| Literature DB >> 22563513 |
Amine Toumi1, Sadok Chlif, Jihene Bettaieb, Nissaf Ben Alaya, Aicha Boukthir, Zaher E Ahmadi, Afif Ben Salah.
Abstract
BACKGROUND: Old world Zoonotic Cutaneous Leishmaniasis (ZCL) is a vector-borne human disease caused by Leishmania major, a unicellular eukaryotic parasite transmitted by pool blood-feeding sand flies mainly to wild rodents, such as Psammomys obesus. The human beings who share the rodent and sand fly habitats can be subverted as both sand fly blood resource. ZCL is endemic in the Middle East, Central Asia, Subsaharan and North Africa. Like other vector-borne diseases, the incidence of ZCL displayed by humans varies with environmental and climate factors. However, so far no study has addressed the temporal dynamics or the impact of climate factors on the ZCL risk. PRINCIPALEntities:
Mesh:
Year: 2012 PMID: 22563513 PMCID: PMC3341328 DOI: 10.1371/journal.pntd.0001633
Source DB: PubMed Journal: PLoS Negl Trop Dis ISSN: 1935-2727
Figure 1Location of study area.
(a) Tunisia Location Within Mediterranean Basin. (b) Location of Sidi Bouzid Governorate Within Tunisia.
Yearly descriptive statistics of ZCL incidence, rainfall humidity and temperature during the study period.
| Year | ZCL incidence (no) | Rainfall (mm) | Humidity (%) | Temperature (°C) | ||||||||||||
| Med | Mean | Min | Max | Med | Mean | Min | Max | Med | Mean | Min | Max | Med | Mean | Min | Max | |
| 1991 | 88.5 | 289.75 | 4 | 1139 | 20.15 | 19.6 | 0 | 43.3 | 63 | 61.33 | 48 | 72 | 14.6 | 17.2 | 9.7 | 27.9 |
| 1992 | 96.5 | 289.67 | 2 | 1608 | 33.8 | 30.74 | 0.2 | 60.1 | 61.5 | 62.42 | 52 | 72 | 15.7 | 16.24 | 8.1 | 25.2 |
| 1993 | 35.5 | 93.25 | 2 | 446 | 18.4 | 17.43 | 0.2 | 49.4 | 62.5 | 61.25 | 47 | 72 | 16.8 | 18.35 | 9.1 | 28.6 |
| 1994 | 18.5 | 32.17 | 2 | 147 | 14.8 | 15.62 | 0 | 43.2 | 60 | 57.58 | 45 | 67 | 18.5 | 19.63 | 11.2 | 30.3 |
| 1995 | 10.5 | 15 | 0 | 50 | 13.95 | 23.03 | 0 | 65.4 | 56.5 | 57.92 | 47 | 73 | 17.5 | 18.7 | 10.3 | 28.3 |
| 1996 | 6.5 | 12.42 | 1 | 39 | 22.1 | 27.65 | 0 | 66.2 | 57.5 | 58.67 | 49 | 67 | 15.9 | 18.42 | 10.6 | 28.8 |
| 1997 | 7 | 32 | 2 | 142 | 14.45 | 26.44 | .6 | 143.5 | 60 | 58.67 | 47 | 70 | 20.6 | 19.87 | 11.6 | 29.1 |
| 1998 | 9.5 | 54.17 | 0 | 296 | 6.7 | 14.81 | 0 | 64.9 | 59.5 | 59 | 44 | 70 | 19.05 | 18.97 | 9.9 | 28.9 |
| 1999 | 40.5 | 227.92 | 0 | 1321 | 18.75 | 27.48 | 0.1 | 145.5 | 61 | 61.08 | 51 | 72 | 20.8 | 20.55 | 10.6 | 31.2 |
| 2000 | 78.5 | 222 | 0 | 643 | 3.5 | 7.33 | 0 | 19.4 | 62 | 59.08 | 46 | 67 | 18.7 | 18.88 | 8.5 | 28.8 |
| 2001 | 51 | 164.25 | 0 | 553 | 7.3 | 16.77 | 0 | 63.6 | 58 | 58.67 | 46 | 70 | 20.75 | 20.17 | 10.8 | 29.7 |
| 2002 | 42.5 | 163.17 | 1 | 593 | 10.05 | 14.58 | 1.4 | 44.4 | 61.5 | 59.83 | 47 | 69 | 16.7 | 17.68 | 9.4 | 28.4 |
| 2003 | 53.5 | 204.92 | 0 | 1099 | 26.1 | 36.67 | 4.9 | 87.9 | 67 | 63.08 | 49 | 71 | 16.9 | 18.45 | 9.7 | 30.9 |
| 2004 | 92.5 | 368.5 | 0 | 1591 | 17.75 | 19.11 | 0 | 53.7 | 60.5 | 60.42 | 49 | 72 | 15.65 | 18.27 | 11.3 | 29.5 |
| 2005 | 5.5 | 71.67 | 0 | 279 | 11.15 | 11.89 | 0 | 30 | 59.5 | 59.83 | 46 | 69 | 18.5 | 18.28 | 9.6 | 28.4 |
| 2006 | 26.5 | 47.08 | 0 | 149 | 12.7 | 21.99 | 0 | 71.4 | 57.5 | 58.83 | 43 | 74 | 17.55 | 18.19 | 8.3 | 28.5 |
| 2007 | 8 | 18.67 | 0 | 63 | 17.1 | 20.97 | 0 | 75.6 | 61 | 58.75 | 44 | 71 | 16.4 | 19.21 | 10.6 | 29.1 |
Abbreviations: Med, Median; Min, Minimum;Max, Maximum.
Figure 2Box plot with monthly ZCL incidence.
Data was aggregated from January 1991 to December 2007. The box represents the 25th and 75th percentiles. The median is represented by a solid horizontal line. The whiskers of the graph show the 1st percentile to the 99th percentile. Values lower than the first and greater than the 99th percentile are represented by a point.
Figure 3Autocorrelation Function (ACF) of monthly ZCL incidence.
Figure 4Monthly ZCL incidence adjusted vs not adjusted for monthly seasonality (1991–2007).
Figure 5Adjusted relationship between ZCL incidence and humidity, temperature and rainfall.
There were no turning points in the relation between temperature/humidity and ZCL incidence. Therefore, we assume these relationships as linear. For rainfall lagged by 12 to 14 months, a turning point equal to 37.34 exists. The range, from each plot, that the climate variables have a positive effect on ZCL incidence is over the zero axis.
Adjusted impact of climate variables on the ZCL incidence estimated by GEE model.
| Variables | Unit | % Change | 95% CI | P Value |
| R1mean14-12
| 1 mm below 37.34 mm | 2.0 | 0.2, 3.8 | 0.02 |
| R2mean14-12
| 1 mm above 37.34 mm | −3.1 | −7.4, 1.7 | 0.19 |
| Humiditylag2
| 1% | 5.0 | 1.2, 10.3 | 0.01 |
| Temperaturelag2
| 1°C | 8.2 | −5.3, 36.9 | 0.17 |
*: CI, confidence interval.
R1 refers to the mean rainfall below 37.34 mm; R2 is the rainfall above the 37.34 mm.
The lag 2 in humidity and temperature refers to the effect of the months July and August of these climate variables on the ZCL cases that emerged in September and October respectively; ZCL incidence during the remaining months was influenced by the temperature and humidity of the month of September.