By D. D. Alexakis, D. G. Hadjimitsis, S. Michaelides, I. Tsanis, A. Retalis, C. Demetriou (auth.), Costas G. Helmis, Panagiotis T. Nastos (eds.)
This booklet primarily contains the lawsuits of the eleventh overseas convention of Meteorology, Climatology and Atmospheric Physics (COMECAP 2012) that's held in Athens from 30 could to at least one June 2012. The convention addresses researchers, pros and scholars attracted to the subsequent issues: Agricultural Meteorology and Climatology, Air caliber, utilized Meteorology and Climatology, purposes of Meteorology within the strength area, 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 comprises all papers which have been authorised for presentation on the conference.
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Additional info for Advances in Meteorology, Climatology and Atmospheric Physics
1189 A. Poupkou, K. Markakis, N. M. Giannaros, U. Im, N. Daskalakis, S. Myriokefalitakis, D. Melas, P. Zanis, M. S. Zerefos Temporal Variability of Surface Ozone Concentrations in Volos, Greece . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1197 G. Proias, I. Larissi, K. T. G. Paliatsos Air Pollution in Eastern Mediterranean: Nested-Grid GEOS-CHEM Model Results and Airborne Observations . . . . . . . . . . . . . . . P. Protonotariou, E.
Precipitation diagram for the flood period event (lower left). Diagram of observed and simulated flow results for the period 2003 and 2010 (lower right) (mountainous) part of the catchment area (Fig. 3 lower left). Similarly, temperature data were provided from “Politiko” and “Kornos” weather stations that are established in close vicinity to the study area. The meteorological data covered a period of 3 years in total (2 years before and 1 year after the event). In addition, concerning the calibration process and assessment of the accuracy of simulated runoff results, observed flow data from “Potamia”, “Kotsiatis” and “Nisou” stream gauges for the same period were used.
The parameters of the model are representative cross-sections including left and right bank locations roughness coefficients (Manning’s coefficient) and finally contraction and expansion coefficients. The roughness coefficients are crucial for the implementation of the model (they represent a surface’s resistance to flow and are integral parameters for the calculation of water depth) and are calculated by combining land use data with tables of Manning’s n values. As it was mentioned the rainfall-runoff models simulate the runoff response of an area to a given amount and distribution of precipitation over a certain period of time.
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.)