Articles | Volume 26, issue 3
https://doi.org/10.5194/acp-26-2391-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-26-2391-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Observed multiscale dynamical processes responsible for an extreme gust event in Beijing
Xiaoran Guo
State Key Laboratory of Severe Weather Meteorological Science and Technology & Specialized Meteorological Support Technology Research Center, Chinese Academy of Meteorological Sciences, Beijing 100081, China
Key Laboratory of South China Sea Meteorological Disaster Prevention and Mitigation of Hainan Province, Haikou 570203, China
State Key Laboratory of Severe Weather Meteorological Science and Technology & Specialized Meteorological Support Technology Research Center, Chinese Academy of Meteorological Sciences, Beijing 100081, China
Ning Li
State Key Laboratory of Severe Weather Meteorological Science and Technology & Specialized Meteorological Support Technology Research Center, Chinese Academy of Meteorological Sciences, Beijing 100081, China
Zhen Zhang
State Key Laboratory of Severe Weather Meteorological Science and Technology & Specialized Meteorological Support Technology Research Center, Chinese Academy of Meteorological Sciences, Beijing 100081, China
Department of Atmospheric and Oceanic Sciences and Institute of Atmospheric Sciences, Fudan University, Shanghai 200438, China
Tianmeng Chen
State Key Laboratory of Severe Weather Meteorological Science and Technology & Specialized Meteorological Support Technology Research Center, Chinese Academy of Meteorological Sciences, Beijing 100081, China
State Key Laboratory of Atmospheric Environment and Extreme Meteorology, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
Pengzhan Yao
State Key Laboratory of Severe Weather Meteorological Science and Technology & Specialized Meteorological Support Technology Research Center, Chinese Academy of Meteorological Sciences, Beijing 100081, China
Department of Atmospheric and Oceanic Sciences and Institute of Atmospheric Sciences, Fudan University, Shanghai 200438, China
Shuairu Jiang
State Key Laboratory of Severe Weather Meteorological Science and Technology & Specialized Meteorological Support Technology Research Center, Chinese Academy of Meteorological Sciences, Beijing 100081, China
Lei Zhao
Key Laboratory of South China Sea Meteorological Disaster Prevention and Mitigation of Hainan Province, Haikou 570203, China
Fei Hu
State Key Laboratory of Atmospheric Environment and Extreme Meteorology, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
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This study analyzed the nature, mechanisms and drivers for hot-and-polluted episodes (HPEs) in the Pearl River Delta, China. A total of eight HPEs were identified and can be grouped into three clusters of HPEs that were respectively driven (1) by weak subsidence and convection induced by approaching tropical cyclones, (2) by calm conditions with low wind speed in the lower atmosphere and (3) by the combination of both aforementioned conditions.
Tianmeng Chen, Zhanqing Li, Ralph A. Kahn, Chuanfeng Zhao, Daniel Rosenfeld, Jianping Guo, Wenchao Han, and Dandan Chen
Atmos. Chem. Phys., 21, 6199–6220, https://doi.org/10.5194/acp-21-6199-2021, https://doi.org/10.5194/acp-21-6199-2021, 2021
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A convective cloud identification process is developed using geostationary satellite data from Himawari-8.
Convective cloud fraction is generally larger before noon and smaller in the afternoon under polluted conditions, but megacities and complex topography can influence the pattern.
A robust relationship between convective cloud and aerosol loading is found. This pattern varies with terrain height and is modulated by varying thermodynamic, dynamical, and humidity conditions during the day.
Jianping Guo, Boming Liu, Wei Gong, Lijuan Shi, Yong Zhang, Yingying Ma, Jian Zhang, Tianmeng Chen, Kaixu Bai, Ad Stoffelen, Gerrit de Leeuw, and Xiaofeng Xu
Atmos. Chem. Phys., 21, 2945–2958, https://doi.org/10.5194/acp-21-2945-2021, https://doi.org/10.5194/acp-21-2945-2021, 2021
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Vertical wind profiles are crucial to a wide range of atmospheric disciplines. Aeolus is the first satellite mission to directly observe wind profile information on a global scale. However, Aeolus wind products over China have thus far not been evaluated by in situ comparison. This work is expected to let the public and science community better know the Aeolus wind products and to encourage use of these valuable data in future research and applications.
Cited articles
Abulikemu, A., Wang, Y., Gao, R., Wang, Y., and Xu, X.: A numerical study of convection initiation associated with a gust front in Bohai Bay Region, North China, Journal of Geophysical Research: Atmospheres, 124, 13843–13860, https://doi.org/10.1029/2019JD030883, 2019.
Adams-Selin, R. D., van den Heever, S. C., and Johnson, R. H.: Impact of Graupel parameterization schemes on idealized bow echo simulations, Monthly Weather Review, 141, 1241–1262, https://doi.org/10.1175/MWR-D-12-00064.1, 2013.
Adler, B. and Kalthoff, N.: Multi-scale transport processes observed in the boundary layer over a mountainous island, Bound.-Lay. Meteorol., 153, 515–537, https://doi.org/10.1007/s10546-014-9957-8, 2014.
Atkins, N. T. and Laurent, M. St.: Bow echo mesovortices. Part I: Processes that influence their damaging potential, Monthly Weather Review, 137, 1497–1513, https://doi.org/10.1175/2008MWR2649.1, 2009.
Atkins, N. T., Bouchard, C. S., Przybylinski, R. W., Trapp, R. J., and Schmocker, G.: Damaging surface wind mechanisms within the 10 June 2003 Saint Louis bow echo during BAMEX, Monthly Weather Review, 133, 2275–2296, https://doi.org/10.1175/MWR2973.1, 2005).
Azorin-Molina, C., Guijarro, J.-A., Mcvicar, T. R., Vicente-Serrano, S. M., Chen, D., Jerez, S., and Espírito-Santo, F.: Trends of daily peak wind gusts in Spain and Portugal, 1961–2014, Journal of Geophysical Research: Atmospheres, 121, 1059–1078, https://doi.org/10.1002/2015JD024485, 2016.
Barthelmie, R. J.: Evaluating the impact of wind induced roughness change and tidal range on extrapolation of offshore vertical wind speed profiles, Wind Energ., 4: 99-105, https://doi.org/10.1002/we.45, 2001.
Beck, J. and Weiss, C.: An Assessment of Low-Level Baroclinity and Vorticity within a Simulated Supercell, Monthly Weather Review, 141, 649–669, https://doi.org/10.1175/MWR-D-11-00115.1, 2013.
Bélair, F., Dyer-Hawes, Q., and Romanic, D.: The Dynamics of the Urban Boundary Layer Before and During a Severe Thunderstorm Outflow Over Downtown Montreal, Bound.-Lay. Meteorol., 191, 6, https://doi.org/10.1007/s10546-024-00896-4, 2025.
Bellamy, J. C.: Objective calculations of divergence, vertical velocity and vorticity, Bulletin of the American Meteorological Society, 30, 45–49, https://doi.org/10.1175/1520-0477-30.2.45, 1949.
Bentley, M. L. and Mote, T. L.: A Climatology of Derecho-Producing Mesoscale Convective Systems in the Central and Eastern United States, 1986–95. Part I: Temporal and Spatial Distribution, Bulletin of the American Meteorological Society, 79, 2527–2540, https://doi.org/10.1175/1520-0477(1998)079<2527:ACODPM>2.0.CO;2, 1998.
Bentley, M. L. and Sparks, J. M.: A 15 yr climatology of derecho-producing mesoscale convective systems over the central and eastern United States, Climate Res., 24, 129–139, 2003.
Bessho, K., Date, K., Hayashi, M., Ikeda, A., Imai, T., Inoue, H., Kumagai, Y., Miyakawa, T., Murata, H., Ohno, T., Okuyama, A., Oyama, R., Sasaki, Y., Shimazu, Y., Shimoji, K., Sumida, Y., Suzuki, M., Taniguchi, H., Tsuchiyama, H., Uesawa, D., Yokota, H., and Yoshida, R.: An introduction to Himawari-8/9 – Japan's new-generation geostationary meteorological satellites, Journal of the Meteorological Society of Japan Series II, 94, 151–183, https://doi.org/10.2151/jmsj.2016-009, 2016.
Bluestein, H. B.: Fronts and Jet Streaks: A Theoretical Perspective, in: Mesoscale meteorology and forecastingm edited by: Ray, P. S., American Meteorological Society, pp. 173–215, https://doi.org/10.1007/978-1-935704-20-1_9, 1986.
Bony, S. and Stevens, B.: Measuring area-averaged vertical motions with dropsondes, Journal of the Atmospheric Sciences, 76, 767–783, https://doi.org/10.1175/JAS-D-18-0141.1, 2019.
Bosart, L. R. and Sanders, F.: The Johnstown flood of July 1977: A long-lived convective system, Journal of the Atmospheric Sciences, 38, 1616–1642, https://doi.org/10.1175/1520-0469(1981)038<1616:TJFOJA>2.0.CO;2, 1981.
Burghardt, B. J., Evans, C., and Roebber, P. J.: Assessing the predictability of convection initiation in the high plains using an object-based approach, Weather and Forecasting, 29, 403–418, https://doi.org/10.1175/WAF-D-13-00089.1, 2014.
Brandes, E. A. and Ziegler, C. L.: Mesoscale downdraft influences on vertical vorticity in a mature mesoscale convective system, Monthly Weather Review, 121, 1337–1353, https://doi.org/10.1175/1520-0493(1993)121<1337:MDIOVV>2.0.CO;2, 1993.
Browand, F. K. and Winant, C. D.: Laboratory observations of shear-layer instability in a stratified fluid, Bound.-Lay. Meteorol., 5: 67-77, https://doi.org/10.1007/BF02188312, 1973.
Browning, K. A., Marsham, J. H., Nicol, J. C., Perry, F. M., White, B. A., Blyth, A. M., and Mobbs, S. D.: Observations of dual slantwise circulations above a cool undercurrent in a mesoscale convective system, Q. J. R. Meteorol. Soc., 136: 354-373, https://doi.org/10.1002/qj.582, 2010.
Byrne, D. and Zhang, J. A.: Height-dependent transition from 3-D to 2-D turbulence in the hurricane boundary layer, Geophysical Research Letters, 40, 1439–1442, https://doi.org/10.1002/grl.50335, 2013.
Chen, D., Guo, J., Yao, D., Lin, Y., Zhao, C., Min, M., Xu, H., Liu, L., Huang, X., Chen, T., and Zhai, P.: Mesoscale convective systems in the Asian monsoon region from Advanced Himawari Imager: Algorithms and preliminary results, Journal of Geophysical Research: Atmospheres, 124, 2210–2234, https://doi.org/10.1029/2018JD029707, 2019.
Chen, M., Wang, Y., Gao, F., and Xiao, X.: Diurnal variations in convective storm activity over contiguous North China during the warm season based on radar mosaic climatology, Journal of Geophysical Research: Atmospheres, 117, D20115, https://doi.org/10.1029/2012JD018158, 2012.
Chen, M., Wang, Y., Gao, F., and Xiao, X.: Diurnal evolution and distribution of warm – season convective storms in different prevailing wind regimes over contiguous North China, Journal of Geophysical Research: Atmospheres, 119, 2742–2763, 2014.
Chen, T., Guo, J., Guo, X., Zhang, Y., Xu, H., and Zhang, D.-L.: On the multiscale processes leading to an extreme gust wind event in East China: Insights from radar wind profiler mesonet observations, Journal of Geophysical Research: Atmospheres, 129, e2024JD041484, https://doi.org/10.1029/2024JD041484, 2024.
Coniglio, M. C., Corfidi, S. F., and Kain, J. S.: Environment and early evolution of the 8 May 2009 derecho-producing convective system, Monthly Weather Review, 139, 1083–1102, https://doi.org/10.1175/2010MWR3413.1, 2011.
Da, C.: Preliminary assessment of the Advanced Himawari Imager (AHI) measurement onboard Himawari-8 geostationary satellite, Remote Sensing Letters, 6, 637–646, https://doi.org/10.1080/2150704x.2015.1066522, 2015.
Dai, C., Wang, Q., Kalogiros, J. A., Lenschow, D. H., Gao, Z., and Zhou, M.: Determining boundary-layer height from aircraft measurements, Bound.-Lay. Meteorol., 152, 277–302, https://doi.org/10.1007/s10546-014-9929-z, 2014.
Dodson, D. S. and Small Griswold, J. D.: Turbulent and boundary layer characteristics during VOCALS-REx, Atmos. Chem. Phys., 21, 1937–1961, https://doi.org/10.5194/acp-21-1937-2021, 2021.
Emanuel, K. A.: Frontal Circulations in the Presence of Small Moist Symmetric Stability, Journal of the Atmospheric Sciences, 42, 1062–1071, https://doi.org/10.1175/1520-0469(1985)042<1062:FCITPO>2.0.CO;2, 1985.
Evans, C., Weisman, M. L., and Bosart, L. F.: Development of an intense, warm-core mesoscale vortex associated with the 8 May 2009 “super derecho” convective event, Journal of the Atmospheric Sciences, 71, 1218–1240, https://doi.org/10.1175/JAS-D-13-0167.1, 2014.
Fiori, E., Parodi, A., and Siccardi, F.: Uncertainty in prediction of deep moist convective processes: Turbulence parameterizations, microphysics and grid-scale effects, Atmospheric Research, 100, 447–456, https://doi.org/10.1016/j.atmosres.2010.10.003, 2011.
Fovell, R. G.: Upstream influence of numerically simulated squall-line storms, Q. J. R. Meteorol. Soc., 128, 893–912, https://doi.org/10.1256/0035900021643737, 2002.
Fovell, R. G. and Cao, Y.: Wind and gust forecasting in complex terrain, in: 15th WRF Users' Workshop, Boulder, CO, NCAR, 5A.2, http://www2.mmm.ucar.edu/wrf/users/workshops/WS2014/ppts/5A.2.pdf (last access: 10 December 2025), 2014.
French, A. J. and Parker, M. D.: Observations of mergers between squall lines and isolated supercell thunderstorms, Weather and Forecasting, 27, 255–278, https://doi.org/10.1175/WAF-D-11-00058.1, 2012.
French, A. J. and Parker, M. D.: Numerical simulations of bow echo formation following a squall line–supercell merger, Monthly Weather Review, 142, 4791–4822, https://doi.org/10.1175/MWR-D-13-00356.1, 2014.
Fujita, T. T.: Manual of downburst identification for Project NIMROD, Satellite and Mesometeorology Research Paper 156, 111 pp., https://ntrs.nasa.gov/citations/19780022828 (last access: 12 December 2025), 1978.
Goyette, S., Brasseur, O., and Beniston, M.: Application of a new wind gust parameterization: Multiscale case studies performed with the Canadian regional climate model, Journal of Geophysical Research: Atmospheres, 108, 4374, https://doi.org/10.1029/2002JD002646, D13, 2003.
Guo, J., Liu, B., Gong, W., Shi, L., Zhang, Y., Ma, Y., Zhang, J., Chen, T., Bai, K., Stoffelen, A., de Leeuw, G., and Xu, X.: Technical note: First comparison of wind observations from ESA's satellite mission Aeolus and ground-based radar wind profiler network of China, Atmos. Chem. Phys., 21, 2945–2958, https://doi.org/10.5194/acp-21-2945-2021, 2021a.
Guo, J., Zhang, J., Yang, K., Liao, H., Zhang, S., Huang, K., Lv, Y., Shao, J., Yu, T., Tong, B., Li, J., Su, T., Yim, S. H. L., Stoffelen, A., Zhai, P., and Xu, X.: Investigation of near-global daytime boundary layer height using high-resolution radiosondes: first results and comparison with ERA5, MERRA-2, JRA-55, and NCEP-2 reanalyses, Atmos. Chem. Phys., 21, 17079–17097, https://doi.org/10.5194/acp-21-17079-2021, 2021b.
Guo, X., Guo, J., Zhang, D-L., and Yun, Y.: Vertical divergence profiles as detected by two wind profiler mesonets over East China: implications for nowcasting convective storms, Q. J. R. Meteorol. Soc., 149, 1629–1649, https://doi.org/10.1002/qj.4474, 2023.
Guo, X., Guo, J., Chen, T., Li, N., Zhang, F., and Sun, Y.: Revisiting the evolution of downhill thunderstorms over Beijing: a new perspective from a radar wind profiler mesonet, Atmos. Chem. Phys., 24, 8067–8083, https://doi.org/10.5194/acp-24-8067-2024, 2024.
Guzman-Morales, J., Gershunov, A., Theiss, J., Li, H., and Cayan, D.: Santa Ana Winds of Southern California: Their climatology, extremes, and behavior spanning six and a half decades, Geophysical Research Letters, 43, 2827–2834, https://doi.org/10.1002/2016GL067887, 2016.
Grim, J. A., Rauber, R. M., McFarquhar, G. M., Jewett, B. F., and Jorgensen, D. P.: Development and forcing of the rear inflow jet in a rapidly developing and decaying squall line during BAMEX, Monthly Weather Review, 137, 1206–1229, https://doi.org/10.1175/2008mwr2503.1, 2009.
Grubišić, V., Doyle, J. D., Kuettner, J., Mobbs, S., Smith, R. B., Whiteman, C. D., Dirks, R., Czyzyk, S., Cohn, S. A., Vosper, S., Weissmann, M., Haimov, S., De Wekker, S. F. J., Pan, L. L., and Chow, F. K.: The terrain-induced rotor experiment: A field campaign overview including observational highlights, Bulletin of the American Meteorological Society, 89, 1513–1534, https://doi.org/10.1175/2008BAMS2487.1, 2008.
Hadavi, M. and Romanic, D.: Atmospheric conditions conducive to thunderstorms with downbursts in Canada and a downburst precursor parameter, Atmospheric Research, 305, 428, https://doi.org/10.1016/j.atmosres.2024.107428, 2024.
Han, B., Du, Y., Wu, C., and Liu, X.: Microphysical characteristics of the coexisting frontal and warm-sector heavy rainfall in South China, Journal of Geophysical Research: Atmospheres, 126, e2021JD035446, https://doi.org/10.1029/2021JD035446, 2021.
Haerter, J. O., Böing, S. J., Henneberg, O., and Nissen, S. B.: Circling in on convective organization, Geophysical Research Letters, 46, 7024–7034, https://doi.org/10.1029/2019GL082092, 2019.
Harris, A. R. and Kahl, J. D. W.: Gust factors: Meteorologically stratified climatology, data artifacts, and utility in forecasting peak gusts, Journal of Applied Meteorology and Climatology, 56, 3151–3166, https://doi.org/10.1175/jamc-d-17-0133.1, 2017.
Hersbach, H., Bell, B., Berrisford, P., Biavati, G., Horányi, A., Muñoz Sabater, J., Nicolas, J., Peubey, C., Radu, R., Rozum, I., Schepers, D., Simmons, A., Soci, C., Dee, D., and Thépaut, J.-N.: ERA5 hourly data on pressure levels from 1940 to present, Copernicus Climate Change Service (C3S) Climate Data Store (CDS) [data set], https://doi.org/10.24381/cds.bd0915c6, 2023.
Hirt, M. and Craig, G. C.: A cold pool perturbation scheme to improve convective initiation in convection-permitting models, Q. J. R. Meteorol. Soc., 147, 2429–2447, https://doi.org/10.1002/qj.4032, 2021.
Houze Jr., R. A.: Orographic effects on precipitating clouds, Rev. Geophys., 50, RG1001, https://doi.org/10.1029/2011RG000365, 2012.
Houze Jr., R. A. (Ed.): Chapter 9 – Mesoscale convective systems, in: International geophysics, Academic Press, pp. 237–286, https://doi.org/10.1016/B978-0-12-374266-7.00009-3, 2014.
Houze, R. A., Rutledge, S. A., Biggerstaff, M. I., and Smull, B. F.: Interpretation of Doppler Weather Radar Displays of Midlatitude Mesoscale Convective Systems, Bulletin of the American Meteorological Society, 70, 608–619, https://doi.org/10.1175/1520-0477(1989)070<0608:IODWRD>2.0.CO;2, 1989.
Johns, R. H. and Hirt, W. D.: Derechos: Widespread convectively induced windstorms, Weather and Forecasting, 2, 32–49, https://doi.org/10.1175/1520-0434(1987)002<0032:DWCIW>2.0.CO;2, 1987.
Johnson, R. H. and Hamilton, P. J.: The Relationship of Surface Pressure Features to the Precipitation and Airflow Structure of an Intense Midlatitude Squall Line. Monthly Weather Review, 116, 1444–1473, https://doi.org/10.1175/1520-0493(1988)116<1444:TROSPF>2.0.CO;2, 1988.
Kahl, J. D. W.: Forecasting peak wind gusts using meteorologically stratified gust factors and MOS guidance, Weather and Forecasting, 35, 1129–1143, https://doi.org/10.1175/waf-d-20-0045.1, 2020.
Kelley, D. I., Burton, C., Di Giuseppe, F., Jones, M. W., Barbosa, M. L. F., Brambleby, E., McNorton, J. R., Liu, Z., Bradley, A. S. I., Blackford, K., Burke, E., Ciavarella, A., Di Tomaso, E., Eden, J., Ferreira, I. J. M., Fiedler, L., Hartley, A. J., Keeping, T. R., Lampe, S., Lombardi, A., Mataveli, G., Qu, Y., Silva, P. S., Spuler, F. R., Steinmann, C. B., Torres-Vázquez, M. Á., Veiga, R., van Wees, D., Wessel, J. B., Wright, E., Bilbao, B., Bourbonnais, M., Gao, C., Di Bella, C. M., Dintwe, K., Donovan, V. M., Harris, S., Kukavskaya, E. A., N'Dri, A. B., Santín, C., Selaya, G., Sjöström, J., Abatzoglou, J. T., Andela, N., Carmenta, R., Chuvieco, E., Giglio, L., Hamilton, D. S., Hantson, S., Meier, S., Parrington, M., Sadegh, M., San-Miguel-Ayanz, J., Sedano, F., Turco, M., van der Werf, G. R., Veraverbeke, S., Anderson, L. O., Clarke, H., Fernandes, P. M., and Kolden, C. A.: State of Wildfires 2024–2025, Earth Syst. Sci. Data, 17, 5377–5488, https://doi.org/10.5194/essd-17-5377-2025, 2025.
Kolmogorov, A. N.: The local structure of turbulence in incompressible viscous fluid for very large Reynolds numbers, Doklady Akademii Nauk SSSR, 30, 299–303, 1941.
Kraichnan, R. H.: Inertial ranges in two-dimensional turbulence, The Physics of Fluids, 10, 1417–1423, https://doi.org/10.1063/1.1762301, 1967.
Lafore, J. and Moncrieff, M. W.: A numerical investigation of the organization and interaction of the convective and stratiform regions of tropical squall lines, Journal of the Atmospheric Sciences, 46, 521–544, https://doi.org/10.1175/1520-0469(1989)046<0521:ANIOTO>2.0.CO;2, 1989.
Lenschow, D. H., Savic-Jovcic, V., and Stevens, B.: Divergence and vorticity from aircraft air motion measurements, J. Atmos. Oceanic Technol., 24, 2062–2072, https://doi.org/10.1175/2007JTECHA940.1, 2007.
Letson, F., Pryor, S. C., Barthelmie, R. J., and Hu, W.: Observed gust wind speeds in the coterminous United States, and their relationship to local and regional drivers, J. Wind Eng. Ind. Aerodyn., 173, 199–209, https://doi.org/10.1016/j.jweia.2017.12.008, 2018.
Li, H., Cui, X., and Zhang, D. L.: On the initiation of an isolated heavy-rain-producing storm near the central urban area of Beijing metropolitan region, Monthly Weather Review, 145, 181–197, https://doi.org/10.1175/MWR-D-16-0115.1, 2017.
Liu, B., Guo, J., Gong, W., Shi, L., Zhang, Y., and Ma, Y.: Characteristics and performance of wind profiles as observed by the radar wind profiler network of China, Atmos. Meas. Tech., 13, 4589–4600, https://doi.org/10.5194/amt-13-4589-2020, 2020.
Liu, B., Ma, X., Guo, J., Wen, R., Li, H., Jin, S., Ma, Y., Guo, X., and Gong, W.: Extending the wind profile beyond the surface layer by combining physical and machine learning approaches, Atmos. Chem. Phys., 24, 4047–4063, https://doi.org/10.5194/acp-24-4047-2024, 2024.
Liu, Q., Xu, X., Zhao, K., and Zhou, A.: A merger-formation bow echo caused by low-level mesovortex in South China, Journal of Geophysical Research: Atmospheres, 128, e2022JD037954, https://doi.org/10.1029/2022JD037954, 2023.
Lombardo, K. and Kumjian, M. R.: Observations of the Discrete Propagation of a Mesoscale Convective System during RELAMPAGO–CACTI, Monthly Weather Review, 150, 2111–2138, https://doi.org/10.1175/MWR-D-21-0265.1, 2022.
Luchetti, N. T., Friedrich, K., Rodell, C. E., and Lundquist, J. K.: Characterizing thunderstorm gust fronts near complex terrain, Monthly Weather Review, 148, 3267–3286, https://doi.org/10.1175/mwr-d-19-0316.1, 2020.
Luu, L. N., van Meijgaard, E., Philip, S. Y., Kew, S. F., de Baar, J. H. S., and Stepek, A.: Impact of surface roughness changes on surface wind speed over western Europe: A study with the regional climate model RACMO, Journal of Geophysical Research: Atmospheres, 128, e2022JD038426, https://doi.org/10.1029/2022JD038426, 2023.
Lyu, M., Potter, H., Collins, C. O., Yang, X., and Wang, X.: The impacts of gustiness on the evolution of surface gravity waves, Geophysical Research Letters, 50, https://doi.org/10.1029/2023gl104085, 2023.
Mahoney, K. M. and Lackmann, G. M.: The sensitivity of momentum transport and severe surface winds to environmental moisture in idealized simulations of a mesoscale convective system, Monthly Weather Review, 139, 1352–1369, https://doi.org/10.1175/2010mwr3468.1, 2011.
Mahoney, K. M., Lackmann, G. M., and Parker, M. D.: The role of momentum transport in the motion of a quasi-idealized mesoscale convective system, Monthly Weather Review, 137, 3316–3338, https://doi.org/10.1175/2009mwr2895.1, 2009.
Mahrt, L., Vickers, D., Frederickson, P., Davidson, K., and Smedman, A.-S.: Sea-surface aerodynamic roughness, Journal of Geophysical Research, 108, 3171, https://doi.org/10.1029/2002JC001383, C6, 2003.
Marino, R., Pouquet, A., and Rosenberg, D.: Resolving the paradox of oceanic large-scale balance and small-scale mixing, Physical Review Letters, 114, 114504, https://doi.org/10.1103/physrevlett.114.114504, 2015.
Meng, Z., Zhang, F., Markowski, P., Wu, D., and Zhao, K.: A modeling study on the development of a bowing structure and associated rear inflow within a squall line over South China, Journal of the Atmospheric Sciences, 69, 1182–1207, https://doi.org/10.1175/JAS-D-11-0121.1, 2012.
Miller, J. E.: ON THE CONCEPT OF FRONTOGENESIS, Journal of the Atmospheric Sciences, 5, 169–171, https://doi.org/10.1175/1520-0469(1948)005<0169:OTCOF>2.0.CO;2, 1948.
Monahan, A. H., Rees, T., He, Y., and McFarlane, N.: Multiple regimes of wind, stratification, and turbulence in the stable boundary layer, Journal of the Atmospheric Sciences, 72, 3178–3198, https://doi.org/10.1175/jas-d-14-0311.1, 2015.
Monin, A. S. and Obukhov, A. M.: Basic laws of turbulent mixing in the surface layer of the atmosphere, Tr. Akad. Nauk SSSR Geophiz. Inst., 24, 163, 1954.
Neiman, P. J., Hardesty, R. M., Shapiro, M. A., and Cupp, R. E.: Doppler Lidar Observations of a Downslope Windstorm, Monthly Weather Review, 116, 2265–2275, https://doi.org/10.1175/1520-0493(1988)116<2265:DLOOAD>2.0.CO;2, 1988.
Oke, T.: Boundary Layer Climates, 2nd Edn., Routledge, London, UK, ISBN 9780415043199, 1987.
Peterson, T. C., Karl, T. R., Kossin, J. P., Kunkel, K. E., Lawrimore, J. H., Mcmahon, J. R., Vose, R. S., and Yin, X.: Changes in weather and climate extremes: State of knowledge relevant to air and water quality in the United States, Journal of the Air and Waste Management Association, 64, 184–197, https://doi.org/10.1080/10962247.2013.851044, 2014.
Powell, D. C. and Elderkin, C. E.: An investigation of the application of Taylor's hypothesis to atmospheric boundary layer turbulence, Journal of the Atmospheric Sciences, 31, 990–1002, https://doi.org/10.1175/1520-0469(1974)031<0990:AIOTAO>2.0.CO;2, 1974.
Powell, M. D., Vickery, P. J., and Reinhold, T. A.: Reduced drag coefficient for high wind speeds in tropical cyclones, Nature, 422, 279–283, https://doi.org/10.1038/nature01481, 2003.
Prein, A. F., Coen, J., and Jaye, A.: The character and changing frequency of extreme California fire weather, Journal of Geophysical Research: Atmospheres, 127, e2021JD035350, https://doi.org/10.1029/2021JD035350, 2022.
Pryor, S. C. and Barthelmie, R. J.: Climate change impacts on wind energy: A review, Renewable and Sustainable Energy Reviews, 14, 430–437, https://doi.org/10.1016/j.rser.2009.07.028, 2010.
Pryor, S. C. and Barthelmie, R. J.: Assessing climate change impacts on the near-term stability of the wind energy resource over the USA, Climate Dynamics, 108, 8167–8171, https://doi.org/10.1007/s00382-010-0955-3, 2011.
Pryor, S. C. and Barthelmie, R. J.: A global assessment of extreme wind speeds for wind energy applications, Nature Energy, 6, 268–276, https://doi.org/10.1038/s41560-020-00773-7, 2021.
Pryor, S. C., Barthelmie, R. J., and Schoof, J. T.: Past and future wind climates over the contiguous USA based on the North American Regional Climate Change Assessment Program model suite, Journal of Geophysical Research, 117, D19119, https://doi.org/10.1029/2012JD017449, 2012.
Raupach, M. R.: Simplified expressions for vegetation roughness length and zero-plane displacement as functions of canopy height and area index, Bound.-Lay. Meteorol., 71, 211–216, https://doi.org/10.1007/BF00709229, 1994.
Rocque, M. N. and Rasmussen, K. L.: The Impact of Topography on the Environment and Life Cycle of Weakly and Strongly Forced MCSs during RELAMPAGO, Monthly Weather Review, 150, 2317–2338, https://doi.org/10.1175/MWR-D-22-0049.1, 2022.
Romanic, D., Chowdhury, J., Chowdhury, J., and Hangan, H.: Investigation of the transient nature of thunderstorm winds from Europe, the united states, and Australia using a new method for detection of changepoints in wind speed records, Monthly Weather Review, 148, 3747–3771, https://doi.org/10.1175/MWR-D-19-0312.1, 2020.
Shao, X., Zhang, N., Peng, Z., Zhao, K., Luo, Y., and Song, X.: Observed surface drag coefficient under high wind speed conditions and the relationship with coherent structures, Journal of Geophysical Research: Atmospheres, 127, https://doi.org/10.1029/2021jd035301, 2022.
Shao, X., Zhang, N., and Tang, J.: A physical model for the observed inverse energy cascade in typhoon boundary layers, Geophysical Research Letters, 50, https://doi.org/10.1029/2023gl105546, 2023a.
Shao, X., Zhang, N., and Tang, J.: The impact of observed drag reduction over land on typhoon forecasting, Journal of Geophysical Research: Atmospheres, 128, https://doi.org/10.1029/2022jd038278, 2023b.
Shapiro, A., Potvin, C. K., and Jidong, G.: Use of a vertical vorticity equation in variational dual-Doppler wind analysis, J. Atmos. Oceanic Technol., 26, 2089–2106, 2009.
Shi, Y. and Hu, F.: Ramp-like PM2.5 accumulation process and Z-less similarity in the stable boundary layer, Geophysical Research Letters, 47, e2019GL086530, https://doi.org/10.1029/2019gl086530, 2020.
Shi, Y., Hu, F., Xiao, Z. S., Fan, G. Q., and Zhang, Z.: Comparison of four different types of planetary boundary layer heights during a haze episode in Beijing, Science of the Total Environment, 711, 134928, https://doi.org/10.1016/j.scitotenv.2019.134928, 2020.
Smith, R. B.: The influence of mountains on the atmosphere, Advances in Geophysics, 21, 87–230, https://doi.org/10.1016/S0065-2687(08)60262-9, 1979.
Su, T. N., Li, Z. Q., and Zheng, Y. T.: Cloud-Surface Coupling Alters the Morning Transition from Stable to Unstable Boundary Layer, Journal of Geophysical Research, 50, e2022GL102256, https://doi.org/10.1029/2022gl102256, 2023.
Tang, J., Byrne, D., Zhang, J. A., Wang, Y., Lei, X.-T., Wu, D., Fang, P., and Zhao, B.: Horizontal transition of turbulent cascade in the near-surface layer of tropical cyclones, Journal of the Atmospheric Sciences, 72, 4915–4925, https://doi.org/10.1175/jas-d-14-0373.1, 2015.
Taszarek, M., Pilguj, N., Orlikowski, J., Surowiecki, A., Walczakiewicz, S., Pilorz, W., Piasecki, K., Pajurek, Ł., and Półrolniczak, M.: Derecho evolving from a mesocyclone – A study of 11 August 2017 severe weather outbreak in Poland: Event analysis and high-resolution simulation, Monthly Weather Review, 147, 2283–2306, https://doi.org/10.1175/MWR-D-18-0330.1, 2019.
Taylor, G. I.: The spectrum of turbulence, Proc. R. Soc. London, A164, 476–490, 1938.
Torralba, V., Doblas-Reyes, F. J., and Gonzalez-Reviriego, N.: Uncertainty in recent near-surface wind speed trends: A global reanalysis intercomparison, Environmental Research Letters, 12, 114019, https://doi.org/10.1088/1748-9326/aa8a58, 2017.
Tucker, S. C., Senff, C. J., Weickmann, A. M., Brewer, W. A., Banta, R. M., Sandberg, S. P., Law, D. C., and Hardesty, R. M.: Doppler lidar estimation of mixing height using turbulence, shear, and aerosol profiles, J. Atmos. Oceanic Technol., 26, 673–688, https://doi.org/10.1175/2008JTECHA1157.1, 2009.
Vose, R. S., Applequist, S., Bourassa, M. A., Pryor, S. C., Barthelmie, R. J., Blanton, B., Bromirski, P. D., Brooks, H. E., DeGaetano, A. T., Dole, R. M., Easterling, D. R., Jensen, R. E., Karl, T. R., Katz, R. W., Klink, K., Kruk, M. C., Kunkel, K. E., MacCracken, M. C., Peterson, T. C., Shein, K., Thomas, B. R., Walsh, J. E., Wang, X. L., Wehner, M. F., Wuebbles, D. J., and Young, R. S.: Monitoring and understanding changes in extremes: Extratropical storms, winds, and waves, Bulletin of the American Meteorological Society, 95, 377–386, https://doi.org/10.1175/BAMS-D-12-00162.1, 2014.
Wakimoto, R. M., Murphey, H. V., Davis, C. A., and Atkins, N. T.: High winds generated by bow echoes. Part II: The relationship between the mesovortices and damaging straight-line winds, Monthly Weather Review, 134, 2813–2829, https://doi.org/10.1175/MWR3216.1, 2006.
Wandishin, M. S., Stensrud, D. J., Mullen, S. L., and Wicker, L. J.: On the predictability of mesoscale convective systems: Three-dimensional simulations, Monthly Weather Review, 138, 863–885, https://doi.org/10.1175/2009MWR2961.1, 2010.
Weisman, M. L.: The role of convectively generated rear-inflow jets in the evolution of long-lived mesoconvective systems, Journal of the Atmospheric Sciences, 49, 1826–1847, https://doi.org/10.1175/1520-0469(1992)049<1826:TROCGR>2.0.CO;2, 1992.
Weisman, M. L. and Davis, C. A.: Mechanisms for the generation of mesoscale vortices within quasi-linear convective systems, Journal of the Atmospheric Sciences, 55, 2603–2622, https://doi.org/10.1175/1520-0469(1998)055<2603:MFTGOM>2.0.CO;2, 1998.
Weisman, M. L. and Trapp, R. J.: Low-level mesovortices within squall lines and bow echoes. Part I: Overview and dependence on environmental shear, Monthly Weather Review, 131, 2779–2803, https://doi.org/10.1175/1520-0493(2003)131<2779:LMWSLA>2.0.CO;2, 2003.
Wilson, J. W., Feng, Y., Chen, M., and Roberts, R. D.: Nowcasting challenges during the Beijing Olympics: Successes, failures, and implications for future nowcasting systems, Weather and Forecasting, 25, 1691–1714, https://doi.org/10.1175/2010WAF2222417.1, 2010.
Wheatley, D. M. and Trapp, R. J.: The effect of mesoscale heterogeneity on the Genesis and structure of mesovortices within quasi-linear convective systems, Monthly Weather Review, 136, 4220–4241, https://doi.org/10.1175/2008MWR2294.1, 2008.
Wu, L., Su, H., Zeng, X., Posselt, D. J., Wong, S., Chen, S., and Stoffelen, A.: Uncertainty of Atmospheric Winds in Three Widely Used Global Reanalysis Datasets, Journal of Applied Meteorology and Climatology, 63, 165–180, https://doi.org/10.1175/JAMC-D-22-0198.1, 2024.
Xiao, X, Sun, J., Chen, M. X., Qie, X., Wang, Y., and Ying, Z. M.: The characteristics of weakly forced mountain-to-plain precipitation systems based on radar observations and high-resolution reanalysis, Journal of Geophysical Research: Atmospheres, 122, 3193–3213, 2017.
Xiao, X, Sun, J., Chen, M. X., Qie, X., Ying, Z. M., Wang, Y., and Ji, L.: Comparison of environmental and mesoscale characteristics of two types of mountain-to-plain precipitation systems in the Beijing region, China, Journal of Geophysical Research: Atmospheres, 124, 6856–6872, 2019.
Xu, X., Xue, M., and Wang, Y.: The genesis of mesovortices within a real-data simulation of a bow echo system, Journal of the Atmospheric Sciences, 72, 1963–1986. https://doi.org/10.1175/JAS-D-14-0209.1, 2015a.
Xu, X., Xue, M., and Wang, Y.: Mesovortices within the 8 May 2009 bow echo over the central United States: Analyses of the characteristics and evolution based on Doppler radar observations and a high-resolution model simulation, Monthly Weather Review, 143, 2266–2290, https://doi.org/10.1175/MWR-D-14-00234.1, 2015b.
Xu, X., Ju, Y., Liu, Q., Zhao, K., Xue, M., Zhang, S., Zhou, A., Wang, Y., and Tang, Y.: Dynamics of Two Episodes of High Winds Produced by an Unusually Long-Lived Quasi-Linear Convective System in South China, Journal of the Atmospheric Sciences, 81, 1449–1473, https://doi.org/10.1175/JAS-D-23-0047.1, 2024.
Yanai, M. and Nitta, T.: Computation of vertical motion and vorticity budget in a Caribbean easterly wave, J. Meteor. Soc. Japan, 45, 444–466, 1967.
Yang, H. and Du, Y.: Distinct Convection Initiation Near and Far ahead of an Idealized Squall Line, Journal of the Atmospheric Sciences, 83, 151–168, https://doi.org/10.1175/JAS-D-25-0073.1, 2026.
Zhang, D.-L.: The Formation of a cooling-induced mesovortex in the trailing stratiform region of a midlatitude squall line, Monthly Weather Review, 120, 2763–2785, https://doi.org/10.1175/1520-0493(1992)120<2763:TFOACI>2.0.CO;2, 1992.
Zhang, D.-L., and Gao, K.: Numerical simulation of an intense squall line during 10–11 June 1985 PRE-STORM. Part II: Rear inflow, surface pressure perturbations and stratiform precipitation, Monthly Weather Review, 117, 2067–2094, 1989.
Zhang, L., Sun, J., Ying, Z., and Xiao, X.: Initiation and development of a squall line crossing Hangzhou Bay, Journal of Geophysical Research: Atmospheres, 126, https://doi.org/10.1029/2020JD032504, 2021.
Zhou, A., Zhao, K., Lee, W.-C., Huang, H., Hu, D., and Fu, P.: VDRAS and polarimetric radar investigation of a bow echo formation after a squall line merged with a preline convective cell, Journal of Geophysical Research: Atmospheres, 125, e2019JD031719. https://doi.org/10.1029/2019JD031719, 2020.
Zhou, X., Zhang, C., Xiao, Z., Li, Y., and Lu, G.: Inverse Energy Cascades in the Boundary Layer During Strong Winds Based on Doppler Lidar, Geophysical Research Letters, 52, https://doi.org/10.1029/2024GL113273, 2025.
Short summary
Wind gusts threaten safety and infrastructure but are hard to predict. To address this gap, we studied an extreme wind gust event in Beijing on 30 May 2024. We used seven radar wind profilers to track how this gust developed. It formed when cold northeasterly air clashed with warm southerly winds as the storm moved downhill. Evaporation of rain cooled the air, boosting downward air movement and wind strength. The turbulence transferring energy from small to large eddies intensify winds.
Wind gusts threaten safety and infrastructure but are hard to predict. To address this gap, we...
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