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. 2019 Dec 20;9:19503. doi: 10.1038/s41598-019-55847-8

Table 4.

Differences in ΔT (K) during ENSO events of El Niño (EN) and La Niña (LN) in daytime and nighttime at Tokyo, Phoenix, Bandung, and Quito sites based on biophysical drivers of surface albedo change (E1), convection reduction (E2), evaporation reduction (E3), heat storage change (E4), and anthropogenic release (E5); total biophysical intrinsic drivers (ΔTBI) from E1 to E5; and CLM (ΔTCLM).

ΔTEL-LN (Daytime) ΔTEL-LN (Nighttime)
Tokyo Phoenix Bandung Quito Tokyo Phoenix Bandung Quito
Surface albedo change (E1) 0.01 0.01 0.00 0.00 0.00 0.00 0.00 0.00
Convection reduction (E2) −0.01 −0.01 0.05 −0.22 0.19 −0.09 −0.01 0.00
Evaporation reduction (E3) 0.23 −0.06 0.03 0.06 0.01 0.09 0.01 0.00
Heat storage change (E4) −0.04 −0.02 0.00 0.10 0.02 −0.13 0.08 −0.11
Anthropogenic heat release (E5) −0.02 0.00 0.00 0.00 −0.08 −0.03 0.00 0.00
Total biophysical drivers (ΔTBI) 0.16 −0.08 0.08 −0.05 0.15 −0.16 0.08 −0.11
CLM (ΔTCLM) 0.11 −0.06 0.10 −0.06 0.07 −0.33 0.14 −0.09