Endre søk
RefereraExporteraLink to record
Permanent link

Direct link
Referera
Referensformat
  • apa
  • ieee
  • modern-language-association-8th-edition
  • vancouver
  • Annet format
Fler format
Språk
  • de-DE
  • en-GB
  • en-US
  • fi-FI
  • nn-NO
  • nn-NB
  • sv-SE
  • Annet språk
Fler språk
Utmatningsformat
  • html
  • text
  • asciidoc
  • rtf
Deuterium excess record from a small Arctic ice cap
Norwegian Polar Res Inst, Polar Environm Ctr, N-9296 Tromso, Norway..
Norwegian Polar Res Inst, Polar Environm Ctr, N-9296 Tromso, Norway..
Uppsala Univ, Dept Earth Sci, SE-75236 Uppsala, Sweden..
Univ Groningen, Ctr Isotope Res, NL-9714 AG Groningen, Netherlands..
Vise andre og tillknytning
Ansvarlig organisasjon
2008 (engelsk)Inngår i: Journal of Geophysical Research - Atmospheres, ISSN 2169-897X, E-ISSN 2169-8996, Vol. 113, nr D19, artikkel-id D19104Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

In this paper we present a deuterium excess (d) record from an ice core drilled on a small ice cap in Svalbard in 1997. The core site is located at Lomonosovfonna at 1255 m asl, and the analyzed time series spans the period 1400-1990 A. D. The record shows pronounced multidecadal to centennial-scale variations coherent with sea surface temperature changes registered in the subtropical to southern middle-latitude North Atlantic during the instrumental period. We interpret the negative trend in the deuterium excess during the 1400s and 1500s as an indication of cooling in the North Atlantic associated with the onset of the Little Ice Age. Consistently positive anomalies of d after 1900, peaking at about 1950, correspond with well-documented contemporary warming. Yet the maximum values of deuterium excess during 1900-1990 are not as high as in the early part of the record (pre-1550). This suggests that the sea surface temperatures during this earlier period of time in the North Atlantic to the south of approximately 45 degrees N were at least comparable with those registered in the 20th century before the end of the 1980s. We examine the potential for a cold bias to exist in the deuterium excess record due to increased evaporation from the local colder sources of moisture having isotopically cold signature. It is argued that despite a recent oceanic warming, the contribution from this local moisture to the Lomonosovfonna precipitation budget is still insufficient to interfere with the isotopic signal from the primary moisture region in the midlatitude North Atlantic.

sted, utgiver, år, opplag, sider
2008. Vol. 113, nr D19, artikkel-id D19104
Forskningsprogram
SWEDARCTIC
Identifikatorer
URN: urn:nbn:se:polar:diva-2428DOI: 10.1029/2008JD010076ISI: 000259803900003OAI: oai:DiVA.org:polar-2428DiVA, id: diva2:883560
Tilgjengelig fra: 2015-12-17 Laget: 2015-10-07 Sist oppdatert: 2017-12-01

Open Access i DiVA

Fulltekst mangler i DiVA

Andre lenker

Forlagets fulltekst
I samme tidsskrift
Journal of Geophysical Research - Atmospheres

Søk utenfor DiVA

GoogleGoogle Scholar

doi
urn-nbn

Altmetric

doi
urn-nbn
Totalt: 34 treff
RefereraExporteraLink to record
Permanent link

Direct link
Referera
Referensformat
  • apa
  • ieee
  • modern-language-association-8th-edition
  • vancouver
  • Annet format
Fler format
Språk
  • de-DE
  • en-GB
  • en-US
  • fi-FI
  • nn-NO
  • nn-NB
  • sv-SE
  • Annet språk
Fler språk
Utmatningsformat
  • html
  • text
  • asciidoc
  • rtf