2016
DOI: 10.1007/978-3-319-35095-0_40
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The DAPHNE Conceptual Model for Designing a Precipitation Enhancement Project in Thessaly, Greece

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Cited by 2 publications
(5 citation statements)
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“…To understand the main mechanisms driving the long-range transport of volcanic aerosol over the Mediterranean during the event, we examined the major atmospheric processes taking place in the area on a synoptic scale, as resolved by the WRF-ARW model [50]. This transport episode is associated with a closed long wave trough [91][92][93] affecting the North Italy on the isobaric level of 500 hPa. The modeled geopotential height at 500 hPa at 02:00 UTC, 30 May 2019, (which is around the starting time of the eruption) shows a low-height center (at 5600 gpm) located Northeast of Italy (Figure 3a).…”
Section: Transport Of So 2 and Volcanic Ashmentioning
confidence: 99%
“…To understand the main mechanisms driving the long-range transport of volcanic aerosol over the Mediterranean during the event, we examined the major atmospheric processes taking place in the area on a synoptic scale, as resolved by the WRF-ARW model [50]. This transport episode is associated with a closed long wave trough [91][92][93] affecting the North Italy on the isobaric level of 500 hPa. The modeled geopotential height at 500 hPa at 02:00 UTC, 30 May 2019, (which is around the starting time of the eruption) shows a low-height center (at 5600 gpm) located Northeast of Italy (Figure 3a).…”
Section: Transport Of So 2 and Volcanic Ashmentioning
confidence: 99%
“…The main aim of the current study is to evaluate the performance of the Weather Research and Forecasting (WRF) numerical model and propose the best combination of its parameterizations, which should be used for the forecast of convective events that shall take place in the area of Thessaly, in central Greece. This study was part of the research project named "DAPHNE" aiming to tackle the problem of drought in this area, by examining the possibility of a rain enhancing program through Weather Modification (Karacostas et al, 2015). The scheduling of the flights would require an a priori good knowledge of the possibility of convective activity in the area.…”
Section: Aim -Objectivesmentioning
confidence: 99%
“…A large number of scientific contributions have been produced during those years by members of the Department (Bampzelis et al, 2015;Karacostas et al, 2018;Kartsios et al, 2017Kartsios et al, , 2015Kartsios et al, , 2014bKartsios et al, , 2014aKatragkou et al, 2015;Krestenitis et al, 2017;Pytharoulis et al, 2015aPytharoulis et al, , 2015bPytharoulis et al, , 2014aPytharoulis et al, , 2018Pytharoulis et al, , 2016Stolaki et al, 2012;Tegoulias et al, 2017Tegoulias et al, , 2014aTegoulias et al, , 2014b The WRF Model -Overview and parameterizations used 9 2.2 The ARW Dynamics Solver…”
Section: The Dynamic Solvers Together With the Physics Packages Interfacing With Thementioning
confidence: 99%
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