Pregled bibliografske jedinice broj: 873123
Near-surface wind pattern in regional climate projections over the broader Adriatic region
Near-surface wind pattern in regional climate projections over the broader Adriatic region // EGU General Assembly 2017
Beč, Austrija, 2017. (poster, međunarodna recenzija, sažetak, znanstveni)
CROSBI ID: 873123 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Near-surface wind pattern in regional climate projections over the broader Adriatic region
Autori
Belušić, Andreina ; Telišman Prtenjak, Maja ; Güttler, Ivan ; Ban, Nikolina ; Leutwyler, David ; Schär, Christoph
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Skup
EGU General Assembly 2017
Mjesto i datum
Beč, Austrija, 24.05.2017. - 28.05.2017
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Adriatic region ; CORDEX ; convection-resolving models ; climate projections
Sažetak
The Adriatic region is characterized by the complex coastline, strong topographic gradients and specific wind regimes. This represents excellent test area for the latest generation of the regional climate models (RCMs) applied over the European domain. The most famous wind along the Adriatic coast is bora, which due to its strength, has a strong impact on all types of human activities in the Adriatic region. The typical bora wind is a severe gusty downslope flow perpendicular to the mountains. Besides bora, in the Adriatic region, typical winds are sirocco (mostly during the wintertime) and sea/land breezes (dominantly in the warm part of the year) as a part of the regional Mediterranean wind system. Thus, it is substantial to determine future changes in the wind filed characteristics (e.g., changes in strength and frequencies). The first step was the evaluation of a suite of ten EURO- and MED-CORDEX models (at 50 km and 12.5 km resolution), and two additional high resolution models from the Swiss Federal Institute of Technology in Zürich (ETHZ, at 12.5 km and 2.2. km resolution) in the present climate. These results provided a basis for the next step where wind field features, in an ensemble of RCMs forced by global climate models (GCMs) in historical and future runs are examined. Our aim is to determine the influence of the particular combination of RCMs and GCMs, horizontal resolution and emission scenario on the future changes in the near-surface wind field. The analysis reveals strong sensitivity of the simulated wind flow and its statistics to both season and location analyzed, to the horizontal resolution of the RCM and on the choice of the particular GCM that provides boundary conditions.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb