Fig. 2: Different diabatic cooling and energy budgets associated with variations in TP SCE increment and TP SCE.
From: A dynamic link between spring Arctic sea ice and the Tibetan Plateau snow increment indicator
Anomalies of OND a SCE increment (unit: %) and c 2 m air temperature increment (unit: 10−1 °C) obtained by linear regression onto the SCEII during 1979–2021. b, d same as in a, c but for the SCE and 2 m air temperature regressed onto the SCEI. e The red and blue bars are same as in b and a, respectively, but for the TP area-weighted mean of the 2 m air temperature (unit: 10−1 °C), USWR, ULWR, SH and LH anomalies (red bars; unit: W m−2), and its increment anomalies (blue bars). f Relative changes in regression coefficients in the increment field compared to that in the original field (unit: %). The stippling denotes the regions where the regression coefficients are statistically significant at the 5% level.
