 This study examined the differences in the rate of climate warming between permafrost and non-permafrost regions in the northern mid-high latitudes. It found that permafrost regions experienced warming at a faster rate than non-permafrost regions, with the difference being most pronounced during the winter months. Additionally, the study found that the rate of warming in non-permafrost regions has been slowing down recently, while the rate of warming in permafrost regions has remained relatively constant. This suggests that carbon emissions from thawing soil may be a factor in the rapid warming observed in permafrost regions, that the potential feedback between ground thawing and climate warming in these regions remains uncertain.