| description abstract | A cluster algorithm was implemented to analyze the backward trajectories arriving in the Barcelona area (BCN), located at the eastern coast of the Iberian Peninsula. Five years of 4-day kinematic back trajectories, computed with version 4 of the Hybrid Single-Particle Lagrangian Integrated Trajectory model (HYSPLIT), were clustered and classified in groups of similar length and curvature. To describe better the tropospheric circulations at BCN, backward trajectories arriving at 5500, 3000, and 1500 m above sea level were analyzed. The main transport patterns are identified at 5500 m: westerly flows (49% of the total situations), northwesterly flows (17%), southwesterly flows (20%), and regional recirculations over Europe and the Mediterranean Sea (15%). An annual distribution of the transport patterns is described. During the summertime, moderate westerlies (19%) and southwesterlies (13%) in the middle troposphere, slow westerlies (11%) and southwesterlies (10%) at 3000 m, and regional recirculations (29%) at 1500 m characterize the BCN long-range transport. This general pattern varies during wintertime, with more westerlies at 5500 m and an increase of northern and northwestern situations at 1500 m. A large number of situations with decoupling between the lower and middle troposphere are observed when combining 5500- and 1500-m cluster results. Interannual variability is discussed, and the influence of the North Atlantic Oscillation phase is captured by winter average regime patterns. | |
