- Influence of the Tropical Diabatic Heating on the South Pacific Subtropical Anticyclone: Abdullah al Fahad, Natalie J. Burls, Erik T. Swenson, David M. Straus. (In preparation)
- How will Southern Hemisphere Subtropical Anticyclones and Hadley Cell Edge Respond to Climate Change? – Evaluating CMIP5 Model Projections: Abdullah al Fahad, Natalie J. Burls. (In preparation)
- The Cape Town "Day Zero" drought and Hadley Expansion (2019): Natalie J. Burls, Ross C. Blamey, Benjamin Cash, Erik T. Swenson, Abdullah al Fahad, Mary-Jane Bopape, David Straus, Chris J.C. Reason. (https://doi.org/10.1038/s41612-019-0084-6)
- The Role of Tropical Heating and Internal Variability in the California Response to the 2015/16 ENSO Event (2019): Erik T. Swenson, David M. Straus, Chelsea E. Snide, Abdullah al Fahad. (https://doi.org/10.1175/JAS-D-19-0064.1)
Uneven heating of the Earth’s surface acts as the primary driving force behind large-scale atmospheric circulation between the tropics and high latitudes. Warm air rises in the tropics and descends over the subtropics of the both hemispheres and completes a circulation pattern known as Hadley Circulation (Fig.1). The descending branch of the Hadley circulation creates a high-pressure system in the subtropical regions of the both hemispheres. Radiative cooling is the primary mechanism that allows subtropical air to descend. These high-pressure systems produce an anticyclonic atmospheric circulation over the surface of subtropical oceans in both hemispheres known as subtropical anticyclones (SA) (Fig.2).
These SAs are an important element of the coupled ocean-atmosphere system within the subtropics dictating oceanic conditions. Although SAs are associated with the descending branches of the Hadley cells, the various mechanisms that control their respective strengths, seasonality, internal variability and response to climate change are still debated within the scientific literature. For example, seasonal cycles in the area, intensity, and position of the SAs in both hemispheres show distinct patterns. If Hadley cell decent were the only mechanism controlling the strength of the SAs one would expect each SA to reach their maximum strength in local winter when the Hadley cell is at its strongest within the respective hemisphere. While this is true for the Southern Hemisphere with SAs strength generally peaking during June-July-August (JJA) within the Southern Hemisphere (SH), this does not occur in the Northern Hemisphere (NH). SAs in the NH also peak in JJA despite that fact that the NH branch of the Hadley cell is at its seasonal minimum (Hoskins 1996). This aspect raises the central question that I deal with in my research: what drives the strength and structure of the SAs?
What controls Subtropical Anticyclones area and strength
WRF model cumulus physics parameterization
ICRC-CORDEX 2016, Stockholm University, Sweden
ENSO impact on 2015/16 Dry California winter
Recent (2015-2017) Cape Town drought