caa a22 4500 469052449 CHVBK 20180323132833.0 cr unu---uuuuu 170328e19920301xx s 000 0 eng 10.1007/BF01029575 doi (NATIONALLICENCE)springer-10.1007/BF01029575 Kraus H. Meteorologisches Institut der Universität Bonn, Puf dem Hügel 20, D-W-5300, Bonn 1, Germany aut Turbulence frontogenesis [Elektronische Daten] [H. Kraus] Summary: The frontogenesis function in terms of the time derivative of the gradient of any relevant airborne quantity comprises all processes contributing to frontogenesis. Thus the various terms of this function are able to reveal processes of frontal development and their structure. Therefore the evaluation of these terms from measurements or in the frame of model simulations offers the chance of gaining more insight in frontal processes. If frontogenesis is evaluated from average basic data representative for a certain time-or space-scale, the result will be a kind of average frontogenesis, which naturally contains turbulence terms in the form of covariances. The processes described by these terms are called turbulence frontogenesis. This paper describes the basic formalisms of turbulence frontogenesis, offers cross-sections of these terms gained in experiments flown in sea-breeze fronts and gives some hints about their general behaviour. Springer-Verlag, 1992 Meteorology and Atmospheric Physics Springer-Verlag 48/1-4(1992-03-01), 309-315 0177-7971 48:1-4<309 1992 48 703 https://doi.org/10.1007/BF01029575 text/html Onlinezugriff via DOI 1 research-article jats NATIONALLICENCE 856 40 https://doi.org/10.1007/BF01029575 text/html Onlinezugriff via DOI NATIONALLICENCE 100 1- Kraus H. Meteorologisches Institut der Universität Bonn, Puf dem Hügel 20, D-W-5300, Bonn 1, Germany aut NATIONALLICENCE 773 0- Meteorology and Atmospheric Physics Springer-Verlag 48/1-4(1992-03-01), 309-315 0177-7971 48:1-4<309 1992 48 703 Metadata rights reserved Springer special CC-BY-NC licence nationallicence BK010053 XK010053 XK010000 NATIONALLICENCE NATIONALLICENCE NL-springer