Climatic Study of the Marine Surface Wind Field over the Greek Seas with the Use of a High Resolution RCM Focusing on Extreme Winds

The marine surface wind field (10 m) over the Greek seas is analyzed in this study using The RegCM. The model’s spatial resolution is dynamically downscaled to 10 km × 10 km, in order to simulate more efficiently the complex coastlines and the numerous islands of Greece. Wind data for the 1980–2000...

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Main Authors: Christos Vagenas, Christina Anagnostopoulou, Konstantia Tolika
Format: Article
Language:English
Published: MDPI AG 2017-03-01
Series:Climate
Subjects:
Online Access:http://www.mdpi.com/2225-1154/5/2/29
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spelling doaj-3987ae47e18644cdbd3f1dc0ac1a3d3e2020-11-24T23:24:41ZengMDPI AGClimate2225-11542017-03-01522910.3390/cli5020029cli5020029Climatic Study of the Marine Surface Wind Field over the Greek Seas with the Use of a High Resolution RCM Focusing on Extreme WindsChristos Vagenas0Christina Anagnostopoulou1Konstantia Tolika2Institute of Meteorology, Freie Universität Berlin, Berlin 14195, GermanyDepartment of Meteorology and Climatology, School of Geology, Faculty of Sciences, Aristotle University of Thessaloniki, Thessaloniki 54124, GreeceDepartment of Meteorology and Climatology, School of Geology, Faculty of Sciences, Aristotle University of Thessaloniki, Thessaloniki 54124, GreeceThe marine surface wind field (10 m) over the Greek seas is analyzed in this study using The RegCM. The model’s spatial resolution is dynamically downscaled to 10 km × 10 km, in order to simulate more efficiently the complex coastlines and the numerous islands of Greece. Wind data for the 1980–2000 and 2080–2100 periods are produced and evaluated against real observational data from 15 island and coastal meteorological stations in order to assess the model’s ability to reproduce the main characteristics of the surface wind fields. RegCM model shows a higher simulating skill to project seasonal wind speeds and direction during summer and the lowest simulating skill in the cold period of the year. Extreme wind speed thresholds were estimated using percentiles indices and three Peak Over Threshold (POT) techniques. The mean threshold values of the three POT methods are used to examine the inter-annual distribution of extreme winds in the study region. The highest thresholds were observed in three poles; the northeast, the southeast, and the southwest of Aegean Sea. Future changes in extreme speeds show a general increase in the Aegean Sea, while lower thresholds are expected in the Ionian Sea. Return levels for periods of 20, 50, 100, and 200 years are estimated.http://www.mdpi.com/2225-1154/5/2/29Peak Over Threshold (POT) techniqueRegCMAegean and Ioanian seasextreme wind speedreturn periods
collection DOAJ
language English
format Article
sources DOAJ
author Christos Vagenas
Christina Anagnostopoulou
Konstantia Tolika
spellingShingle Christos Vagenas
Christina Anagnostopoulou
Konstantia Tolika
Climatic Study of the Marine Surface Wind Field over the Greek Seas with the Use of a High Resolution RCM Focusing on Extreme Winds
Climate
Peak Over Threshold (POT) technique
RegCM
Aegean and Ioanian seas
extreme wind speed
return periods
author_facet Christos Vagenas
Christina Anagnostopoulou
Konstantia Tolika
author_sort Christos Vagenas
title Climatic Study of the Marine Surface Wind Field over the Greek Seas with the Use of a High Resolution RCM Focusing on Extreme Winds
title_short Climatic Study of the Marine Surface Wind Field over the Greek Seas with the Use of a High Resolution RCM Focusing on Extreme Winds
title_full Climatic Study of the Marine Surface Wind Field over the Greek Seas with the Use of a High Resolution RCM Focusing on Extreme Winds
title_fullStr Climatic Study of the Marine Surface Wind Field over the Greek Seas with the Use of a High Resolution RCM Focusing on Extreme Winds
title_full_unstemmed Climatic Study of the Marine Surface Wind Field over the Greek Seas with the Use of a High Resolution RCM Focusing on Extreme Winds
title_sort climatic study of the marine surface wind field over the greek seas with the use of a high resolution rcm focusing on extreme winds
publisher MDPI AG
series Climate
issn 2225-1154
publishDate 2017-03-01
description The marine surface wind field (10 m) over the Greek seas is analyzed in this study using The RegCM. The model’s spatial resolution is dynamically downscaled to 10 km × 10 km, in order to simulate more efficiently the complex coastlines and the numerous islands of Greece. Wind data for the 1980–2000 and 2080–2100 periods are produced and evaluated against real observational data from 15 island and coastal meteorological stations in order to assess the model’s ability to reproduce the main characteristics of the surface wind fields. RegCM model shows a higher simulating skill to project seasonal wind speeds and direction during summer and the lowest simulating skill in the cold period of the year. Extreme wind speed thresholds were estimated using percentiles indices and three Peak Over Threshold (POT) techniques. The mean threshold values of the three POT methods are used to examine the inter-annual distribution of extreme winds in the study region. The highest thresholds were observed in three poles; the northeast, the southeast, and the southwest of Aegean Sea. Future changes in extreme speeds show a general increase in the Aegean Sea, while lower thresholds are expected in the Ionian Sea. Return levels for periods of 20, 50, 100, and 200 years are estimated.
topic Peak Over Threshold (POT) technique
RegCM
Aegean and Ioanian seas
extreme wind speed
return periods
url http://www.mdpi.com/2225-1154/5/2/29
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