Fig. 3: Impact of ADO of increasing intensity on thermodynamic parameters.
From: Increasing atmospheric dust transport towards the western Mediterranean over 1948–2020

Median values (and 95% confidence intervals) of anomalies of temperature at 850 hPa (TANOM in °C), in the SW, SE, Central and E regions of the IP (a) and in the BI and the NE, NW and N regions of the IP (b) during ADO of increasing intensity in the period 2001–2020. ADO-L low event, ADO-M moderate event, ADO-H high event, ADO-VH very high event, IP Iberian Peninsula, BI Balearic Islands.