Titlebook: Weather and Weather Maps; A Volume Dedicated t G?sta H. Liljequist Book 1981 Springer Basel AG 1981 memory.Volume.Weather.Weather map

Plaque

打谷工具

Pseudo-cold-fronts in the USA,ation in driving these circulations, their relation to the synoptic-scale environment including the supply of water vapor, the character of the pseudo-cold-front boundary, and the distribution of precipitation related to severe storm circulations.

GLUE

Synoptic Meteorology: An Historical Review,950 are mostly considered as lying too near in time to be viewed ‘historically’. Achievements or methods without a clear connection with forecasting weather will generally not be treated. Not even will space permit any account of the advances in the fields of cloud physics, orographic effects or dyn

思考才皺眉

,Tor Bergeron’s First Year in the Bergen School: Towards an Historical Appreciation,ted with ‘the structure of scientific revolutions’. But in some respects the prevailing state of affairs was acutely disturbing. Not enough was being done in the detailed analysis of actual cases of scientific revolutions, and the whole subject was in danger of becoming a jousting-ground for the con

N斯巴達(dá)人

BARB

,Comments on Tor Bergeron’s Contributions to Synoptic Meteorology,been a member of the original Bergen School in 1919 and had returned to it twice in the 1920’s, his line of work differed remarkably from that of the other members. In his own way, he decisively helped his Norwegian colleagues to win worldwide recognition for the so-called polar front theory, not by

我要威脅

On the Concept of Indirect Aerology, various weather systems and their three-dimensional structure. The models of cyclones and fronts were created by the Bergen school, and Bergeron shares the merit for this work with other members of that school. However, nobody possessed his pedagogic interest, enthusiasm and ability in bringing ‘th

難管

The Weather Forecast, now predict the development of synoptic weather systems in great detail for a few days ahead, while large-scale phenomena like blocking can be predicted for about a week or more..The local forecasting problem is presently being attacked by statistical- and meso-scale models using the large-scale pr

易受刺激

,Insight into the Nature of Precipitation — Some Achievements by T. Bergeron in Retrospect,anner. Naturally, this is not an automatic process and the new fields opened up may, for the favourable growth of new ideas, be ‘seeded’ by previous knowledge, scientific intuition and stimulation — and still there will be no guarantee for scientific progress.

Dignant

Bergeron and the Oreigenic (Orographic) Maxima of Precipitation,windward side of slopes. However, remembering the complexities of the precipitation process, many exceptions to this simple rule must occur. Suffice it to mention that over large mountain ranges the precipitation at the divide is only a small fraction of the upslope maximum, the latter usually occur