Urban Climate · 2026

Where ERA5-Land Misses Urban Heat

A UK-wide, observation-led evaluation of air temperature and dew point biases—and what those biases mean for heat exposure, mortality risk and building energy analysis.

Junjie Yu, Wenyuan Li, Lingcheng Li, Divya Kumar, Hongyu Sun, David O. Topping, Guoqiang Tang & Zhonghua Zheng

Research demo only. This page highlights the study's central evidence. Read the full article below for the complete data processing, statistical methods, assumptions, uncertainty and limitations.

Evaluation framework

From observations to consequences

The study goes beyond error statistics by tracing reanalysis bias through multiple urban-climate applications.

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Observe

Quality-controlled hourly air temperature and dew point records from the Met Office MIDAS network.

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Match

Elevation-adjusted ERA5-Land time series aligned with observations at the nearest grid cells.

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Stratify

Station environments characterized using local and grid-scale impervious surface area.

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Propagate

Biases evaluated across heat exposure, mortality-risk and building-energy case studies.

Observation record

A warming signal, station by station

The animated MIDAS record shows the evolution of annual mean air temperature across the selected long-term UK stations. The aggregated observational trend is 0.20°C per decade.

0.20°Cper decade · MIDAS
Animated annual MIDAS station temperatures from 1990 onward, showing a UK warming trend of 0.20 degrees Celsius per decade
Animated annual MIDAS trend. The study reports 0.18°C per decade for ERA5-Land, compared with 0.20°C per decade in the observations.

Core evidence

Useful reanalysis—with an urban blind spot

ERA5-Land captures broad patterns, but smooths temperature variability and increasingly underestimates warmth as the surrounding built fraction rises.

Observation scale

14.9M

Hourly records from 64 long-term stations support the temporal evaluation.

Daily maximum

−0.66°C

ERA5-Land underestimates daily maximum air temperature.

Daily minimum

+0.44°C

ERA5-Land overestimates daily minimum air temperature.

Urban sensitivity

30–50%

Indicative ISA transition range above which the cold bias becomes more pronounced.

Compressed temperature range

Maximums are too cool while minimums are too warm: the amplitude of observed temperature is damped.

Daily maximum bias−0.66°C
Daily minimum bias+0.44°C

Built-up environments matter

More ISA → stronger cold bias

Local impervious cover and insufficient representation of urban surfaces within the ERA5-Land grid jointly shape the underestimation.

Bias propagation

Small climate biases can change decisions

HEAT EXPOSURE

Too few extreme-heat hours

Annual extreme-heat exposure is underestimated in both urban and rural areas.

HEALTH

>10% heat-mortality bias

The Greater London case study can underestimate heat-attributable deaths by more than 10%.

ENERGY

Demand shifts

Cooling demand is underestimated by 2.90–3.14%, while heating demand is overestimated by 3.11–3.38%.

Full research article

Read beyond the demo

Complete methods, evaluation, impact case studies and limitations.

Yu, J., Li, W., Li, L., Kumar, D., Sun, H., Topping, D. O., Tang, G., and Zheng, Z.: Evaluating ERA5-Land air temperature and dew point biases in built-up environments in the UK, Urban Climate, 69, 103088, 2026.

Collaborators: Pacific Northwest National Laboratory, Microsoft AI, and Wuhan University.

🎧 Audio:
🇨🇳 中文
🇬🇧 English

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