2009
DOI: 10.2495/rav090131
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Wind and wave storms, storm surges and sea level rise along the Estonian coast of the Baltic Sea

Abstract: Winter changes in atmospheric circulation above Northern Europe are among the most prominent regional manifestations of global climate change. Particularly vulnerable are the coastal regions along the so-called North Atlantic storm track, along which these changes threaten shipping, infrastructure and human lives. The aim of this paper is to present an overview of storm climatology over the Baltic Sea and to investigate the effects of changes in wind climate on the hydrodynamic regime in the almost tideless fe… Show more

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Cited by 12 publications
(16 citation statements)
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References 7 publications
(15 reference statements)
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“…The most rapid changes in Osmussaar have occurred either during exceptionally strong storms or in periods of increased cyclonic and wave activity, the last high phase of which occurred in 1980s-1990s (Fig. 5) [3,15]. Map analyses indicate that the processes were twice as rapid during 1982-1998 than in other periods (Figs.…”
Section: Coastal Developments In Relation To Long-term Changes In Wavmentioning
confidence: 95%
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“…The most rapid changes in Osmussaar have occurred either during exceptionally strong storms or in periods of increased cyclonic and wave activity, the last high phase of which occurred in 1980s-1990s (Fig. 5) [3,15]. Map analyses indicate that the processes were twice as rapid during 1982-1998 than in other periods (Figs.…”
Section: Coastal Developments In Relation To Long-term Changes In Wavmentioning
confidence: 95%
“…However, the share of erosion never exceeded a third of the total changes during the analysed periods. Due to sea level rise and increased storminess [11,14,15], very few sandy beaches in the world are still accumulative, and we can conclude that exposure to the prevailing storm winds allows the sandy shores in Keibu Bay to belong among those few accumulation dominated shores.…”
Section: Coastal Developments In Relation To Long-term Changes In Wavmentioning
confidence: 99%
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“…Tide gauge operation, and the processing, distribution and archiving of the data are the responsibility of a single national agency per country, for instance the Swedish Meteorological and Hydrographical Institute (SMHI), the Danish Meteorological Institute (DMI), the Estonian Meteorological and Hydrographical Institute (EMHI), the Finnish Barbosa et al (2008) Baltic Sea basin wide Omstedt and Nyberg (1991), Heyen et al (1996), Carlsson (1997Carlsson ( , 1998aCarlsson ( , 1998b, Liebsch (1997), Janssen (2002), Baerens et al (2003), Meier et al (2004), Novotny et al (2006), Hünicke and Zorita (2006, 2007, 2008, Barbosa (2008), , Ekman (2009) and references therein; Hünicke (2010), Donner et al (2012) Southern Baltic Sea coast Richter et al (2007Richter et al ( , 2011 Lithuania Dailidienė et al (2004Dailidienė et al ( , 2005Dailidienė et al ( , 2006Dailidienė et al ( , 2011Dailidienė et al ( , 2012, Jarmalavicius et al (2007) Russia Bogdanov et al (2000), Averkiev and Klevannyy (2010), Navrotskaya and Chubarenko (2012) Estonia Suursaar et al (2002Suursaar et al ( , 2006aSuursaar et al ( , 2010, Kullas (2006, 2009b), Suursaar and Sooäär (2007), Suursaar (2010), Tõnisson et al (2011) Poland Zawadzka (2005, 2008), Richter et al (2007…”
Section: Tide Gaugesmentioning
confidence: 99%
“…Global, including Baltic Sea (observations from ships) No Gulev et al (2003) 1970No Gulev et al (2005 Danish waters (Drogden, multiple locations of lightships) 1931-1994-Sparre (1982 Swedish waters (multiple locations and lightships) 1965-1972No Wahl (1974 Lithuanian waters ( 1978-1996No Blomgren et al (2001 Entrance to Warnemünde harbour 1956-1993(single storms) 1988-1993No Gayer et al (1995 Pomeranian Bay No Paplińska (1999 Suursaar (2010Suursaar ( , 2013, Suursaar et al (2010Suursaar et al ( , 2012 …”
Section: Visual Observationsmentioning
confidence: 99%