Fig. 4: Separate contributions (K decade−1) of background climate change (BCC), urbanization (URB), and landscape greening (LSG) to urban surface warming trends.
From: Surface warming in global cities is substantially more rapid than in rural background areas
Map of daytime for BCC, URB, and LSG (a–c), map of nighttime for BCC, URB, and LSG (e–g), and probability density distribution of the separate contributions for daytime (d) and nighttime (h).
