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  • 1
    Call number: 9783319350950 (e-book)
    Description / Table of Contents: This book provides the proceedings of the 13th International Conference of Meteorology, Climatology and Atmospheric Physics (COMECAP 2016) that is held in Thessaloniki from 19 to 21 September 2016. The Conference addresses fields of interest for researchers, professionals and students related to the following topics: Agricultural Meteorology and Climatology, Air Quality (Indoor and Outdoor), Applied Meteorology and Climatology, Applications of Meteorology in the Energy sector, Atmospheric Physics and Chemistry, Atmospheric Radiation, Atmospheric Boundary layer, Biometeorology and Bioclimatology, Climate Dynamics, Climatic Changes, Cloud Physics, Dynamic and Synoptic Μeteorology, Extreme Events, Hydrology and Hydrometeorology, Mesoscale Meteorology, Micrometeorology-Urban Microclimate, Remote Sensing- Satellite Meteorology and Climatology, Weather Analysis and Forecasting. The book includes all papers that have been accepted after peer review for presentation in the conference
    Type of Medium: 12
    Pages: 1 Online-Ressource (XXXI, 1259 Seiten) , Illustrationen
    ISBN: 9783319350950 , 978-3-319-35095-0
    ISSN: 2194-5217 , 2194-5225
    Series Statement: Springer atmospheric sciences
    Language: English
    Note: Contents Part I Meteorology The Influence of WRF Parameterisation Schemes on High Resolution Simulations Over Greece / I. Tegoulias, S. Kartsios, I. Pytharoulis, S. Kotsopoulos and Theodore S. Karacostas Assessing the Sensitivity of COSMO/GR Atmospheric Model to Effectively Simulate the Influence of Diabatic Heating on Eastern Mediterranean Explosive Cyclogenesis Under Different Parameterizations of the Model Physics / J. Kouroutzoglou, E. Avgoustoglou, H.A. Flocas, M. Hatzaki, P. Skrimizeas, A. Lalos, K. Keay and I. Simmonds Evaluation of WRF Parameterization Schemes During Heat-Wave Events Over the Greater Area of South–East Mediterranean / C. Giannaros, D. Melas and T.M. Giannaros A Study of an Extreme Hot Weather Event in Greece with the WRF-ARW Atmospheric Model / G. Emmanouil, D. Vlachogiannis, A. Sfetsos, S. Karozis and A. Tasopoulou Lightning Forecasting in Europe: Results Obtained from One Year of Operational Simulations / T.M. Giannaros, V. Kotroni and K. Lagouvardos Numerical Simulations and Observational Study of a Mesoscale Convective System in France, During the HyMeX—SOP1 Using the WRF Model /1 S. Dafis, K. Lagouvardos, V. Kotroni, T.M. Giannaros and A. Bartzokas Design and Evaluation of Sensitivity Tests of COSMO Model Over the Mediterranean Area / E. Avgoustoglou, A. Voudouri, P. Khain, F. Grazzini and J.M. Bettems Comparison and Validation of WRF Model Physics Parameterizations Over the Domain of Greece / N. Politi, P.T. Nastos, A. Sfetsos, D. Vlachogiannis, N.R. Dalezios, N. Gounaris, M.R. Cardoso and M.M.P. Soares Severe Weather Events and Sea Level Variability Over the Mediterranean Sea: The WaveForUs Operational Platform / Y. Krestenitis, I. Pytharoulis, Theodore S. Karacostas, Y. Androulidakis, C. Makris, K. Kombiadou, I. Tegoulias, V. Baltikas, S. Kotsopoulos and S. Kartsios The Implementation of a Dust Wet Deposition Scheme in the WRF-CHEM Model / K. Tsarpalis, A. Papadopoulos and P. Katsafados Temperature Seasonal Predictability of the WRF Model / G. Varlas, P. Katsafados and A. Papadopoulos Numerical Modeling of a Tornado Event at Skala, Lakonia, Peloponnese in September 2015 / M.P. Mylonas, P.T. Nastos and Ioannis T. Matsangouras Towards Predictability Limit: Advancing the Deterministic Skill of Ensembles / I. Kioutsioukis Marine Boundary Layer Offshore and Coastal Coupled Simulations / C. Stathopoulos, G. Galanis and G. Kallos Observational and Numerical Study of a Tornado Outbreak in Attica and Euboea / A. Lampiris, S. Dafis and G. Papavasileiou The Effect of Surface Heterogeneity on the Vertical Structure of the Saharan Convective Boundary Layer / G. Papangelis, M. Tombrou and J. Kalogiros Numerical Study of the Medicane of November 2014 / I. Pytharoulis, Ioannis T. Matsangouras, I. Tegoulias, S. Kotsopoulos, Theodore S. Karacostas and P.T. Nastos Numerical Modeling Analysis of Tornadoes Using the COSMO.GR Model Over Greece / Ioannis T. Matsangouras, E. Avgoustoglou, F. Gofa, I. Pytharoulis, P.T. Nastos and H.W. Bluestein Performance of RegCM4 Model During Heat Waves—A Case Study for China / D.K. Papanastasiou, X. Huang, A. Poupkou, X. Pu, P. Zanis, T. Wang and D. Melas The Role of Heat Extinction Depth Concept to Fire Behavior: An Application to WRF-SFIRE Model / S. Kartsios, Theodore S. Karacostas, I. Pytharoulis and A.P. Dimitrakopoulos Impacts of Observational Data Assimilation on Operational Forecasts / A. Voudouri, E. Avgoustoglou and P. Kaufmann Comparative Forecasts of a Local Area Model (WRF) in Summer for Cyprus / F. Tymvios, D. Charalambous, J. Lelieveld and S. Michaelides Implementation of a Hybrid Surface Layer Parameterization Scheme for the Coupled Atmosphere-Ocean Wave System WEW / P. Katsafados, G. Varlas, A. Papadopoulos and G. Korres Development and Implementation of a Soil Moisture Perturbation Method for EPS Initial Conditions / P. Louka, F. Gofa, C. Marsigli and A. Montani The Impact of Cyclone Xaver on Hydropower Potential in Norway . . . 175 I. Cheliotis, G. Varlas and K. Christakos Heavy Convective Rainfall Forecast Over Paraguay Using Coupled WRF-Cloud Model / V. Spiridonov, J. Baez and B. Telenta The Heat Health Warning System of DWD—Concept and Lessons Learned / A. Matzarakis Impact of Storm Seeding to Hailstone Features in Central Macedonia / D. Foris and V. Foris Validating SAF NWC Products Over the Greek Area / A. Karagiannidis, K. Lagouvardos, V. Kotroni and T.M. Giannaros Use of Global Precipitation Measurement’s Satellite Data for the Study of a Mesoscale Convective System /D. Mitropoulos and H. Feidas Flash Flood Risk and Vulnerability Analysis in Urban Areas: The Case of October 22, 2015, in Attica, Greece / K. Papagiannaki, V. Kotroni, K. Lagouvardos and A. Bezes The First Joint Hydro-Meteo Warnings in Croatia During Heavy Rainfall Period in October 2015 / P. Mutic, T. Jurlina, T. Vujnovic, D. Oskorus, N. Strelec-Mahovic and T. Renko A Total Weighted Least Squares Method for the Determination of the Meteoric Water Line of Precipitation for Hydrological Purposes / A.A. Argiriou, V. Salamalikis and E. Dotsika Storm Characteristics Over Central Macedonia and Thessaly and Their Relation to Atmospheric Parameters / E. Chatzi Radar Climatology of Supercell Thunderstorms in Northern and Central Greece / M. Christodoulou and M. Sioutas Comparison of Physically and Image Based Atmospheric Correction Methods for Sentinel-2 Satellite Imagery / G. Lantzanakis, Z. Mitraka and N. Chrysoulakis First Rains as Extreme Events Influencing Marine Primary Production / D. Kotta, D. Kitsiou and P. Kassomenos Hail Characteristics and Cloud Seeding Effect for Hail Suppression in Central Macedonia, Greece / M. Sioutas Satellite Rainfall Error Analysis with the Use of High-Resolution X-Band Dual-Polarization Radar Observations Over the Italian Alps / M.N. Anagnostou, J. Kalogiros, E. Nikolopoulos, Y. Derin, E.N. Anagnostou and M. Borga The DAPHNE Conceptual Model for Designing a Precipitation Enhancement Project in Thessaly, Greece / Theodore S. Karacostas, I. Pytharoulis, I. Tegoulias, D. Bampzelis, S. Kartsios, S. Kotsopoulos, P. Zanis, E. Katragkou and K. Tympanidis Watershed Size, an Alternative or a Misguided Parameter for River’s Waterpower? Implementation in Macedonia, Greece / G. Grimpylakos, K. Albanakis and Theodore S. Karacostas Survey of the Severe Hailstorms During Summer 2014 in the Northern Part of Greece / P. Fragkouli, A. Tyraski and K. Lagouvardos Assessment of the Thermal Comfort Conditions in a University Campus Using a 3D Microscale Climate Model, Utilizing Mobile Measurements / P.T. Nastos, K.P. Moustris, I. Charalampopoulos, I.K. Larissi and Athanasios G. Paliatsos Diurnal Distribution of Storm Characteristics in Central Macedonia During the Warm Season of the Year Using a C-Band Weather Radar / D. Bampzelis and Theodore S. Karacostas Rain Enhancement Feasibility Potential of Orographic Clouds Over Northern Greece / K. Tympanidis, Theodore S. Karacostas and D. Bampzelis A Preliminary Study on the Effect of Rainfall Events on Human Thermal Comfort Under Hot Weather Conditions / I. Charalampopoulos and I. Tsiros One Day-Ahead Prognosis of Energy Demand Using Artificial Intelligence and Biometeorological Indices / D. Zafirakis, K.P. Moustris, D.H. Alamo and R.J. Nebot Medina The Effect of Rainfall Intensity on the Flood Generation of Mountainous Watersheds (Chalkidiki Prefecture, North Greece) / A. Kastridis and D. Stathis Air Temperature Estimation Over the Ainos Mountain, Kefallinia Island Using Linear Regression Analysis / S. Maniatis, A. Kamoutsis, A. Chronopoulou-Sereli and P.T. Nastos Dust Over the Area of the East Mediterranean: The Severe Dust Event of the Period 7–12 September 2015. Synoptic and Dynamic Analysis / K. Nicolaides and F. Tymvios On the Dynamics Underlying the Emergence of Coherent Structures in Barotropic Turbulence / N.A. Bakas, N.C. Constantinou and P.J. Ioannou Structure and Stability of Low Amplitude Jet Equilibria in Barotropic Turbulence / N.C. Constantinou, P.
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  • 2
    Publication Date: 2020-07-08
    Description: The UV-Index (UVI) is aimed at the prevention of skin cancer as well as other negative implications of ultraviolet radiation exposure. In order to support health related applications, assessments and planning that rely on long term data in high spatial resolution and as there exist only limited ground-based measurements, satellite products from reliable atmospheric monitoring services are used as sustainable data sources to create a climatology of the UVI at the local noon. In this study, the (all-sky) UVI as well as the hypothetically clear-sky UVI were analysed for the European region from 30° North to 65° North and from 25° West to 35° East in a spatial resolution of 0.05° for the time period 1983 to 2015. Maps of the monthly mean UVI provide an overview of the distribution of UVI for Europe as well as the spatial and temporal differences and regional variability at local solar noon. Additionally, eight selected locations provide insight into the effects of latitude and altitude on UVI in Europe. Monthly boxplots for each location provide information about regional differences in the variability of UVI, showing maximum variability in Northern and Central Europe in summer, where in Southern Europe this basically occurs in spring. The frequency of the World Health Organization exposure categories moderate, high and very high UVI is provided based on ten-day means for each month. The maximum difference between mean values per decade of 2006–2015 compared to 1983–1992 ranges from −1.2 to +1.2 for UVI and from −0.4 to +0.6 for UVI c l e a r − s k y . All locations, except the Northern European site, show an increase of UVI during spring and early summer months. A statistically significant increase in the annual mean all-sky UVI has been found for four sites, which ranges from +1.2% to +3.6% per decade. The latest eleven-year period of the UVI climatology (2005–2015) has been validated with UVI measured in five sites. The sites that are located north of the Alps show an underestimation of the UVI, likely due to the cloud modification. In the south, the UVI climatology provides values that are on average overestimated, possibly related to the use of climatological aerosol information. For the site within the Alps, a switch between underestimation and overestimation during the course of the year has been found. 7% to 9% of the UVI values of the climatology differ from the measured UVI by more than one unit.
    Electronic ISSN: 2073-4433
    Topics: Geosciences
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  • 3
    Publication Date: 2016-02-01
    Print ISSN: 0960-1481
    Electronic ISSN: 1879-0682
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Published by Elsevier
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    Publication Date: 2016-09-01
    Print ISSN: 1352-2310
    Electronic ISSN: 1873-2844
    Topics: Energy, Environment Protection, Nuclear Power Engineering , Geosciences , Physics
    Published by Elsevier
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  • 7
    Publication Date: 2018-06-01
    Print ISSN: 1352-2310
    Electronic ISSN: 1873-2844
    Topics: Energy, Environment Protection, Nuclear Power Engineering , Geosciences , Physics
    Published by Elsevier
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  • 8
    Publication Date: 2020-09-29
    Description: We present the inter-comparison of delta slant column densities (SCDs) and vertical profiles of nitrous acid (HONO) derived from measurements of different multi-axis differential optical absorption spectroscopy (MAX-DOAS) instruments and using different inversion algorithms during the Second Cabauw Inter-comparison campaign for Nitrogen Dioxide measuring Instruments (CINDI-2) in September 2016 at Cabauw, the Netherlands (51.97∘ N, 4.93∘ E). The HONO vertical profiles, vertical column densities (VCDs), and near-surface volume mixing ratios are compared between different MAX-DOAS instruments and profile inversion algorithms for the first time. Systematic and random discrepancies of the HONO results are derived from the comparisons of all data sets against their median values. Systematic discrepancies of HONO delta SCDs are observed in the range of ±0.3×1015 molec. cm−2, which is half of the typical random discrepancy of 0.6×1015 molec. cm−2. For a typical high HONO delta SCD of 2×1015 molec. cm−2, the relative systematic and random discrepancies are about 15 % and 30 %, respectively. The inter-comparison of HONO profiles shows that both systematic and random discrepancies of HONO VCDs and near-surface volume mixing ratios (VMRs) are mostly in the range of ∼±0.5×1014 molec. cm−2 and ∼±0.1 ppb (typically ∼20 %). Further we find that the discrepancies of the retrieved HONO profiles are dominated by discrepancies of the HONO delta SCDs. The profile retrievals only contribute to the discrepancies of the HONO profiles by ∼5 %. However, some data sets with substantially larger discrepancies than the typical values indicate that inappropriate implementations of profile inversion algorithms and configurations of radiative transfer models in the profile retrievals can also be an important uncertainty source. In addition, estimations of measurement uncertainties of HONO dSCDs, which can significantly impact profile retrievals using the optimal estimation method, need to consider not only DOAS fit errors, but also atmospheric variability, especially for an instrument with a DOAS fit error lower than ∼3×1014 molec. cm−2. The MAX-DOAS results during the CINDI-2 campaign indicate that the peak HONO levels (e.g. near-surface VMRs of ∼0.4 ppb) often appeared in the early morning and below 0.2 km. The near-surface VMRs retrieved from the MAX-DOAS observations are compared with those measured using a co-located long-path DOAS instrument. The systematic differences are smaller than 0.15 and 0.07 ppb during early morning and around noon, respectively. Since true HONO values at high altitudes are not known in the absence of real measurements, in order to evaluate the abilities of profile inversion algorithms to respond to different HONO profile shapes, we performed sensitivity studies using synthetic HONO delta SCDs simulated by a radiative transfer model with assumed HONO profiles. The tests indicate that the profile inversion algorithms based on the optimal estimation method with proper configurations can reproduce the different HONO profile shapes well. Therefore we conclude that the features of HONO accumulated near the surface derived from MAX-DOAS measurements are expected to represent the ambient HONO profiles well.
    Print ISSN: 1867-1381
    Electronic ISSN: 1867-8548
    Topics: Geosciences
    Published by Copernicus on behalf of European Geosciences Union.
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  • 9
    Publication Date: 1995-12-01
    Print ISSN: 1352-2310
    Electronic ISSN: 1873-2844
    Topics: Energy, Environment Protection, Nuclear Power Engineering , Geosciences , Physics
    Published by Elsevier
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  • 10
    Publication Date: 2017-07-11
    Description: This study assesses the impact of dust on surface solar radiation focussing on an extreme dust event. For this purpose, we exploited the synergy of AERONET measurements and passive and active satellite remote sensing (MODIS and CALIPSO) observations, in conjunction with radiative transfer model (RTM) and chemical transport model (CTM) simulations and the 1-day forecasts from the Copernicus Atmosphere Monitoring Service (CAMS). The area of interest is the eastern Mediterranean where anomalously high aerosol loads were recorded between 30 January and 3 February 2015. The intensity of the event was extremely high, with aerosol optical depth (AOD) reaching 3.5, and optical/microphysical properties suggesting aged dust. RTM and CTM simulations were able to quantify the extent of dust impact on surface irradiances and reveal substantial reduction in solar energy exploitation capacity of PV and CSP installations under this high aerosol load. We found that such an extreme dust event can result in Global Horizontal Irradiance (GHI) attenuation by as much as 40–50 % and a much stronger Direct Normal Irradiance (DNI) decrease (80–90 %), while spectrally this attenuation is distributed to 37 % in the UV region, 33 % in the visible and around 30 % in the infrared. CAMS forecasts provided a reliable available energy assessment (accuracy within 10 % of that obtained from MODIS). Spatially, the dust plume resulted in a zonally averaged reduction of GHI and DNI of the order of 150 W m−2 in southern Greece, and a mean increase of 20 W m−2 in the northern Greece as a result of lower AOD values combined with local atmospheric processes. This analysis of a real-world scenario contributes to the understanding and quantification of the impact range of high aerosol loads on solar energy and the potential for forecasting power generation failures at sunshine-privileged locations where solar power plants exist, are under construction or are being planned.
    Print ISSN: 1867-1381
    Electronic ISSN: 1867-8548
    Topics: Geosciences
    Published by Copernicus on behalf of European Geosciences Union.
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