| Literature DB >> 26079620 |
David Roiz1, Philippe Boussès1, Frédéric Simard1, Christophe Paupy1, Didier Fontenille2.
Abstract
BACKGROUND: Extreme precipitation events are increasing as a result of ongoing global warming, but controversy surrounds the relationship between flooding and mosquito-borne diseases. A common view among the scientific community and public health officers is that heavy rainfalls have a flushing effect on breeding sites, which negatively affects vector populations, thereby diminishing disease transmission. During 2014 in Montpellier, France, there were at least 11 autochthonous cases of chikungunya caused by the invasive tiger mosquito Aedes albopictus in the vicinity of an imported case. We show that an extreme rainfall event increased and extended the abundance of the disease vector Ae. albopictus, hence the period of autochthonous transmission of chikungunya. METHODOLOGY/PRINCIPALEntities:
Mesh:
Year: 2015 PMID: 26079620 PMCID: PMC4469319 DOI: 10.1371/journal.pntd.0003854
Source DB: PubMed Journal: PLoS Negl Trop Dis ISSN: 1935-2727
Fig 1Mean number of Ae. albopictus eggs per trap per week (black line), Ae. albopictus females per trap per day (grey area) in 24 BGs and 24 ovitraps positioned in 8 locations in Montpellier in 2014.
Autochthonous chikungunya transmission period (green line); weekly bounded accumulated Growing Degree Days (red line); weekly rainfall (black bars).
Results of the model selection of the Generalized Linear Model with negative binomial distribution showing the effect of climatic variables on Ae. albopictus abundances before the inundation in 2014.
| Variable | AICc | delta | weight |
|---|---|---|---|
| Bounded accumulated GDD | 86.20 | 0.00 | 0.99 |
| Accumulated GDD | 95.37 | 9.17 | 0.01 |
| Accumulated temperatures one month before | 99.12 | 12.92 | 0.00 |
| Maximum weekly temperatures | 103.41 | 17.21 | 0.00 |
| Accumulated temperatures two weeks before | 103.66 | 17.46 | 0.00 |
| Accumulated rainfall two weeks before | 104.30 | 18.10 | 0.00 |
| Growing degree days (GDD) | 105.04 | 18.83 | 0.00 |
| Mean weekly temperature | 105.04 | 18.83 | 0.00 |
| Weekly rainfall | 105.65 | 19.45 | 0.00 |
| Weekly insolation time | 105.95 | 19.74 | 0.00 |
| Accumulated rainfall one week before | 106.12 | 19.92 | 0.00 |
| Accumulated temperature one week before | 106.33 | 20.13 | 0.00 |
| Weekly minimal temperatures | 106.49 | 20.28 | 0.00 |
| Accumulated rainfall four weeks before | 107.07 | 20.86 | 0.00 |
The best model explains 69.3% of the variance.
Fig 2Results from the Generalized Linear Model with negative binomial distribution showing the impact of climatic variables on Ae. albopictus abundances before (left panel) and after (right panel) the extreme precipitation event in 2014.
Before the inundations, weekly bounded accumulated Growing Degree Days were related to vector abundance. After the inundations, accumulated rainfall is more important than temperature (see also Table 1).
Results of the model selection of the Generalized Linear Model with negative binomial distribution showing the effect of climatic variables on Ae. albopictus abundances after the inundation in 2014.
| Variable | AICc | delta | weight |
|---|---|---|---|
| Accumulated rainfall four weeks before | 46.54 | 0.00 | 0.60 |
| Maximum weekly temperatures | 48.35 | 1.81 | 0.24 |
| Accumulated temperatures two weeks before | 50.11 | 3.57 | 0.10 |
| Accumulated temperature one week before | 53.34 | 6.81 | 0.02 |
| Mean weekly temperature | 54.01 | 7.47 | 0.01 |
| Growing degree days (GDD) | 55.08 | 8.54 | 0.01 |
| Accumulated GDD | 55.67 | 9.14 | 0.01 |
| Accumulated temperatures one month before | 56.03 | 9.50 | 0.01 |
| Weekly minimal temperatures | 58.19 | 11.66 | 0.00 |
| Bounded accumulated GDD | 58.68 | 12.15 | 0.00 |
| Weekly insolation time | 61.78 | 15.25 | 0.00 |
| Accumulated rainfall two weeks before | 62.45 | 15.92 | 0.00 |
| Accumulated rainfall one week before | 64.40 | 17.86 | 0.00 |
| Weekly rainfall | 64.88 | 18.34 | 0.00 |
The best model explains 92.3% of the variance.