G-P05 · TOPIC · buildings-and-heatGCRI dossier · service level R0
GCRICities and Built EnvironmentIn development
Topic dossier · Cities and Built Environment

Buildings and heat

Cities are hotter than their surroundings, and their buildings decide how much of that heat reaches the people inside. Dark surfaces, dense construction, little shade and waste heat raise urban temperatures, while poorly insulated or unventilated homes trap heat at night. This page sets out how urban heat develops, how it is measured inside and out, and what evidence serves the health, housing and city authorities that respond to it.

The interactive map needs JavaScript; the layer list and sources are below.

Layers 3

Climate signals, for this page

Latest available

NASA GIBS / EOSDIS · ASTER GDEM (METI, NASA) · Blue Marble (NASA) · © OpenStreetMap contributors (ODbL) · Natural Earth

Loading the latest NASA imagery.

Drag to move. Ctrl or ⌘ and scroll, pinch or the buttons to zoom; hover for the values under the pointer; reset returns to the region.

For buildings and heat, in GCRI's spatial-intelligence reading, the map opens on daytime surface heat, true-colour imagery and population density with relief in 3D, a past-year temperature and sunshine chart at the centre and true colour from NASA GIBS, framed on India; 3 further NASA layers wait in the list.Satellite and model products as NASA publishes them, each with its own date; indicators, not assessments of any place; claim ceiling INTEGRATED.

Data: NASA GIBS · ASTER GDEM · Blue Marble · © OpenStreetMap contributors · Natural Earth · NASA EONET · Copernicus Sentinel-2 L2A · NASA HLS S30Sources and licences

  • We acknowledge the use of imagery provided by services from NASA's Global Imagery Browse Services (GIBS), part of NASA's Earth Science Data and Information System (ESDIS). Colours redrawn from the published colour map; values averaged into H3 cells where shown (modified). NASA open data
  • We acknowledge the use of imagery provided by services from NASA's Global Imagery Browse Services (GIBS), part of NASA's Earth Science Data and Information System (ESDIS). Colours redrawn from the published colour map; values averaged into H3 cells where shown (modified). NASA open data
  • VIIRS near-real-time products (flood, land surface temperature, snow cover, corrected reflectance), NASA LANCE; imagery via NASA GIBS. Colours redrawn from the published colour map; values averaged into H3 cells where shown (modified). NASA open data
  • Center for International Earth Science Information Network (CIESIN), Columbia University. 2018. Gridded Population of the World, Version 4 (GPWv4): Population Density, Revision 11. NASA Socioeconomic Data and Applications Center (SEDAC). Licensed under CC BY 4.0. Colours redrawn from the published colour map; values averaged into H3 cells where shown (modified). CC BY 4.0
  • VIIRS Black Marble night-time lights, NASA Goddard Space Flight Center; distributed by the NASA Level-1 and Atmosphere Archive and Distribution System (LAADS DAAC); imagery via NASA GIBS. Colours redrawn from the published colour map; values averaged into H3 cells where shown (modified). NASA open data
  • MODIS land products (vegetation indices, gross primary production, land cover), NASA LP DAAC and LANCE; imagery via NASA GIBS. Colours redrawn from the published colour map; values averaged into H3 cells where shown (modified). NASA open data
  • ASTER GDEM is a product of METI and NASA (ASTER Global Digital Elevation Model V003, NASA LP DAAC); imagery via NASA GIBS. Colours redrawn from the published colour map; values averaged into H3 cells where shown (modified). NASA open data
  • Made with Natural Earth. Free vector and raster map data @ naturalearthdata.com. Public domain
  • © OpenStreetMap contributors (ODbL), via NASA GIBS (coastlines, boundaries, roads and place names). Colours redrawn from the published colour map; values averaged into H3 cells where shown (modified). ODbL
  • Blue Marble, NASA Earth Observatory; imagery via NASA GIBS. Colours redrawn from the published colour map; values averaged into H3 cells where shown (modified). NASA open data
  • Context on the globe and flat map: coastlines, boundaries, roads and place names from NASA GIBS reference layers (OpenStreetMap data, ODbL, © OpenStreetMap contributors); Blue Marble imagery as an optional base; 3D terrain and the elevation read-out from the ASTER GDEM elevation colour index (5 m to 200 m classes, exaggerated for legibility). Boundaries are drawn as published and imply no position on any territory.
  • Globe: MapLibre GL JS 6.9.1, BSD-3-Clause, © MapLibre contributors.
  • Live: NASA EONET Events are indicative, not official warnings.
  • Observed (EO): Copernicus Sentinel-2 L2A (contains modified Copernicus Sentinel data 2026), Microsoft Planetary Computer
  • Observed (EO): NASA HLS S30 (contains modified Copernicus Sentinel data 2026). We acknowledge the use of imagery provided by services from NASA's Global Imagery Browse Services (GIBS), part of NASA's Earth Science Data and Information System (ESDIS).
  • Optional layers (24 sources in the layer list: live, forecast, observed and context) print their provider credit on the map and here when switched on; forecasts are model output and derived indices are estimates.

Layers and dates

  • Land surface temperature, day, 8-day composite: VIIRS NOAA-20 Level 3, 8-day, NASA LANCE · 14 Sep 2026
  • True colour: VIIRS NOAA-20 corrected reflectance, NASA LANCE · 13 Oct 2026
  • Population density, 2020: Population: CIESIN, Columbia University, Gridded Population of the World v4.11 (2018), NASA SEDAC, CC BY 4.0 · static
  • Land surface temperature, night, 8-day composite: VIIRS NOAA-20 Level 3, 8-day, NASA LANCE · 14 Sep 2026
  • Night-time lights, daily: VIIRS Black Marble (VNP46A2), NASA LAADS DAAC · 12 Oct 2026
  • Land cover type (IGBP), yearly: MODIS Terra and Aqua land cover (MCD12Q1), NASA LP DAAC · 2024

01In brief

The short answer.

Urban heat is the extra heat that cities generate and trap, through dark surfaces, dense construction, little vegetation and waste heat. Buildings decide how much reaches people indoors, and exposure falls hardest on older, ill and poorly housed residents. Satellites, stations and indoor sensors measure different parts of it.

02Console

Urban heat console, in outline.

The working screen behind this subject: its structure, terms and states. Names are placeholders and values illustrative.

Urban heat console: the screen's structure, terms and states for Buildings and heat.Placeholder names and illustrative values; a design, not a record or a live system.
03The question

Buildings and heat: how the risk develops.

Building performance and urban heat. The dossier below sets out how the risk develops, what is measured, where the data come from, how it is modelled and who decides.

Mechanism

The urban heat island

Paved and built surfaces absorb sunlight and release it slowly, while less vegetation means less evaporative cooling. Cities stay warmer than rural areas, especially at night.

Mechanism

Indoor heat follows the building

Insulation, orientation, glazing, ventilation, thermal mass and roof colour set indoor temperatures. Top-floor flats and lightweight roofs can be much hotter than outside air.

Mechanism

Exposure is unequal

Older people, those with chronic illness, outdoor workers and people in poor housing face the greatest risk. Hot neighbourhoods often have fewer trees and poorer housing.

Mechanism

Cooling raises demand

Air conditioning protects health but raises electricity demand and waste heat. Peak demand during heatwaves can strain grids, and those who cannot afford cooling remain exposed.

04Key terms

Terms used on this page.

Each term as this page uses it. Where a standard-setting body defines the term, the wording follows that body.

TermDefinition
Land surface temperatureThe temperature of the ground and building surfaces as measured by satellite thermal sensors.
Indoor overheatingIndoor temperatures high enough to cause discomfort or health risk, judged against stated criteria.
Heat-health action planA plan that sets warnings, actions and responsibilities to protect health during hot weather.
05Indicators

What is measured, and how well.

Each indicator carries its unit, its cadence, the kind of source behind it and the evidence label a value would carry. No values are shown: a programme supplies them under its own authority.

IndicatorUnitCadenceSource typeLabel
Land surface temperaturedegrees Celsiusper satellite overpassSatellite thermal imageryOBSERVED
Air temperature difference urban to ruraldegrees CelsiushourlyUrban and reference weather stationsOBSERVED
Indoor temperature in monitored dwellingsdegrees CelsiushourlyIndoor sensorsOBSERVED
Tree canopy coverpercent of areaper assessmentAerial and satellite imageryOBSERVED
Heat-related excess mortalitydeaths above expectedper heat seasonMortality statistics and modelsESTIMATED
Households with access to coolingpercent of householdsper surveyHousehold surveysREPORTED
06Canvas

From sources to decisions.

The topic as a computational graph: named sources feed the methods, an evidence review gates the outputs, and the decisions stay with the authorities that hold them.

Pipeline canvas · Buildings and heat as a run graphDesign, not a record
Buildings and heat: asset register to adaptation optionsThe asset register is overlaid on hazard layers to find exposure; vulnerability classes turn exposure into expected damage; assets are ranked and adaptation options costed into the capital plan. Design of the process, not a record of a run.

Fig. 02Nodes carry their type, two metric rows and a state; connectors show what feeds what; dashed frames name the owners; the timeline is the cadence. Design of the pipeline, not a record of a run.

07Sources

Where the evidence comes from.

Named public datasets and institutional records, each with its licence class. Sources by agreement are used only under their terms and never republished.

SourceWhat it givesLicence class
Landsat Collection 2 surface temperature (USGS)Land surface temperature at thirty-metre resolutionPublic domain, US government data
ECOSTRESS (NASA)Land surface temperature at different times of dayOpen, NASA data policy
Copernicus Urban Atlas and street tree layerUrban land use and trees for European citiesFree, Copernicus terms
WHO and WMO heat-health guidanceHeat-health action planning and warning systemsPublic, WHO and WMO terms of use
IEA cooling and buildings dataCooling demand and appliance ownershipLicence per dataset (to check)
08Decisions

Who decides, and what the evidence serves.

Cities and Built Environment prepares evidence. The decisions below are taken by the authorities named, under their own rules, and never by the platform.

Who decidesThe questionEvidence this page serves
City governmentsWhere to plant trees, add shade and cool surfaces firstHeat maps; canopy cover; vulnerability profiles
Public health agenciesWho to reach and when during heatwavesVulnerability profiles; excess mortality evidence
Building regulators and housing agenciesWhich standards and retrofits prevent indoor overheatingIndoor overheating assessments

Outputs this topic produces

  • Urban heat maps combining satellite, station and sensor evidence
  • Indoor overheating assessments for housing types
  • Heat vulnerability profiles by neighbourhood
  • Evidence notes for heat-health action plans
09Core questions

What experts ask.

  1. 01

    Where is heat most dangerous?

    Which neighbourhoods and building types reach the highest indoor and outdoor temperatures.

  2. 02

    Who is most at risk?

    Older people, people living alone, those with chronic illness, outdoor workers and residents of top-floor or poorly ventilated homes.

  3. 03

    What reduces indoor heat?

    The effect of shading, insulation, ventilation, reflective surfaces and thermal mass.

  4. 04

    How does cooling affect the grid?

    How rising air-conditioning demand interacts with power supply during heatwaves.

10Mechanisms

What drives the risk.

The urban heat island arises because built surfaces absorb and store solar energy and release it slowly, vegetation and evaporation are reduced, and vehicles, industry and cooling equipment add waste heat. Night-time warmth is particularly harmful because bodies cannot recover.

Indoor conditions depend on design. Lightweight roofs, large unshaded glazing and poor ventilation can make homes hotter than outdoors. Insulation helps or harms depending on climate and ventilation. Mechanical cooling protects occupants but raises electricity demand and adds heat outside.

Heat risk is social. Isolation, poverty and illness turn high temperatures into deaths, which is why public health and housing must be considered together.

11Methods and limits

How evidence is gathered, and where it stops.

Method or dataWhat it showsIts limit
Thermal satellite imagerySurface temperature patternsSurface is not air or indoor temperature
Street and indoor sensorsActual temperatures people experienceSparse networks, calibration needs
Building energy simulationPerformance of design optionsDepends on occupant behaviour assumptions
Health recordsHeat-related illness and mortalityUnder-recording and attribution limits
13Questions

Questions and answers.

What is the urban heat island?
The tendency of cities to be warmer than their rural surroundings, especially at night, because built surfaces store heat and there is less vegetation and evaporation.
Why is land surface temperature different from air temperature?
Satellites measure how hot surfaces are, which can be far hotter than the air above them in sun. Air temperature and humidity govern human heat stress.
How can buildings stay cooler?
Through shading, insulation, reflective roofs, ventilation and thermal mass, and in the street through trees and green space, guided by local climate and building codes.
Is air conditioning the answer to urban heat?
It protects occupants, but it raises electricity demand and outdoor heat. Passive design, shading and greening reduce the need for it.
Does the platform issue heat warnings?
No. Heat-health warnings come from mandated public health and meteorological authorities.
Why does night-time temperature matter?
Because people recover from daytime heat at night. Warm nights in dense districts are strongly associated with heat-related harm.
Cities and Built Environment

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