Very interesting. Thank you Sujit for sharing this article!
1. It first looked like “period prevalence" to me, but when I read the paper, it also seemed like incidence risk. While I wasn’t able to understand most of the methods, I read the methods section of the actual PNAS paper the article was referring to, because it was confusing to me how they derived that specific result only given that number in the newspaper. (The actual study can be found at
https://www.pnas.org/content/118/41/e2024792118 )
So, my guess is
-Denominator: The world population in mid-2016 (See their UN reference data; File 18 at
https://population.un.org/wup/Download/ )
-Numerator: 1.7 billion people. But I’m not sure how they got this number even after reading their methods section. I assume that this reflects the total number of urban population exposed to deadly city heat during the year 2016.
* The only sentence I could assume as above was this sentence in the abstract: Exposure trajectories increased for 46% of urban settlements, which together in 2016 comprised 23% of the planet’s population (1.7 billion people).
* Two criteria on extreme heat events: 1-d or longer periods in which WBGTmax > 30 °C and 2-d or longer periods in which the maximum HImax > 40.6 °C.
2. A) Compare to 1983, those who live in Bangladesh’s capital in 2016 have experienced increased exposure to extreme heat. This was measured as the product of how many people experienced extreme heat and how many days they suffered from heat; basically, it is “person” x “days”, which was 575 million person-days in this study.
B) This gives us more information since it contains not only the number of people involved but also how many days they were affected. Furthermore, we could glimpse a hint on actual methods the researchers were using in this study.
* Their methods described in the paper:
We quantify urban exposure to extreme heat in person-days/year−1 for each GHS-UCDB urban settlement from 1983 to 2016. Person-days/year−1 is a widely used metric to compare and contrast exposure to extreme heat across geographies and time periods.
- For a given year (Yi) and for a given urban settlement (j), we multiply the urban settlement’s population (Nij) by the number of days for year i that a threshold is exceeded (e.g., WBGTmax > 30 °C, Daysij).
- After summing exposure in person-days/year−1 for each year at municipality, national, regional, and global scales, we evaluate annual rate of increase in exposure from 1983 to 2016 (person-days/year−1) across spatial scales by fitting simple ordinary least squares linear regression models (OLS).
* By the way, Fig S4 in the supplement showed the change in global urban extreme-heat exposure (in Person-days/year) according to time (year). They show how “person-year” value of heat exposure changed over time, providing evidence for climate change. (The Supplement:
https://www.pnas.org/content/pnas/suppl/2021/09/28/2024792118.DCSupplemental/pnas.2024792118.sapp.pdf)
3. RR > 1 is expected. Numerator: Risk of death in the extreme heat-exposed group, Denominator: Risk of death in the unexposed group.
4. AR=(Risk of deaths in extreme heat-exposed group - Risk of deaths in non-exposed group)/Risk of deaths in extreme heat-exposed group.
I think a simple approach would be choosing a specific date (or multiple dates) in early-July (e.g. a day with relatively average temperature, at least a week before extreme heat comes) and measure prevalenceo of death on that day due to heat; then, choose a date (or multiple dates) with extreme heat (e.g. >30°C) and measure prevalence of death due to heat on that day(s). The difference between the two divided by the latter would be attributable to extreme heat. I think it can be done more easily by doing a retrospective research since the mortality and temperature points are already available.