| Literature DB >> 32948946 |
Taiwo Temitope Lasisi1, Kayode Kolawole Eluwole2,3.
Abstract
Several conspiracy theories and hypotheses have been postulated by some individuals from various strata of governance globally concerning the outbreak and spread of the novel coronavirus in the last quarter of 2019. A pertinent hypothesis is the correlation of meteorological elements to the spread of the pandemic. To verify this claim and also confirm the initial findings of Tosepu et al.'s (2020), this study investigated the Spearman rank-order correlation of the number of confirmed COVID-19 cases in the Russian Federation with temperature-maximum, minimum, and average as well as precipitation. Our findings indicated a stronger correlation between average temperature (rs = 0.75***) and also recorded significant correlations for the other variants of temperature. Hence, the hypothesis of weather-induced COVID-19 spread is substantiated.Entities:
Keywords: COVID-19; Meteorology; Precipitation; Russia; Temperature
Mesh:
Year: 2020 PMID: 32948946 PMCID: PMC7500989 DOI: 10.1007/s11356-020-10808-x
Source DB: PubMed Journal: Environ Sci Pollut Res Int ISSN: 0944-1344 Impact factor: 4.223
Fig. 1Visual representation of variables for Russia from March to May, 2020
Data notation and source
| Variable name | Notation | Source |
|---|---|---|
| Number of coronavirus cases | COVID-19 | Statista ( |
| Maximum temperature (°C) | T-MAX | National Oceanic and Atmospheric Administration ( |
| Minimum temperature (°C) | T-MIN | National Oceanic and Atmospheric Administration ( |
| Average temperature (°C) | T-AVG | National Oceanic and Atmospheric Administration ( |
| Precipitation (mm) | PREP | National Oceanic and Atmospheric Administration ( |
All variables are daily data
Descriptive statistics
| Variables | COVID-19 | T-MAX | T-MIN | T-AVG | PREP |
|---|---|---|---|---|---|
| Mean | 5489.826 | 55.52174 | 27.65217 | 41.42029 | 0.070145 |
| Median | 5849.000 | 57.00000 | 27.00000 | 39.00000 | 0.000000 |
| Maximum | 11656.00 | 81.00000 | 48.00000 | 61.00000 | 0.790000 |
| Minimum | 53.00000 | 33.00000 | 0.000000 | 27.00000 | 0.000000 |
| Std. dev. | 4037.380 | 11.75561 | 10.33388 | 8.384870 | 0.151633 |
| Skewness | − 0.057154 | 0.157673 | − 0.449072 | 0.440757 | 2.821032 |
| Kurtosis | 1.448966 | 2.250585 | 3.494309 | 2.375944 | 11.36901 |
| Jarqua-Bera | 6.953968 | 1.900564 | 3.021634 | 3.353722 | 292.8853 |
| Probability | 0.030900 | 0.386632 | 0.220730 | 0.186960 | 0.000000 |
| Sum | 378,798.0 | 3831.000 | 1908.000 | 2858.000 | 4.840000 |
| Sum sq. dev. | 1.11E+09 | 9397.217 | 7261.652 | 4780.812 | 1.563499 |
| Observations | 69 | 69 | 69 | 69 | 69 |
Spearman rank-order correlation of weather variables
| Weather variables | Spearman correlation coefficient | ||
|---|---|---|---|
| T-MAX | 0.569*** | 5.659 | .000 |
| T-MIN | 0.720*** | 8.480 | .000 |
| T-AVG | 0.748*** | 9.215 | .000 |
| PREP | 0.131 | 1.082 | .283 |
Johansen cointegration result
| Hypothesized no. of CE(s) | Eigenvalue | Trace statistic | 0.05 | Prob.** |
|---|---|---|---|---|
| None* | 0.369554 | 86.55792 | 69.81889 | 0.0013 |
| At most 1* | 0.353854 | 56.11031 | 47.85613 | 0.0069 |
| At most 2 | 0.244343 | 27.28610 | 29.79707 | 0.0948 |
| At most 3 | 0.104108 | 8.795007 | 15.49471 | 0.3847 |
| At most 4 | 0.023053 | 1.539295 | 3.841465 | 0.2147 |
Trace test indicates 2 cointegrating eqn(s) at the 0.05 level
*Denotes rejection of the hypothesis at the 0.05 level
**MacKinnon-Haug-Michelis (1999) p values