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The 1954 start of operational Numerical Weather Prediction in Sweden

The 1954 start of operational Numerical Weather Prediction in Sweden. Why Sweden? -C. G. Rossby back from the US 1947 (home-longing, management and politics) -Swedish state-of-art computers (BARK 1950, BESK 1953) -International support (from the USA and Belgium). 1953 BESK=

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The 1954 start of operational Numerical Weather Prediction in Sweden

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  1. The 1954 start of operational Numerical Weather Prediction in Sweden NWP Symposium University of Maryland June 2004

  2. Why Sweden? -C. G. Rossby back from the US 1947 (home-longing, management and politics) -Swedish state-of-art computers (BARK 1950, BESK 1953) -International support (from the USA and Belgium) NWP Symposium University of Maryland June 2004

  3. 1953 BESK= Binary Electronic Sequence Calculator NWP Symposium University of Maryland June 2004

  4. BESK In 1953 the world’s “best” computer Arithmetic unit Electrostatic drum memory Control desk “Williams tube” memory NWP Symposium University of Maryland June 2004

  5. The International Meteorological Institute Rossby wanted, like V. Bjerknes after WWI, to play an international role in the political reconstruction after WWII Steyer Vuorela Eady Hubert Rossby V. Mieghem NWP Symposium University of Maryland June 2004

  6. Baroclinic or barotropic models? …yes, but the large scale motion can kinematically be described by a barotropic model The atmospheric motions are driven by thermal processes as reflected in baroclinic developments C. G. Rossby R. C. Sutcliffe NWP Symposium University of Maryland June 2004

  7. Common misinterpretations of Rossby’s barotropic concept -Only valid for stationary waves -Can only perform linear extrapolations -Only valid for barotropic features -Group velocity…. NWP Symposium University of Maryland June 2004

  8. The concept of group velocity tells us that any boundaries have to be placed far enough away from the verification region 24-hour compu- tational areas for - MISU - UKMO NWP Symposium University of Maryland June 2004

  9. A +24 hour forecast from the UKMO system winter 1953-54 Boundary errors and numerical instability NWP Symposium University of Maryland June 2004

  10. Only in 1965 did the UKMO go operational with NWP after a personal intervention by the new Director General John Mason Dear members of the press, radio and TV... Oh dear... NWP Symposium University of Maryland June 2004

  11. In Stockholm tendency calculations were carried out, first by hand in 1952, later on BESK in 1953 The Swedish tabloid “Expressen” published the results almost a year before “Tellus” (forecast left, analysis right) NWP Symposium University of Maryland June 2004

  12. Barotropic re-run of the “tree-feller” storm the 2-3 January 1954 2 January 1954 00 UTC +24 h baro- tropic forecast 3 January 1954 00 UTC NWP Symposium University of Maryland June 2004

  13. First real time NWP in late September 1954 Not quite the 72 hour computational area 72 hour verification area NWP Symposium University of Maryland June 2004

  14. From the operational period Dec 1954-May 1955 -Professor Dahlqvist, when is Spring coming? NWP Symposium University of Maryland June 2004

  15. -Tomorrow at 2 pm! +72 hours NWP Symposium University of Maryland June 2004

  16. …and Spring came! NWP Symposium University of Maryland June 2004

  17. Why Sweden succeeded: -C. G. Rossby back from the USA 1947 -Swedish state-of-art computers -International support -Choice of barotropic model (skilful and providing operational experience) -Efficient automatic analysis system (Bergthorsson-Döös, 1955) -Not too small NWP area (but not too big either, avoiding retrogression of the planetary waves!) NWP Symposium University of Maryland June 2004

  18. From wheat to bread! Bert Bolin shows automated 500 mb forecasts for Ragnar Fjørtoft (Norway) and George Corby (UK) around 1956 NWP Symposium University of Maryland June 2004

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