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  • Katrantsiotis, ChristosStockholms universitet,Institutionen för naturgeografi,Navarino Environmental Observatory (NEO), Greece,Stockholm Univ, Dept Phys Geog, Stockholm, Sweden; NEO, Messenia, Greece; Stockholm Univ, Bolin Ctr Climate Res, Stockholm, Sweden (författare)

Climate changes in the Eastern Mediterranean over the last 5000 years and their links to the high-latitude atmospheric patterns and Asian monsoons

  • Artikel/kapitelEngelska2019

Förlag, utgivningsår, omfång ...

  • Elsevier BV,2019
  • printrdacarrier

Nummerbeteckningar

  • LIBRIS-ID:oai:DiVA.org:su-167739
  • https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-167739URI
  • https://doi.org/10.1016/j.gloplacha.2019.02.001DOI
  • https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-382656URI

Kompletterande språkuppgifter

  • Språk:engelska
  • Sammanfattning på:engelska

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Klassifikation

  • Ämneskategori:ref swepub-contenttype
  • Ämneskategori:art swepub-publicationtype

Anmärkningar

  • This research aims to improve the knowledge of the mid to late Holocene climate changes and the underlying drivers in the eastern Mediterranean. We focus on the Peloponnese peninsula, SW Greece, characterized by a W-E rainfall/temperature gradient and a strong climate-sensitivity to shifts in the large-scale atmospheric patterns. A radiocarbon-dated sediment core, taken from the ancient Lake Lerna, a former lake in NE Peloponnese, was analyzed for distribution and hydrogen isotope (δD) composition of n-alkanes and bulk organic geochemistry (δ13C, TOC). The predominantly macrophyte (submerged/floating)-derived δD23 profile exhibits the largest long-term fluctuation in the record and co-varies with δD of long-chain n-alkanes providing evidence for precipitation and temperature changes over the last 5000 years. The Lerna δD23 signal is sometimes in agreement with other n-alkane δD records from SW Peloponnese indicating wetter conditions in the peninsula at ca 5000–4600, ca 4500–4100, ca 3000–2600 (more unstable in SW) and after ca 700 cal BP with drier periods at ca 4100–3900 and ca 1000–700 cal BP. Conversely, a NE-SW climate see-saw is revealed at ca 4600–4500, ca 3200, ca 2600–1800, and ca 1200–1000 cal BP when the δD23 Lerna exhibits more positive trends (drier in NE) with a reversal at ca 3900–3300, ca 3200–3000 and ca 1800–1300 cal BP. These opposing and sometimes similar signals between NE and SW Peloponnese can be explained by the relative dominance of high-latitude atmospheric patterns over the peninsula. A similar signal would be expected when the North Atlantic Oscillation (NAO) exerts the main control with NAO (+) creating conditions of reduced moisture. The dipole pattern is likely driven by shifts in North Sea–Caspian Atmospheric pattern (NCP), which account for the present-day regional climate variability with NCP (+) leading to wetter and colder conditions in NE Peloponnese. The Asian monsoonal system likely has an additional impact on the δD variabilities through influencing the summer temperatures. There is a consistency between the Peloponnesian δD signals and monsoonal records after ca 4000 cal BP confirming the actualistic models. Strong monsoonal periods coincide with cooler summers (lower δD values) in Lerna, due to the northerly winds, the Etesians. On the contrary, SW Peloponnese is dominated by warmer conditions during the same periods as the area is located on the lee side of the mountain and highly influenced by the adiabatic warming associated with the subsidence over the Eastern Mediterranean.

Ämnesord och genrebeteckningar

Biuppslag (personer, institutioner, konferenser, titlar ...)

  • Norström, ElinStockholms universitet,Institutionen för geologiska vetenskaper,Navarino Environmental Observatory (NEO), Greece,NEO, Messenia, Greece; Stockholm Univ, Bolin Ctr Climate Res, Stockholm, Sweden; Stockholm Univ, Dept Geol Sci, Stockholm, Sweden(Swepub:su)norst (författare)
  • Smittenberg, Rienk H.Stockholms universitet,Institutionen för geologiska vetenskaper,Stockholm Univ, Bolin Ctr Climate Res, Stockholm, Sweden; Stockholm Univ, Dept Geol Sci, Stockholm, Sweden(Swepub:su)rsmit (författare)
  • Finné, MartinUppsala universitet,Antikens kultur och samhällsliv(Swepub:uu)marfi619 (författare)
  • Weiberg, Erika,1971-Uppsala universitet,Antikens kultur och samhällsliv(Swepub:uu)erwei030 (författare)
  • Hättestrand, MartinaStockholms universitet,Institutionen för naturgeografi,Navarino Environmental Observatory (NEO), Greece,Stockholm Univ, Dept Phys Geog, Stockholm, Sweden; NEO, Messenia, Greece; Stockholm Univ, Bolin Ctr Climate Res, Stockholm, Sweden(Swepub:su)hatte (författare)
  • Avramidis, PavlosUniv Patras, Dept Geol, Rion, Greece (författare)
  • Wastegård, StefanStockholms universitet,Institutionen för naturgeografi,Stockholm Univ, Dept Phys Geog, Stockholm, Sweden; Stockholm Univ, Bolin Ctr Climate Res, Stockholm, Sweden(Swepub:su)waste (författare)
  • Stockholms universitetInstitutionen för naturgeografi (creator_code:org_t)

Sammanhörande titlar

  • Ingår i:Global and Planetary Change: Elsevier BV175, s. 36-510921-81811872-6364

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