caa a22 4500 469052724 CHVBK 20180323132834.0 cr unu---uuuuu 170328e19920601xx s 000 0 eng 10.1007/BF01025620 doi (NATIONALLICENCE)springer-10.1007/BF01025620 Petkovšek Z. Department of Physics, Faculty of Sciences (FNT), P.O. Box 64, 61111, Ljubljana, Slovenia aut Turbulent dissipation of cold air lake in a basin [Elektronische Daten] [Z. Petkovšek] Summary: Problems of turbulent dissipation of a cold air lake (CAL) and the inversion layer bordering CAL on the upper boundary are presented and studied with the compound model. In wintertime such cold air lakes can persist for days even if rather strong winds are blowing above them. The required conditions for CAL dissipation are removed processes of its formation or maintenance, as well as a sufficiently strong invasion of turbulence in the inversion layer from above down-wards. By this, the inversion layer at first becomes stronger and dissipation is stopped, until the increase of turbulent kinetic energy of the upper flow enables further dissipation. Such turbulent dissipation process is shown by the model for typical conditions and for different initial values of the relevent variables. Springer-Verlag, 1992 Meteorology and Atmospheric Physics Springer-Verlag 47/2-4(1992-06-01), 237-245 0177-7971 47:2-4<237 1992 47 703 https://doi.org/10.1007/BF01025620 text/html Onlinezugriff via DOI 1 research-article jats NATIONALLICENCE 856 40 https://doi.org/10.1007/BF01025620 text/html Onlinezugriff via DOI NATIONALLICENCE 100 1- Petkovšek Z. Department of Physics, Faculty of Sciences (FNT), P.O. Box 64, 61111, Ljubljana, Slovenia aut NATIONALLICENCE 773 0- Meteorology and Atmospheric Physics Springer-Verlag 47/2-4(1992-06-01), 237-245 0177-7971 47:2-4<237 1992 47 703 Metadata rights reserved Springer special CC-BY-NC licence nationallicence BK010053 XK010053 XK010000 NATIONALLICENCE NATIONALLICENCE NL-springer