ICUC12-87, updated on 21 May 2025
https://doi.org/10.5194/icuc12-87
12th International Conference on Urban Climate
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Exploring the Cooling Potential of Sea and Estuarine Breezes (SEB) in a Mediterranean city’s summer climate
Cláudia Reis1, Dietmar Oettl2, António Lopes1,3, André Santos Nouri4,5,6, and João Vasconcelos7
Cláudia Reis et al.
  • 1University of Lisbon, Institute of Geography and Spatial Planning, Centre of Geographical Studies, Lisbon, Portugal (claudiareis2@campus.ul.pt)
  • 2Regional Government of Styria, Air Quality Control, Landhausgasse 7, 8010 Graz, Austria
  • 3Associated Laboratory Terra, Portugal
  • 4MARE – Marine and Environmental Sciences Centre / Associate Laboratory ARNET – Aquatic Research Network, Portugal
  • 5Department of Environmental Sciences and Engineering, NOVA School of Science and Technology, NOVA University Lisbon, 2829-516 Caparica, Portugal
  • 6Chair of Environmental Meteorology, Faculty of Environment and Natural Resources, Albert-Ludwigs-University, D-79085, Germany
  • 7Instituto Politécnico de Leiria, Portugal

Sea and estuarine breezes (SEB) play a critical role for cooling air temperatures and enhancing thermal comfort during summer in coastal urban areas. This research investigates the dynamics and impacts of SEB in Lisbon (Portugal) by combining data from a mesoscale meteorological network comprising 80 stations with high-resolution wind field simulations during the thermal summer of 2022 (June 10 to October 8). SEB episodes were identified using criteria based on wind direction shifts: the disruption of prevailing northerly winds in the morning (Nortada), transitions to easterly or southerly directions (rotation between 22,6 and 292,5º), and the resumption of regional flow by late afternoon. Wind fields were modeled using GRAMM-SCI, initialized with ERA5 reanalysis data. Finally, air temperature, absolute humidity and thermal comfort (Universal Thermal Climate Index) anomalies (ΔT/Ha/UTCIurb) were calculated to a reference site (the airport weather station) according to the distance to the riverfront area.  SEB at 10 m height, occurred on 31% of summer days, peaking in July and August, with an average duration of six hours (10:00AM – 4:00PM). Considering only the roughness effect of the city and the terrain, these breezes reduced air temperatures up to 4 km inland, with maximum cooling effects (-1.7°C) observed within 500m of the Tagus estuary. Absolute humidity increased by 4.2 g/m³ near the estuary, and UTCI values dropped by 2.2°C on typical breeze days, reaching 5.1°C during heatwave events, substantially reducing heat stress within 1.5 km of the riverfront. However, some riverside areas still experienced moderate heat stress, highlighting the importance of preserving SEB corridors through climate-sensitive urban planning. This study reinforces the importance of integrating natural ventilation processes into urban design to foster cooler and more liveable cities.

How to cite: Reis, C., Oettl, D., Lopes, A., Santos Nouri, A., and Vasconcelos, J.: Exploring the Cooling Potential of Sea and Estuarine Breezes (SEB) in a Mediterranean city’s summer climate, 12th International Conference on Urban Climate, Rotterdam, The Netherlands, 7–11 Jul 2025, ICUC12-87, https://doi.org/10.5194/icuc12-87, 2025.

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