Air temperatures

Changes in Climate icon

Air temperatures

Air temperatures have increased over the past century, driven mainly by changes in nighttime temperatures.


One of the most definitive indicators of climate change is air temperature. The rise in global air temperatures is linked to increased concentrations of carbon dioxide and other greenhouse gases from human activities in the Earth’s atmosphere. Warming air temperatures impact the weather, the water cycle, human health and well-being, and ecosystems. For more information, download the Air Temperatures chapter.

What does this indicator show?

Statewide annual average air temperatures

This line graph shows the annual average air temperatures (°F) from 1895 to 2021 in the grey dotted line and the 11-year running average in the solid red line.

  • Infographic with text explaining that nighttime temperatures warmed three times faster than daytime temperatures. Statewide annual mean temperatures have increased by about 2.5 degrees Fahrenheit (°F) since 1895. Warming has accelerated, and seven of the past eight years have been the warmest on record. 

  • Some of the warmest years coincided with some of the driest years, leading to exacerbated drought conditions. Droughts of the 21st century have been hotter, longer lasting, and more widespread than before. 

Why is this indicator important?

  • A warming climate has far-reaching effects on our health, well-being, ecosystems, and natural resources.   

  • Extreme heat, poor air quality, droughts, and other severe impacts of warming temperatures disproportionately fall on underserved communities. These communities are least able to prepare for and recover from such impacts. 

What factors influence this indicator?

  • Carbon dioxide and other greenhouse gases have driven unprecedented warming worldwide. 

  • Temperatures are also influenced by the natural landscape, elevation, proximity to the ocean, and atmospheric and oceanic circulations. 

  • Changes in land use and land surface exert local effects on temperature. For example, heat-absorbing concrete and asphalt in buildings and roads have a warming effect, and irrigation has a cooling effect. 


All regions of California have warmed over the last century, although at varying rates. Southern California is warming about twice as fast as Northern California.    

A road in Southern California on a sunny day.

Credit: iStock/DutcherAerials

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