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The focal area of this study is the Yunnan border counties in China, comprising 25 counties. These counties serve as the spatial units for this research, with a temporal scope covering a period of seven years. Yunnan Province, positioned in China's southwestern frontier, spans longitudes 97°31′ E to 106°11′ E and latitudes 21°8′ N to 29°15′ N. It shares extensive borders totaling 4,060 kilometers with Myanmar, Laos, and Vietnam, presenting a unique geographical and geopolitical landscape.
The climatic conditions in Yunnan are predominantly of the subtropical plateau monsoon type, which is characterized by complex three-dimensional climate patterns. Under the Köppen climate classification, much of the province lies within the subtropical highland (Köppen Cwb) or humid subtropical zone (Cwa), with mild to warm winters, and tempered summers, except in the almost tropical south, where temperatures regularly exceed 30 °C in the warmer half of the year. From south to north, Yunnan's climate zones can be divided into the following: northern tropics (Jinghong, Yuanjiang, Hekou, Mengding, Yuanmou, and Lujiangba, etc.), southern subtropics (Mengzi, Jianshui, Kailuan, Funing, Jindong, Nangjian, Luxi, Huaping, and Dongchuan, etc.), central subtropics (Maidu, Fengqing, Shidian, Yuxi, Yilang, Mile, Guangnan, Qiu Bei, Bingchuan, and Fugong as well as Yanting, Suijiang, and Yongshan, etc.), and northern subtropics (Kunming Dali, Chuxiong, Baoshan, etc.), South Temperate Zone (Lijiang, northern Dali, northern Qujing and Zhaotong, etc.), Middle Temperate Zone (Northeastern Yunnan and Northwestern Yunnan in the area of about 2,500–3,000 m above sea level), and Alpine Mountainous Zone (Deqin, Zhongdian, Weixi, etc.), totaling 7 climate types. The province experiences clearly defined dry and wet seasons, with temperature changes profoundly influenced by altitude[11]. The climatic zones in Yunnan border areas vary significantly: the northwest experiences a cold climate with prolonged winters, while the southeast enjoys a constant spring-like temperate climate. The southwest and southern borders, extending into the tropics, feature low-heat valley climates.
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Data of confirmed dengue fever cases and population data from 2013 to 2019 were extracted from the China Disease Control and Prevention Information System (CDCIS). This dataset covered the border counties and districts of Yunnan Province, with each county designated as a spatial unit and the data organized on an annual basis.
Meteorological data were obtained from the Resource and Environment Science and Data Center (RESDC). The collected data encompassed temperature, precipitation, relative humidity, barometric pressure, hours of sunshine, and wind speed at 2 meters above the ground, all collated on an annual scale to match the dengue fever case data. The variables and their specific details are systematically listed in Table 1.
Variables Explanation $ \widehat{y} $ Indigenous dengue fever incidence (/100,000) X1 Average annual temperature (°C) X2 Average annual precipitation (mm) X3 Average annual relative humidity (%) X4 Average annual wind speed (m/s) X5 Imported case (no. of cases) Table 1. List of variables
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Both Ordinary Least Square (OLS) regression and GTWR were used to investigate the relationship between dengue incidence and climatological factors. Additionally, to address potential multicollinearity issues, the Variance Inflation Factor (VIF) was calculated for each variable.
OLS regression examines the effects of independent factors on a dependent variable across the entire study area. A limitation of OLS is its inability to account for local variations in the influencing factors, which can be critical in geographical studies. GTWR, by contrast, incorporates both spatial and temporal influences, thereby facilitating a more comprehensive analysis of the spatio-temporal heterogeneity of the factors[12].
The GTWR model integrates spatial and temporal weighting functions in its parameter estimation, defined as follows:
$$ {Y}_{it}={\beta }_{0}\left({u}_{i},{v}_{i}{,t}_{i}\right)+{\sum }_{k=1}^{p}{\beta }_{k}\left({u}_{i},{v}_{i}{,t}_{i}\right){X}_{ik}+{\epsilon }_{i} $$ (1) where \((u_i, v_i, t_i)\) represents the geographical location (longitude and latitude) and observation time for county \(i\), \(X_{ik}\) denotes the influencing factors, and \(\epsilon_i\) is the error term at location \(i\)[13].
$$ {d}_{ij}=\sqrt{\lambda \left[\left({u}_{i}-{u}_{j}\right)+\left({v}_{i}-{v}_{j}\right)\right]+{\mu \left({t}_{i}-{t}_{j}\right)}^{2}} $$ (2) $ \lambda $ and $ \mu $ are scale factors used to measure location and time difference. Distance in equation (2) as a basis in weighting data to estimate GTWR model parameters. The closer the distance between the expected points each county, the greater the weight of the data during the estimation. In this study, data weighting is done by using the adaptive Gaussian kernel function[14].
$$ {w}_{ij}=\text{exp} \left(-{\left({d}_{ij}/ h\right)}^{2}\right) $$ (3) Where, $ h $ is the constant bandwidth performed by the Incremental Spatial Autocorrelation (ISA) method. The Adaptive Gaussian kernel function is used in forming a weighted matrix.
$$ W\left({u}_{i},{v}_{i}{,t}_{i}\right)=diag\left(W\left({u}_{1},{v}_{1}{,t}_{1}\right),\cdots,W\left({u}_{n},{v}_{n}{,t}_{n}\right)\right) $$ (4) Each observed data has one weighted matrix $ W\left({u}_{i},{v}_{i}{,t}_{i}\right) $ in estimating the parameters. Using the algebraic matrix approach and the Weighted least square (WLS) method, the parameter estimation can be written
$$ \widehat{\beta }\left({u}_{i},{v}_{i}{,t}_{i}\right)={\left({X}^{T}W\left({u}_{i},{v}_{i}{,t}_{i}\right)X\right)}^{-1}{X}^{T}W\left({u}_{i},{v}_{i}{,t}_{i}\right) $$ (5) The GTWR model's significance is evaluated against a null hypothesis that tests the function \(\beta_k(u_i, v_i)\) for each coordinate \((u_i, v_i)\) of the research location. Rejection of the null hypothesis indicates the suitability of the GTWR model for the data.
The effectiveness and complexity of the OLS and GTWR models are compared using the coefficient of determination (\(R^2\)) and Akaike’s Information Criterion corrected (AICc)[15]. These metrics assess the models’ fitting effectiveness and allow for a comparison of their respective efficacies.
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As shown in Figure 1, from 2013 to 2019, a total of 13,264 dengue cases were reported in the Yunnan border counties, including 11,266 indigenous and 1,998 imported cases. The data exhibited a distinct seasonal pattern, with a surge in cases from July to November, peaking in September and October. Notably, imported cases predominantly occurred in the first half of the year, followed by a later onset of indigenous cases.
Among the twenty-five counties bordering Myanmar, Laos, and Vietnam, a striking 93.34% (12,381 cases) of dengue fever cases were reported in the seventeen counties adjoining Myanmar, predominantly as indigenous cases (84.80%). Mengla and Jiangcheng, primarily bordering Laos, accounted for 5.74% (762 cases) of the cases, mostly indigenous (85.70%). The counties bordering Vietnam reported 0.88% (117 cases) of the total, with a majority being imported cases (97.44%). Jinghong, Ruili, and Gengma were the most affected counties, with 7,652, 3,010, and 801 cases respectively, representing 57.69%, 22.69%, and 6.04% of the total cases. Detailed distribution is provided in Table 2.
County Types of dengue fever case Total Indigenous cases Imported cases Border with Myanmar 10,499 1,882 12,381 Jinghong 7,571 81 7,652 Ruili 2,373 637 3,010 Gengma 502 299 801 Mangshi 18 33 51 Menglian 15 22 37 Longchuan 13 69 82 Yingjiang 7 154 161 Zhenkang 0 311 311 Menghai 0 210 210 Tengchong 0 45 45 Longling 0 11 11 Cangyuan 0 7 7 Lancang 0 2 2 Ximeng 0 1 1 Fugong 0 0 0 Lushui 0 0 0 Gongshan 0 0 0 Border with Laos and Myanmar 650 108 758 Mengla 650 108 758 Border with Laos and Vietnam 3 1 4 Jiangcheng 3 1 4 Border with Vietnam 114 7 121 Hekou 114 3 117 Jinping 0 2 2 Lvchun 0 1 1 Funing 0 1 1 Malipo 0 0 0 Maguan 0 0 0 Total 11,266 1,998 13,264 Table 2. Distribution of dengue cases in different categories
The study observed notable annual variations in dengue fever (DF) cases in Yunnan border areas. Significant outbreaks occurred in 2013, 2015, 2017, and 2019, with 2019 witnessing the highest incidence, recording 5,371 cases. These fluctuations highlight the dynamic nature of DF transmission over the years. The risk factors contributing to these variations are summarized in Table 3. The border areas of Yunnan Province exhibited an average annual mean temperature of 19.18 °C, average annual mean precipitation of 3.85 mm, relative humidity of 77.32%, and wind speed of 1.42 m/s for the years 2013 to 2019. The prevailing hot and humid conditions in the region are conducive to mosquito breeding.
Variables x Min 1st Q M 3rd Q Max Average annual temperature (°C) 19.18 13.08 18.81 19.59 20.04 21.62 Average annual precipitation (mm) 3.85 2.31 3.38 3.83 4.31 5.63 Average annual relative humidity (%) 77.32 66.26 74.52 77.49 79.78 86.27 Average annual wind speed (m/s) 1.42 1.07 1.23 1.37 1.60 2.10 Imported case (no. of cases) 11.42 0 0 0 3 259 Note. x, mean; Min, minimum; 1st Q, first quartile; M, median; 3rd Q, third quartile; Max, maximum. Table 3. Statistical description of potential risk factors of dengue fever
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The regression modeling of data sets using OLS yields a value of P < 0.001, which is this value of P is greater than the significance level of 0.01. The result indicates that the model contains autocorrelation. The OLS regression model can be written as
$$ \widehat{y}= -137.34 + 7.82X_{1} - 12.47X_{2} + 1.57X_{3} - 25.95X_{4} + 0.60X_{5} $$ As detailed in Table 4, the P-values for the regression coefficients were greater than 0.05 for all variables, except for temperature (P = 0.03) and the number of imported cases (P < 0.01). This suggests that both temperature and imported cases significantly impact the incidence of indigenous dengue fever in the Yunnan border area. The analysis revealed positive correlations with the average annual temperature and the number of imported cases. Specifically, a 1 °C increase in average annual temperature is associated with a 7.82/100,000 increase in indigenous dengue fever incidence, and each additional imported case is linked to a 0.60/100,000 increase in incidence. The VIF values for all variables were below 10, indicating no significant issues with covariance among the predictors.
Variables β sx t P VIF Intercept −137.34 118.79 −1.48 0.14 Average annual temperature (°C), X1 7.82 3.51 2.23 0.03* 1.22 Average annual precipitation (mm), X2 −12.47 9.38 −1.33 0.17 1.49 Average annual relative humidity (%), X3 1.57 1.81 0.87 0.39 1.75 Average annual wind speed (m/s), X4 −25.95 23.28 −1.11 0.27 1.28 Imported case (no. of cases), X5 0.60 0.16 3.76 < 0.01* 1.09 AICc: 1990.14 R2: 0.15 RSS: 819367.91 Note. β, standardized regression coefficient; sx, standard error; *Fisher’s exact test; VIF, variance inflation factor; AICc, Akaike’s information criterion corrected; R2, R square; RSS, residual square summary. Table 4. Analysis results of OLS regression model
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The GTWR model identified an optimal bandwidth (h) of 0.48717. In terms of model fit, the GTWR model demonstrated an \(R^2\) value of 0.20, indicating a better fit than the OLS model. Furthermore, the GTWR model yielded a lower Akaike’s Information Criterion corrected (AICc) value of 1987.98, compared to that of the OLS model, suggesting improved model efficiency.
Analysis of the GTWR results revealed that average annual temperature, relative humidity, and the number of imported cases positively influenced the incidence of indigenous dengue fever. Conversely, average annual precipitation and wind speed were negatively correlated with indigenous dengue incidence, as detailed in Table 5. These findings align with the results obtained from the OLS analysis.
Variables x min 1st Q M 3rd Q max Average annual temperature (°C), X1 9.71 3.64 7.11 10.55 12.61 15.21 Average annual precipitation (mm), X2 −14.57 −19.88 −16.96 −15.68 −12.88 −6.05 Average annual relative humidity (%), X3 1.92 0.20 0.84 2.00 3.06 3.60 Average annual wind speed (m/s), X4 −21.22 −29.79 −22.81 −20.27 −19.09 −16.30 Imported case (no. of cases), X5 0.59 0.54 0.57 0.58 0.61 0.68 Note. x, mean; Min, minimum; 1st Q, first quartile; M, median; 3rd Q, third quartile; Max, maximum; GTWR, geographically and Ttemporally weighted regression. Table 5. Fitting coefficients of risk factors included in GTWR model
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The GTWR model’s fitted coefficients reveal insightful temporal dynamics in the influence of various variables on local dengue incidence. These temporal distributions for each variable have been graphically represented in Figure 2. The analysis highlights a distinct time-trend change in the effects of each variable.
While the direction of the variables’ effects on the incidence of indigenous dengue fever remained consistent over time, notable trends were observed in the intensity of their effects. Both temperature and relative humidity exhibited an increasing trend in their intensity of effect over the years. In contrast, precipitation, wind speed, and the influence of imported cases showed a general decreasing trend year over year.
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The GTWR model’s significant advantage lies in its ability to capture the spatial and temporal variability of independent variables' effects on the dependent variable. As shown in Figure 3, the spatial distribution of fitted coefficients in the GTWR model highlighted distinct spatial patterns: the influence of average annual temperature was notably higher in Yunnan southern subtropical border counties, like Jinghong and Mengla, and lower in the northwestern regions. Average annual precipitation had a minimal impact on eastern border counties, while the effect of average annual relative humidity decreased from west to east along the border. The impact of wind speed was observed to be higher at the extremities and lower in the central regions, particularly affecting counties such as Ruili and Menglian. Interestingly, the distribution of the effect of imported cases showed high influence at both ends of the border and a lower impact in the middle. These findings underscore the spatial variability of climatic factors and imported cases in influencing dengue incidence, highlighting the need for region-specific approaches in dengue prevention and control.
Geographically and Temporally Weighted Regression in Assessing Dengue Fever Spread Factors in YunnanBorder Regions
doi: 10.3967/bes2024.056
- Received Date: 2024-02-01
- Accepted Date: 2024-03-19
Abstract:
Citation: | ZHU Xiao Xiang, WANG Song Wang, LI Yan Fei, ZHANG Ye Wu, SU Xue Mei, ZHAO Xiao Tao. Geographically and Temporally Weighted Regression in Assessing Dengue Fever Spread Factors in YunnanBorder Regions[J]. Biomedical and Environmental Sciences, 2024, 37(5): 511-520. doi: 10.3967/bes2024.056 |