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Effects of Diurnal Temperature Range on Child Bacillary Dysentery

Paper Reviewed
Wen, L., Zhao, K., Cheng, J., Wang, X., Yang, H., Li, K. Xu, Z. and Su, H. 2016. The association between diurnal temperature range and childhood bacillary dysentery. International Journal of Biometeorology 60: 269-276.

Introducing their study, Wen et al. (2016) write that bacillary dysentery or BD is "a bacterial infection of the mucosal surface of the intestines caused by different species of Shigella bacteria." It often results in severe and bloody diarrhea, as well as fever, abdominal cramps and tenesmus with an incubation period of 1 or 2 days, the transmission of which usually occurs "via polluted drinking water and contaminated food or through person-to-person contact."

Noting that "little is known about whether the within-day variation of temperature has any impact on bacillary dysentery," the eight researchers studied "the relationship between diurnal temperature range (DTR) and BD in Hefei, China," focusing on "daily data on BD counts among children aged 0-14 years from 1 January 2006 to 31 December 2012," which they obtained from the Hefei Center for Disease Control and Prevention," while daily data on temperature covering the same period were collected from the Hefei Bureau of Meteorology. And what did they thereby learn?

Wen et al. report that (1) "the DTR effect on childhood bacillary dysentery increased when DTR was over 8°C," that (2) "male children and children aged 0-5 years appeared to be more vulnerable to the DTR effect," and that (3) "the data indicate that large DTR may increase the incidence of childhood BD."

In this regard, we note that in a study of DTR that was conducted for the entirety of China based on data collected from 479 weather stations for the period 1962 to 2011, Shen et al. (2014) found that the country-wide DTR declined at a mean rate of 0.157°C/decade, which phenomenon they attributed to the fact that, in most parts of the world, daily minimum temperatures increased at a faster rate than daily maximum temperatures since the 1950s, citing the similar findings of Karl et al. (1993), Horton (1995), Easterling et al. (1997) and Zhou et al. (2009), while additionally noting that "DTR decreased significantly in China over the past several decades," citing Karl et al. (1991, 1993), Kukla and Karl (1993), Dai et al. (1997, 1999), Liu et al. (2004), Ye et al. (2010), Zhou and Ren (2011), Wang and Dickinson (2013), Xia (2013) and Wang et al. (2014).

In light of this host of DTR findings, it would appear that the global warming of the past century or so has likely helped to significantly reduce the occurrence of childhood BD, not only in Hefei, China, but everywhere that BD typically occurs.

References
Dai, A., DelGenio, A.D. and Fung, I.Y. 1997. Clouds, precipitation and diurnal temperature range. Nature 386: 665-666.

Dai, A., Trenberth, K.E. and Karl, T.R. 1999. Effects of clouds, soil moisture, precipitation, and water vapor on diurnal temperature range. Journal of Climate 12: 2451-2473.

Easterling, D.R., Horton, B., Jones, P.D., Peterson, T.C., Karl, T.R., Parker, D.E., Salinger, M.J., Razuvayev, V., Plummer, N., Jamason, P. and Folland, C.K. 1997. Maximum and minimum temperature trends for the globe. Science 277: 364-367.

Horton, B. 1995. Geographical distribution of changes in maximum and minimum temperatures. Atmospheric Research 37: 101-117.

Karl, T.R., Kukla, G., Razuvayev, V.N., Changery, M.J., Quayle, R.G., Heim Jr., R.R., Easterling, D.R. and Fu, C.B. 1991. Global warming: evidence for asymmetric diurnal temperature change. Geophysical Research Letters 18: 2253-2256.

Karl, T.R., Jones, P.D., Knight, R.W., Kukla, G., Plummer, N., Razuvayev, V., Gallo, K.P., Lindseay, J., Charlson, P.J. and Peterson, T.D. 1993. Asymmetric trends of daily maximum and minimum temperature. Bulletin of the American Meteorology Society 74: 1007-1023.

Kukla, G. and Karl, T.R. 1993. Nighttime warming and the greenhouse effect. Environmental Science and Technology 27: 1468-1474.

Liu, B., Xu, M., Henderson, M., Qi, Y. and Li, Y. 2004. Taking China's temperature: Daily range, warming trends, and regional variations, 1955-2000. Journal of Climate 17: 4453-4462.

Shen, X., Liu, B., Li, G., Wu, Z., Jin, Y., Yu, P. and Zhou, D. 2014. Spatiotemporal change of diurnal temperature range and its relationship with sunshine duration and precipitation in China. Journal of Geophysical Research: Atmospheres 119: 13,163-13,179.

Wang, F., Zhang, C., Peng, Y. and Zhou, H. 2014. Diurnal temperature range variation and its causes in a semiarid region from 1957 to 2006. International Journal of Climatology 34: 343-354.

Wang, K. and Dickinson, R.E. 2013. Contribution of solar radiation to decadal temperature variability over land. Proceedings of the National Academy of Sciences USA 110: 14,877-14,882.

Ye, J., Li, F., Sun, G. and Guo, A. 2010. Solar dimming and its impact on estimating solar radiation from diurnal temperature range in China, 1961-2007. Theoretical and Applied Climatology 101: 137-142.

Zhou, L., Dai, A., Dai, Y., Vose, R.S., Zou, C.Z., Tian, Y. and Chen, H. 2009. Spatial dependence of diurnal temperature range trends on precipitation from 1950-2004. Climate Dynamics 32: 429-440.

Zhou, Y.Q. and Ren, G.Y. 2011. Change in extreme temperature events frequency over Mainland China during 1961-2008. Climatic Research 50: 125-139.

Posted 4 June 2016