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  • Pourquoi nos forêts de sapins disparaissent
  • Kinetic theory. Volume 2, Irreversible processes
  • D02110 - Northerly surface winds over the eastern North Pacific Ocean in spring and summer (DOI 10. 1029/2006JD008053)
  • Climate analysis with satellite versus weather station data
  • 45 BEACON - LETTER FROM HEADQUARTERS - Policy as a Core Mission Activity of the Society
  • Inter-comparison of interpolated background nitrogen dioxide concentrations across Greater Manchester, UK
  • The lost colony and Jamestown droughts
  • Scénarios of extreme temperature events
  • A CO2 laser scintillometer for C index N2 measurements over a many kilometer path
  • Path length variations caused by atmospheric water vapor and their effects on the measurement of mesoscale ocean circulation features by a radar altimeter
  • An analysis of regional haze using tracers of opportunity
  • Application of hydrologic models to rangelands
  • TRANSIENT EDDY FORCING OF BLOCKING FLOWS
  • TORRO THUNDERSTORM REPORT : APRIL 1985
  • AN ANALYSIS OF WAVE HEIGHT RECORDS FOR THE N.E. ATLANTIC
  • WINTER THUNDERSTORMS IN SOUTHERN NORWAY
  • RESONANT INTERACTIONS BETWEEN UNSTABLE AND NEUTRAL BAROCLINIC WAVES : 2
  • Conservative Scheme for the Compressible Nonhydrostatic Models with the Horizontally Explicit and Vertically Implicit Time Integration Scheme
  • The extremes of the extremes : extraordinary floods
  • Climate, history and the modern world

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