pure and applied geophysics

, Volume 119, Issue 3, pp 558–576 | Cite as

Bergeron and the oreigenic (orographic) maxima of precipitation

  • Tage Andersson


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  1. Andersson, T. (1964),On the Accuracy of Rain Measurements and Statistical Results from Rain Studies with Dense Networks (Project Pluvius), Ark. Geofys.4 (13), 307–332. Also MIUM.Google Scholar
  2. Andersson, T. (1969a),Stockholmstraktens nederbörd (Precipitation of the Stockholm Region), MIUR,14.Google Scholar
  3. Andersson, T. (1969b),Small-Scale Variations of the Contamination of Rain Caused by the Low Layers of the Atmosphere, Tellus21, 685–692.Google Scholar
  4. Bader, M. J., andRoach, W. T. (1977),Orographic Rainfall in Warm Sections of Depressions, Q. Jl R. met. Soc.100, 269–280.Google Scholar
  5. Bergeron, T. (1949),The Problem of Artificial Rainfall on the Globe. The Coastal Orographic Maxima of Precipitation in Autumn and Winter, Tellus1 (3), 15–32.Google Scholar
  6. Bergeron, T. (1960a),Problems and Methods of Rainfall Investigations. Address of the Honorary Chairman of the Conference, Monogr. No. 5, Am. Geophys. Union, pp. 5–30.Physics of Precipitation, Proc. of the Cloud Physics Conference, Woods Hole, Mass., 1959. Baltimore, Md. Also MIUM,73.Google Scholar
  7. Bergeron, T. (1960b),Operation and Results of ‘Project Pluvius’, Monogr. No. 5, Am. Geophys. Union, pp. 152–157. Also MIUM,74.Google Scholar
  8. Bergeron, T. (1960c),Possible Man-made Great-Scale Modifications of Precipitation Climate in Sudan, Monogr. No. 5, Am. Geophys. Union, pp. 399–401. Also MIUM,75.Google Scholar
  9. Bergeron, T. (1961),Preliminary Results of Project Pluvius, I.A.S.H. Publ. No. 53, pp. 226–237. Also MIUM,80.Google Scholar
  10. Bergeron, T. (1963),Synpunkter på sommarprognoser (On Summer Forecasts). Stencil. (Swedish Meteorological and Hydrological Institute, Stockholm.)Google Scholar
  11. Bergeron, T. (1965),On the Low-Level Redistribution of Atmospheric Water Caused by Orography, Proc. of the Int. Conf. on Cloud Physics, Tokyo and Sapporo, May 24–June 1, 1965, pp. 96–100. Also MIUM,92, and Project Pluvius Report 5.Google Scholar
  12. Bergeron, T. (1967–68),Mesometeorological Studies of Precipitation (MSP), I–III. (Met. Inst. Uppsala.)Google Scholar
  13. Bergeron, T. (1970),Mesometeorological Studies of Precipitation (MSP), IV. Oreigenic and convective rainfall patterns. With a collection of annotated maps for the Uppsala field, 1953–63. MIUR,20.Google Scholar
  14. Bergeron, T. (1973),Mesometeorological Studies of Precipitation (MSP), V. Monthly rainfall in the Uppsala field. With a collection of annotated maps, 1955–65. MIUR,52.Google Scholar
  15. Browning, K. A. (1980),Structure, Mechanism and Prediction of Orographically Enhanced Rain in Britain. Orographic Effects in Planetary Flows. GARP publication series, No. 23, pp. 86–114.Google Scholar
  16. Dahlström, B. (1973),Investigation of Errors in Rainfall Observations, MIUR,34.Google Scholar
  17. Ludlam, F. H. (1952),Orographic Cirrus Clouds, Q. Jl R. met. Soc.78, 554–562.Google Scholar
  18. Schubert, J. (1905),Wald und Niederschlag in Schlesien, Met. Zeitschrift.40, 566.Google Scholar
  19. Smith, R. B. (1979),The Influence of Mountains on the Atmosphere, Adv. Geophys.21, 169–194.Google Scholar
  20. Storebø, P. B. (1976),Small Scale Topographical Influences on Precipitation, Tellus28, 45–59.Google Scholar
  21. MIUM=Meteorological Institute of Uppsala University, Meddelanden (Communications).Google Scholar
  22. MIUR=Meteorological Institute of Uppsala University, Reports.Google Scholar

Copyright information

© Birkhäuser Verlag 1981

Authors and Affiliations

  • Tage Andersson
    • 1
  1. 1.Swedish Meteorological and Hydrological InstituteNorrköpingSweden

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