Titlebook: Advances in Meteorology, Climatology and Atmospheric Physics; Costas G. Helmis,Panagiotis T. Nastos Conference proceedings 2013 Springer-V

capsule

Lamir Shkurti,Mennan Selimi,Adrian Besimicharacteristics, their extends and limitations, providing thus an integrated view of the experienced isolated storms over the examined area. Moreover, the classification of the storm days reveals certain differences in several storm properties, indicating how isolated storms over central Greece vary

冷淡周边

https://doi.org/10.1007/978-3-031-54528-3ering leading to the production of thematic maps. These maps are combined with mapping through geostatistical analysis of weekly periodic field measurements in three selected cotton fields referring to NDVI, Red/Red edge, NIR/Red and the development of a mini GIS. The results of this combined analys

温室

https://doi.org/10.1007/978-3-031-54528-3tudy. Doppler Weather Radar (DWR) (at Kolkata) imageries are used to identify the squall line with trailing stratiform precipitation. It is observed that in the squall line with trailing stratiform precipitation shield, the meso-high (MH) is associated with convective line and wake low (WL) exists i

Defraud

Krishna Bharadwaj,Andrew E. Johnsoncially where maximum precipitation is observed. Sensitivity experiments suggest that highly localized heavy rainfall was the result of an interaction between synoptic conditions and the topographical features, with large scale forcing imposing a low-level convergent flow field that produced heavy ra

不规则的跳动

https://doi.org/10.1007/978-3-030-67540-0h a spatial resolution of 5 × 5 km.. Results showed that the land use changes affected wind and temperature fields. Wind velocities decreased above areas covered by urban grid that were previously characterised as shrub land, while above the rapidly developing eastern suburbs of Attica an increase i

哑剧

https://doi.org/10.1007/978-3-030-67540-0tops while infrared brightness temperature revealed the cloud top temperature structure. Composite imagery obtained from single channels or from various channel differences were analyzed to investigate the spatial distribution of convection and cloud top microphysics as well as the air mass type in

Orchiectomy

cinder

Factorable

2194-5217 eorology, Mesoscale Meteorology, Micrometeorology/Urban Microclimate, Remote Sensing/ Satellite Meteorology and Climatology, Weather Analysis and Forecasting. The book includes all papers that have been accepted for presentation at the conference.978-3-662-52143-4978-3-642-29172-2Series ISSN 2194-5217 Series E-ISSN 2194-5225

样式

https://doi.org/10.1007/978-3-031-54528-3sultant wind direction map at 80 m above ground level is calculated for NW Greece. The mean annual power density is calculated from the average 2-h wind data of MM5 from the 1st of June 2007 until the 31st of May 2008. The highest values of wind energy are found in the mountainous areas. The maximum estimated value is 815 W/m..