Download Advances in Meteorology, Climatology and Atmospheric Physics by D. D. Alexakis, D. G. Hadjimitsis, S. Michaelides, I. PDF

By D. D. Alexakis, D. G. Hadjimitsis, S. Michaelides, I. Tsanis, A. Retalis, C. Demetriou (auth.), Costas G. Helmis, Panagiotis T. Nastos (eds.)

ISBN-10: 3642291716

ISBN-13: 9783642291715

ISBN-10: 3642291724

ISBN-13: 9783642291722

This booklet basically includes 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 drawn to the subsequent themes: Agricultural Meteorology and Climatology, Air caliber, utilized Meteorology and Climatology, purposes of Meteorology within the strength zone, Atmospheric Physics and Chemistry, Atmospheric Radiation, Atmospheric Boundary Layer, Biometeorology and Bioclimatology, weather Dynamics, Climatic adjustments, 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 permitted for presentation on the conference.

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4 Set Up of Hydrological Model According to Neitsch et al. (2005) SWAT is a conceptual semi-distributed model for watershed hydrology and water quality operating on a daily step. A crucial factor that is usually taken into account is the spatial heterogeneity of the model considering information for elevation (Digital Elevation Model/DEM), soil and land use. The research team proceeded to the model parameterization using the ArcGIS interface for SWAT which provides a graphical support for the disaggregation scheme and this way facilitates the data handling.

In order to model the water flow accurately it is important to include the channel bathymetry in the model as well as the objects that affect the direction and velocity of water flow in the over bank situation such as buildings, bridges etc. (Mandlburger et al. 2009). After the cleaning of the data the mesh procedure can be performed using all the points’ clouds. A 3D mesh was created in the 3D Reshaper software. Estimating Flash Flood Discharge in a Catchment Area 13 Fig. 4 Preliminary result of the DEM output in the downstream with the use of only the elevation data derived from the GPS survey 4 Run-off Model Description The runoff process is modeled using the Hydrologic Engineering Center’s Hydrologic Modeling System (HEC-HMS).

1219 K. Scha¨fer, Y. Wang, S. Norra, R. Shen, J. Xin, H. Ling, G. Tang, C. Mu¨nkel, N. Schleicher, Y. Yu, J. Schnelle-Kreis, L. Shao, V. Dietze, K. Cen, R. Zimmermann, S. Schrader, and P. Suppan Monitoring Cloud Coverage in Cyprus for Solar Irradiance Prediction . . . . . . . . . . . . . . . . . . . . . . . . . . . 1227 R. G. Charalambides Carbonaceous Aerosols Over the Mediterranean and Black Sea . . . 1233 C. Theodosi, D. Smouliotis, P.

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