TY - GEN A1 - Fenner, Daniel A1 - Christen, Andreas A1 - Grimmond, Sue A1 - Meier, Fred A1 - Morrison, William A1 - Zeeman, Matthias A1 - Barlow, Janet A1 - Birkmann, Jörn A1 - Blunn, Lewis A1 - Chrysoulakis, Nektarios A1 - Clements, Matthew A1 - Glazer, Russell A1 - Hertwig, Denise A1 - Kotthaus, Simone A1 - König, Kai A1 - Looschelders, Dana A1 - Mitraka, Zina A1 - Poursanidis, Dimitris A1 - Tsirantonakis, Dimitris A1 - Bechtel, Benjamin A1 - Benjamin, Kit A1 - Beyrich, Frank A1 - Briegel, Ferdinand A1 - Feigel, Gregor A1 - Gertsen, Carlotta A1 - Iqbal, Nimra A1 - Kittner, Jonas A1 - Lean, Humphrey A1 - Liu, Yiqing A1 - Luo, Zhiwen A1 - McGrory, Megan A1 - Metzger, Swen A1 - Paskin, Matthew A1 - Ravan, Marvin A1 - Ruhtz, Thomas A1 - Saunders, Bethany A1 - Scherer, Dieter A1 - Smith, Stefan Thor A1 - Stretton, Megan A1 - Trachte, Katja A1 - Van Hove, Melania T1 - urbisphere-Berlin campaign: Investigating multi-scale urban impacts on the atmospheric boundary layer T2 - Bulletin of the American Meteorological Society N2 - For next-generation weather and climate numerical models to resolve cities, both higher spatial resolution and sub-grid parameterizations of urban canopy-atmosphere processes are required. Key is to better understand intra-urban variability and urban-rural differences in atmospheric boundary layer (ABL) dynamics. This includes upwind-downwind effects due to cities’ influences on the atmosphere beyond their boundaries. To address these aspects a network of >25 ground-based remote-sensing sites was designed for the Berlin region (Germany), considering city form, function, and typical weather conditions. This allows investigation of how different urban densities and human activities impact ABL dynamics. As part of the interdisciplinary European Research Council Grant urbisphere, the network was operated from Autumn 2021 to Autumn 2022. Here we provide an overview of the scientific aims, campaign setup, and results from two days, highlighting multi-scale urban impacts on the atmosphere in combination with high-resolution numerical modeling at 100 m grid-spacing. During a spring day, the analyzes show systematic upwind-city-downwind effects in ABL heights, largely driven by urban-rural differences in surface heat fluxes. During a heatwave day, ABL height is remarkably deep, yet spatial differences in ABL heights are less pronounced due to overall dry soil conditions, resulting in similar observed surface heat fluxes. Our modeling results provide further insights into ABL characteristics not resolved by the observation network, highlighting synergies between both approaches. Our data and findings will support modeling to help deliver services to a wider community from citizens to those managing health, energy, transport, land-use and other city infrastructure and operations. Y1 - 2024 U6 - https://doi.org/10.1175/BAMS-D-23-0030.1 SN - 0003-0007 SN - 1520-0477 VL - 105 PB - American Meteorological Society ER -