Climate science at a glance
- Challenges to human and livestock health are growing due to the increased frequency and intensity of high temperature extremes that cause heat-related illness.
- Heat stress can exacerbate preexisting health conditions and lead to an increase in human mortality.
- As air warms, its capacity to hold water vapor increases, and measurements show that atmospheric humidity is increasing around the globe, consistent with a warming climate.
- The fingerprint of climate change has been found in the increase of wet bulb temperature since 1973, driving heat stress globally.
Relative vs specific humidity
Specific humidity increases as the climate warms. It is an absolute measure of the amount of water in a given amount of air. Just as the absolute amount of water in a given amount of air increases as the climate warms, the amount of water the air can hold increases. Relative humidity looks at how much water is in the air relative to how much could be in the air. This ratio—between how much water is in the air versus how much the air could hold— is expected to remain constant as the climate warms.
U.S. humidity and heat-related illness trends and climate change
- Increasing humidity is contributing to higher nighttime temperatures in the U.S.
- Elevated temperature, combined with increased salinity and humidity, accelerates deterioration in bridges and roads constructed with concrete.
- Absolute humidity is increasing significantly in the Midwest, creating favorable conditions for pests and pathogens and degrading the quality of stored grain.
- In the Midwest, daily minimum temperatures have increased in all seasons due to increasing humidity.
U.S. studies attribute increased humidity and heat stress to climate change
- (Lehner et al. 2018) find that warming in the southwestern U.S. is largely due to greenhouse gas forcing.
- (Diffenbaugh et al. 2017) formally identify the influence of anthropogenic warming in the observed trend of increasing heat extremes over the western U.S.
- (Shiogama et al. 2014) find that anthropogenic warming made a severe heat wave that occurred in the southwestern United States during June and July 2013 more likely.
- (Diffenbaugh and Scherer 2013) show that extreme July temperatures like those observed in 2012 are more than four times as frequent over the north-central and northeastern United States due to anthropogenic climate change.
- (Morak et al. 2011) show that human-caused climate change is at least partly responsible for a strong increase in the number of warm nights in western North America.
Global humidity and heat stress trends and climate change
- The frequency of humid heat so high it comes close to overwhelming the human body’s ability to regulate its temperature has more than doubled in some coastal subtropical regions of the world since 1979.
- IPCC AR5 reported, "It is very likely that global near surface and tropospheric air specific humidity have increased since the 1970s."
- The northern hemisphere has had increasingly warmer and more humid summers, and the global area covered by extreme water vapor is increasing significantly.
Global studies attribute increased humidity and heat stress to climate change
- (Wehner et al. 2018) analyze increases in the frequency and intensity of extremely hot three day periods due to human-caused climate change. They find that the shift in the distribution of surface air temperature since the mid 20th century has been profound and most regions have experienced increases in the frequency an intensity of extremely hot three day periods. Temperatures that were rare prior to the 1980's now occur with regularity.
- (Diffenbaugh et al. 2017) find that anthropogenic global warming had a significant hand in the temperatures seen during the hottest month and on the hottest day on record throughout much of the world from 1931–2016. They find that the global trend in warming contributed to the record for hottest day of the year in at least 82 percent of the records over the 1961-2010 period.
- (Knutson and Ploshay 2016) find that there has been a detectable human-caused increase in mean summertime heat stress since 1973, both globally and in most land regions analyzed.