Fig. 6: Sensitivity of cascading effect to change in background aridity.
From: Interaction between dry and hot extremes at a global scale using a cascade modeling framework
a Spatial map showing the classification of global evaporation regimes based on aridity index (AI) calculated as a ratio of mean annual precipitation and potential evaporation for the 1980–2018 period, b–d mean of statistically significant (at 95% confidence level) AF (%) binned as a function of AI and time-lags (1–7 days) for the three types of dry-to-hot event cascade, b D1pH99p, c D5pH95p, and d D10pH90p, and e–g same as in (b–d) but for the three types of hot-to-dry event cascade, e H99pD1p, f H95pD5p, and g H90pD10p, selected for the study.
