↑ Browning, Keith A. ; Frank H. Ludlam ( 1962 年 4 月)。「対流性暴風雨における気流」(PDF)。Quarterly Journal of the Royal Meteorological Society。88 ( 376): 117–35。Bibcode : 1962QJRMS..88..117B 。doi : 10.1002 / qj.49708837602。Browning, KA ; Ludlam, FH (1962). "対流性暴風雨における気流". Quarterly Journal of the Royal Meteorological Society . 88 (378): 555. Bibcode : 1962QJRMS..88..555B . doi : 10.1002/qj.49708837819 .
↑Browning, Keith A. (November 1964). "Airflow and Precipitation Trajectories Within Severe Local Storms Which Travel to the Right of the Winds". J. Atmos. Sci. 21 (6): 634–9. Bibcode:1964JAtS...21..634B. doi:10.1175/1520-0469(1964)021<0634:AAPTWS>2.0.CO;2. hdl:2027/mdp.39015095125533.
↑Browning, Keith (November 1965). "Some Inferences About the Updraft Within a Severe Local Storm". J. Atmos. Sci. (abstract). 22 (6): 669–77. Bibcode:1965JAtS...22..669B. doi:10.1175/1520-0469(1965)022<0669:SIATUW>2.0.CO;2. hdl:2027/mdp.39015095128867.
↑Sting Jets in Severe Northern European WindstormsArchived 2014-03-20 at the Wayback Machine
↑"Keith Browning". royalsociety.org. Retrieved 15 June 2022.
↑"Fellows". Royal Society. Retrieved 20 December 2010.
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