|
Variables
|
Min
|
Max
|
Mean
|
Median
|
Std
|
|---|---|---|---|---|---|
|
Temperature
|
9.40
|
43.90
|
26.97
|
26.10
|
7.00
|
|
Dew temperature
|
1.43
|
31.74
|
12.59
|
11.61
|
7.33
|
|
Wet temperature
|
3.32
|
33.52
|
20.01
|
19.09
|
4.92
|
|
Relative humidity
|
10.46
|
98.83
|
68.65
|
69.23
|
16.73
|
|
HDI
|
0.64
|
0.82
|
0.76
|
0.77
|
0.03
|
| Analysis of hot and cold spot provinces | |||||
|
Models
|
Total SIR of PTB
|
Area-adjusted for independent variables
|
||||||
|---|---|---|---|---|---|---|---|---|
|
AIC
|
MSE
|
R2
|
OOB R2
|
AIC
|
MSE
|
R2
|
OOB R2
|
|
|
RF
|
-2031.2
|
0.01
|
0.97
|
0.87
|
-2032.9
|
0.01
|
0.97
|
0.87
|
|
GWRF
|
-2051.7
|
0.01
|
0.97
|
0.90
|
-2152.4
|
0.009
|
0.98
|
0.89
|
| Temporal Variation in PTB SIR | ||||||||
| Figure [3], for the period from 2009 to 2023, the highest mean SIR was in the years 2009 and 2013, and the lowest SIR was in 2020. Province-level SIR of PTB remains relatively stable through these years, with notable decrease in the year 2020 concentrated. A total decrease of 0.04 units was observed in both models. | ||||||||
|
Name of provinces
|
2024
|
2025
|
2026
|
2027
|
2028
|
|---|---|---|---|---|---|
|
Sistan va Balochestan
|
3.34
|
3.27
|
3.20
|
3.14
|
3.08
|
|
Golestan
|
2.80
|
2.74
|
2.69
|
2.64
|
2.58
|
|
Khuzestan
|
1.72
|
1.69
|
1.65
|
1.62
|
1.59
|
|
Guilan
|
1.66
|
1.63
|
1.60
|
1.56
|
1.53
|
|
Khorasan Razavi
|
1.61
|
1.58
|
1.55
|
1.52
|
1.49
|
|
Mazandaran
|
1.26
|
1.23
|
1.21
|
1.18
|
1.16
|
|
Kermanshah
|
1.13
|
1.11
|
1.08
|
1.06
|
1.04
|
|
Khorasan North
|
1.11
|
1.09
|
1.07
|
1.05
|
1.03
|
|
Hormozgan
|
1.08
|
1.06
|
1.04
|
1.02
|
1.00
|
|
Kurdistan
|
1.08
|
1.06
|
1.04
|
1.02
|
1.00
|
|
Khorasan South
|
0.87
|
0.85
|
0.84
|
0.82
|
0.80
|
|
Lorestan
|
0.84
|
0.82
|
0.81
|
0.79
|
0.77
|
|
Qom
|
0.83
|
0.82
|
0.80
|
0.79
|
0.77
|
|
Yazd
|
0.83
|
0.81
|
0.79
|
0.78
|
0.76
|
|
Markazi
|
0.79
|
0.77
|
0.76
|
0.74
|
0.73
|
|
Kerman
|
0.78
|
0.76
|
0.74
|
0.73
|
0.71
|
|
Ardebil
|
0.76
|
0.75
|
0.74
|
0.72
|
0.71
|
|
Alborz
|
0.75
|
0.74
|
0.72
|
0.71
|
0.70
|
|
Tehran
|
0.75
|
0.73
|
0.72
|
0.70
|
0.69
|
|
Semnan
|
0.72
|
0.70
|
0.69
|
0.68
|
0.66
|
|
Ilam
|
0.67
|
0.66
|
0.60
|
0.63
|
0.62
|
|
Bushehr
|
0.56
|
0.55
|
0.54
|
0.53
|
0.51
|
|
Hamadan
|
0.52
|
0.51
|
0.50
|
0.49
|
0.48
|
|
Zanjan
|
0.52
|
0.51
|
0.50
|
0.49
|
0.48
|
|
West Azerbaijan
|
0.51
|
0.49
|
0.48
|
0.48
|
0.47
|
|
East Azerbaijan
|
0.46
|
0.45
|
0.44
|
0.43
|
0.42
|
|
Qazvin
|
0.43
|
0.42
|
0.41
|
0.41
|
0.40
|
|
Isfahan
|
0.38
|
0.37
|
0.36
|
0.35
|
0.35
|
|
Kohgiluyeh and Boyerahmad
|
0.35
|
0.35
|
0.34
|
0.33
|
0.32
|
|
Shiraz
|
0.28
|
0.27
|
0.26
|
0.26
|
0.25
|
|
Chaharmahal Bakhtiari
|
0.19
|
0.19
|
0.19
|
0.18
|
0.18
|
| Spatial Heterogeneity of PTB Determinants | |||||
| For the PTB incidence factors, Fig. 4(a) shows that importance of temperature on PTB incidence varies significantly in different provinces The high SIR values of ‘‘temperature’’ are mainly concentrated in the southern and northern regions, indicating the temperature has higher impacts on PTB incidence in these areas than other areas. Figure 4(b) demonstrate that the importance of HDI is high in some provinces in the southern regions such as Sistan va Balochestan, Hormozgan, Shiraz, Yazd, Kurdistan, Mazandaran, Tehran, Alborz, Markazi, and Kohgiluyeh and Boyerahmad. Figure 4(c–e) demonstrate that the importance of relative humidity, wet temperature and dew temperature is high in some cities in the southern and eastern regions. | |||||