Compare temperature, humidity and altitude across all 16 World Cup 2026 stadiums.

This tool lets you compare climate conditions across every World Cup 2026 stadium. Select one or more stadiums, switch between temperature, humidity and altitude, and see how the venues differ at a glance.

Data and visualization by Tales of the Stands. Sharing is allowed with clear credit and a link to this page. Commercial reuse is not permitted without permission.

How to Use

Start at the top with Main Sorting Topic. This decides the order of the chart. If you choose temperature, the stadiums are ranked from the hottest to the coolest. If you choose humidity, the most humid stadium comes first. If you choose altitude, the highest stadium comes first. This is the easiest way to control what the chart is mainly showing.

Then move to Show in Chart. Here you choose which climate data you want to see as bars. You can turn temperature, humidity and altitude on or off. Selecting one gives you a simple, clean ranking. Selecting two or three lets you compare different conditions side by side for each stadium. After that, go to Choose Stadiums. Here you can keep all 16 stadiums, search for a specific one, or build your own smaller selection. This is useful when you want to compare only a few venues directly.

At the bottom you can use Quick Picks. These are shortcuts that instantly load useful groups. The warmest stadiums, the highest stadiums or the most humid stadiums. Once you have chosen your sorting topic, chart topics and stadiums, read the chart from left to right. The tallest and most important values appear first because the order always follows your selected sorting topic. Hover over the bars to see the exact figures, then use the summary and the cards underneath to quickly spot the biggest standout, the lowest point and the biggest gap in your selection

Why Climate matters at the World Cup 2026

Football is usually discussed in terms of tactics, form and individual quality. Yet every match is also played inside a physical environment. Temperature, altitude and humidity influence how the body performs during ninety minutes of high intensity sport. Even small differences in climate can change how quickly players fatigue. How often they need to hydrate. How much energy they can sustain in pressing or repeated sprints.

The 2026 tournament is unusual because the host stadiums are spread across a vast geographical area. Matches take place from the Pacific coast of Canada to the humid subtropical climate of southern Florida and the high plateau of central Mexico. Teams will encounter very different environmental conditions within only a few days. Adapting to those changes becomes part of tournament preparation alongside tactics and squad rotation.

Climate does not determine the outcome of matches on its own. The strongest teams still rely on technical ability, organization and decision making. Environmental conditions do shape the physical demands placed on players. Heat can slow the tempo of a game, humidity can increase fatigue and altitude can alter how quickly the body recovers between intense actions. Across sixteen stadiums and three countries the climate becomes another variable that teams must manage throughout the tournament.

Data and Methodology

Altitude
Altitude was measured at the stadium site itself. Stadium specific elevation data was used where available. If not published, elevation was determined using mapping and geographic databases for the immediate stadium location. Values were verified across multiple sources and standardized to meters above sea level to ensure a consistent and geographically precise comparison between all sixteen stadiums.

Temperature
Temperature values are based on long term climate normals for each host city, using 30 year datasets published by national meteorological agencies and the U.S. National Oceanic and Atmospheric Administration. Because averages for a single calendar day are rarely available, the value for 1 July is approximated using early July daily means or the July monthly average when necessary.

Humidity
Relative humidity represents the average atmospheric moisture level for early July in each host city and is expressed as a percentage. Values are derived from long term climate normals published by national meteorological agencies and NOAA datasets. When daily averages are unavailable, the July monthly mean is used as the closest proxy for typical conditions around 1 July.

Sharing and Credit

You are welcome to share this tool, reference the data or post screenshots from the visualisation. When doing so, please credit Tales of the Stands and link to this page as the original source.

The tool and its dataset were created as part of the Tales of the Stands project. Everything can be used for editorial or informational purposes with clear attribution. Reproducing the full dataset, republishing the tool or using the material for commercial purposes requires prior permission.

Any questions? Reach out to contact@talesofthestands.com!