On the Recent Amplification of Dust Over the Arabian Peninsula During 2002–2012

Using available satellite observations and Modern‐Era Retrospective analysis for Research and Applications Version‐2 data sets for the period 1980–2016, this study reveals a summertime dust amplification over the Arabian Peninsula (AP) during about past two decades. Our results demonstrate a significant positive trend in summertime dust loading over the AP since the year 2002, with a maximum increase of 21% over the southern Red Sea. The increased summertime dust over the southern AP is attributed to the intensification of the remote dust transport from the Sahara Desert through Sudan by a strengthened Tokar Gap westerly jet and a general increased gustiness in the AP. Furthermore, increased both air and soil temperature and reduction in the soil moisture along with increased sensible heat flux led to increased local dryness in the AP and played a significant role in enhancing wind‐induced localized dust emissions therein. The associated changes in the AP include an enhancement of net radiative fluxes, particularly the long wave radiative flux. Plain Language Summary Our results show a significant positive trend in summertime dust loading over the Arabian Peninsula in the recent decade. This increasing summertime dust over the southern Arabian Peninsula is attributed to intensification of westerly winds. Air and soil temperatures play a pivotal role in enhancing wind induced localized dust through a positive feedback. Enhanced dust may also modulate the regional surface net radiative fluxes. Key Points We find a significant positive trend in summertime dust loading over the Arabian Peninsula (AP) in recent decades The increased summertime dust, particularly over the southern AP, is attributed to intensification of westerly winds Air and soil temperatures play a pivotal role in enhancing the wind‐induced localized dust through a positive feedback