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Global Heat Wave Hazard Considering Humidity Effects during the 21st Century

Bibliographic Data

ID15467338
AuthorsXi Chen (0000-0002-2058-0351, Beijing Normal University), Ning Li (0000-0003-4098-1838, Beijing Normal University, corresponding author), Jiawei Liu (0000-0002-8389-0197, Nanjing University of Information Science and Technology), Zhengtao Zhang (0000-0002-3340-0348, Chinese Academy of Sciences), Yuan Liu (0000-0003-2668-0350, Beijing Normal University)
Year2019
Volume16
Issue9
Pages1513-1513
Publication date2019-04-29
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueInternational Journal of Environmental Research and Public Health (JOURNAL)
Journal identifiersISSN: 1661-7827 • E-ISSN: 1660-4601
PublisherMultidisciplinary Digital Publishing Institute (PUBLISHER • CH)
DOI10.3390/ijerph16091513
PMID31035681
OpenAlexW2943615806
LanguageEN
Citations received4
References cited36

Humidity is a significant factor contributing to heat stress, but without enough consideration in studies of quantifying heat hazard or heat risk assessment. Here, the simplified wet-bulb globe temperature (WBGT) considering joint effects of temperature and humidity was utilized as a heat index and the number of annual total heat wave days (HWDs) was employed to quantify heat hazard. In order to evaluate the humidity effects on heat waves, we quantified the difference in the number of HWDs over global land based on air temperature and WBGT. Spatial and temporal changes in surface air temperature, relative humidity, WBGT, and the difference in HWDs were analyzed using multi-model simulations for the reference period (1986-2005) and different greenhouse gas emission scenarios. Our analysis suggests that annual mean WBGT has been increasing since 1986, which is consistent with the rising trend in surface air temperature despite a slight decrease in relative humidity. Additionally, changes in annual mean WBGT are smaller and more spatially uniform than those in annual mean air temperature as a cancelation effect between temperature and water vapor. Results show that there is an underestimation of around 40-140 days in the number of HWDs per year in most regions within 15° latitude of the equator (the humid and warm tropics) during 2076-2095 without considering humidity effects. However, the estimation of HWDs has limited distinction between using WBGT and temperature alone in arid or cold regions

Apparent temperature · Atmospheric sciences · Climate change · Climatology · Geography · Heat index · Humidity · Latitude · Mean radiant temperature · Meteorology · Relative humidity · Water vapor · Wet-bulb globe temperature · Wet-bulb temperature · Atmospheric and Environmental Gas Dynamics · Climate Change and Health Impacts · Climate variability and models · Environmental Science · Geology

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Unique citing works4
Citations per year0,67
Citation span2020 - 2024 (5)
Citation velocityrecent
Highly citedNo
Citation typesNeutral: 4

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