Fig. 5: Irrigation-induced changes in thermodynamic variables in the late afternoon (1500–1800 LT). | npj Climate and Atmospheric Science

Fig. 5: Irrigation-induced changes in thermodynamic variables in the late afternoon (1500–1800 LT).

From: Neglecting irrigation contributes to the simulated summertime warm-and-dry bias in the central United States

Fig. 5

a Difference between irrigation-induced change in LCL and changes in PBL height. Positive values indicate a higher probability of LCL crossing and more low-level clouds, b irrigation-induced change in CAPE, c irrigation-induced change in CIN. Regions with statistically significant changes at the 10% level are indicated with striping.

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