| Literature DB >> 34654461 |
Mehdi Karamian1, Mohammad Amin Ghatee2,3, Majid Shayesteh4, Walter Robert Taylor5,6, Saeed Mohebi-Nejad7, Ghasem Taheri4, Mohammad Reza Jamavar4.
Abstract
BACKGROUND: Cutaneous leishmaniasis (CL) has been reported in recent years in South Khorasan Province, a desert region of eastern Iran, where the main species is Leishmania tropica. Little is known of the influence of geography and climate on its distribution, and so this study was conducted to determine geo-climatic factors by using geographic information system.Entities:
Keywords: Cutaneous leishmaniasis; Emerging focus; GIS; Geo-climatic determinants
Mesh:
Year: 2021 PMID: 34654461 PMCID: PMC8518236 DOI: 10.1186/s13071-021-05046-0
Source DB: PubMed Journal: Parasit Vectors ISSN: 1756-3305 Impact factor: 3.876
Univariate analysis of the effect of climatic factors on CL in South Khorasan Province
| Variable | OR | 95% CI | |
|---|---|---|---|
| MAWD | 0.043 | 1.004 | 1–1.008 |
| MAFD | 0.568 | 0.997 | 0.986–1.008 |
| MASD | 0.429 | 1.137 | 0.827–1.563 |
| MAT | 0.533 | 1.039 | 0.921–1.172 |
| MinMAT | 0.665 | 1.022 | 0.925–1.130 |
| MaxMAT | 0.372 | 1.065 | 0.928–1.223 |
| MAR | 0.301 | 0.996 | 0.988–1.004 |
| MAH | 0.072 | 0.939 | 0.877–1.006 |
Fig. 1The climatic interpolated raster maps: mean annual humidity (a), mean annual rainfall (b), mean annual high-velocity wind days (c), mean annual minimum temperature (d), mean maximum annual temperature (e), mean annual temperature (f), mean annual frosty days (g), and mean annual snowy days (h). The number of days with high wind velocity showed a weak effect on CL occurrence whilst other climatic factors had no effect on CL in South Khorasan Province
Univariate analysis of the effects of environmental factors on CL in South Khorasan Province
| Variable | OR | 95% CI | |
|---|---|---|---|
| Soil class | |||
| Dune land (constant) | 0.000 | ||
| Entisols/Aridisols | 0.462 | 2.153 | 0.279–16.6290 |
| Aridisols | 0.252 | 3.207 | 0.437–23.555 |
| Salt flats | 0.532 | 2.160 | 0.193–24.190 |
| Rocky land | 0.677 | 1.539 | 0.203–11.676 |
| Rock outcrops/entisols | 0.941 | 0.926 | 0.12–7.141 |
| Playa | 1 | 0.000 | |
| Land cover | |||
| Garden (constant) | 0.000 | ||
| Agriculture | 0.005 | 2.769 | 1.358–5.646 |
| Rangeland | 0.773 | 0.894 | 0.420–1.906 |
| Rock | 0.74 | 1.42 | 0.179–11.256 |
| Urban | 0.000 | 49 | 20.888–114.947 |
| Bare land | 0.912 | 1.068 | 0.333–3.427 |
| DEM | 0.022 | 0.999 | 0.999–1 |
Fig. 2Maps of the environmental factors: digital elevation model (a), land cover (b), and soil types (c). Urban and agricultural land cover showed direct positive effects whilst elevation had a negative effect on CL occurrence. Soil type was not associated with CL in South Khorasan Province
Multivariate analysis of geo-climatic factors associated with CL in South Khorasan Province
| Variable | OR | 95% CI | |
|---|---|---|---|
| Land cover | |||
| Garden (constant) | 0.000 | ||
| Agriculture | 0.005 | 3.048 | 1.411–6.585 |
| Rangeland | 0.781 | 0.897 | 0.415–1.939 |
| Rock | 0.839 | 1.241 | 0.154–10.022 |
| Urban | 0.000 | 52.102 | 20.765–130.727 |
| Bare land | 0.923 | 1.061 | 0.320–3.512 |
| DEM | 0.45 | 1 | 1–1.001 |
| MAWD | 0.041 | 1.004 | 1–1.009 |