By D. D. Alexakis, D. G. Hadjimitsis, S. Michaelides, I. Tsanis, A. Retalis, C. Demetriou (auth.), Costas G. Helmis, Panagiotis T. Nastos (eds.)
This ebook basically includes the lawsuits of the eleventh overseas convention of Meteorology, Climatology and Atmospheric Physics (COMECAP 2012) that's held in Athens from 30 may possibly to at least one June 2012. The convention addresses researchers, pros and scholars attracted to the subsequent themes: Agricultural Meteorology and Climatology, Air caliber, utilized Meteorology and Climatology, functions of Meteorology within the power zone, Atmospheric Physics and Chemistry, Atmospheric Radiation, Atmospheric Boundary Layer, Biometeorology and Bioclimatology, weather Dynamics, Climatic alterations, Cloud Physics, Dynamic and Synoptic Μeteorology, severe occasions, Hydrology and Hydrometeorology, Mesoscale Meteorology, Micrometeorology/Urban Microclimate, distant Sensing/ satellite tv for pc Meteorology and Climatology, climate research and Forecasting. The booklet contains all papers which were accredited for presentation on the conference.
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Extra info for Advances in Meteorology, Climatology and Atmospheric Physics
1227 R. G. Charalambides Carbonaceous Aerosols Over the Mediterranean and Black Sea . . . 1233 C. Theodosi, D. Smouliotis, P. Zarmpas, M. Kocak, and N. Mihalopoulos Physical and Chemical Processes of Polluted Air Masses During Etesians: Aegean-Game Airborne Campaign – An Outline . . . . . . 1239 M. Tombrou, E. Bossioli, J. Kalogiros, J. Allan, A. Bacak, G. Biskos, H. Coe, A. Dandou, G. Kouvarakis, N. P. Protonotariou, B. Szabo´-Taka´cs, and E. Triantafillou xxx Contents Lignite Power Plant’s Contribution to the Particulate Pollution in the Grater Western Macedonia Area, Greece .
J. Ioannou between cumulus clouds and the large scale flow (Charney and Eliasen 1964), or between surface heat fluxes and the surface wind (Rotunno and Emanuel 1987). Another theory is based on the idea that patches of high vorticity associated with individual convective systems are quickly axisymmetrized, feeding their energy into the vortex scale flow (Montgomery and Enagonio 1998), a process that can be described in terms of the interaction between Vortex Rossby Waves (VRW) and the circular vortex (Montgomery and Kallenbach 1997).
Farrell 20 real(ρ(t)) 10 0 −10 −20 0 5 10 15 t Fig. 1 Evolution of perturbation density for sheared wave perturbations with (k, l, m) ¼ (1, 8, 5). 6, 1) t ¼ l/k ¼ 8. At that time, the large amplification of the vorticity wave’s meridional velocity due to the Orr mechanism is transferred to vertical velocity, exciting in this case gravity waves. The amplitude of these forced waves increases rapidly and saturates at large values as illustrated in Fig. 1. The amplitude of the forced waves can be calculated in closed form (Bakas and Farrell 2009b) and is of order q(0)FS1/4 for F ~ O(1) showing that a large initial potential vorticity perturbation leads to substantial excitation of waves.
Advances in Meteorology, Climatology and Atmospheric Physics by D. D. Alexakis, D. G. Hadjimitsis, S. Michaelides, I. Tsanis, A. Retalis, C. Demetriou (auth.), Costas G. Helmis, Panagiotis T. Nastos (eds.)