flood assessmentbuilding heightflood protection standardsclimate riskglobal flood modeling

FAQ

What does Kangning Huang research?
Kangning (Ken) Huang researches how urbanization and climate change together affect vulnerability to environmental hazards. His work spans urban expansion modeling, urban heat island dynamics, climate adaptation trade-offs, and urban scaling laws. He develops global-scale urbanization scenarios to explore possible urban climate futures.
Where does Kangning Huang work?
Kangning Huang is an Assistant Professor of Environmental Studies at NYU Shanghai, where he leads the CLUEs (CLimate and Urban Environments) Lab. He received his PhD from Yale University's School of the Environment and was a postdoctoral fellow at the National Center for Atmospheric Research (NCAR).
What is urban heat island research?
Urban heat islands occur when cities become significantly warmer than surrounding rural areas due to built surfaces absorbing and re-emitting heat. Kangning Huang's research shows that global urban expansion through 2050 could intensify urban heat islands by 0.5–0.7 °C on average (up to about 3 °C locally), with nighttime heat stress persisting even when mitigation measures reduce daytime heat islands.
How much will cities expand by 2050?
According to research published in Environmental Research Letters (2019), global urban land area is projected to increase by 78%–171% (0.6–1.3 million km²) between 2015 and 2050, intensifying urban heat islands by 0.5–0.7 °C on average (up to about 3 °C locally) and increasing extreme heat risk for about half of the future urban population.