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Record #186983:

Spatial and temporal stability of the climatic signal in northern Fennoscandian pine tree-ring width and maximum density / Mervi Tuovinen, and 4 others.

Title: Spatial and temporal stability of the climatic signal in northern Fennoscandian pine tree-ring width and maximum density / Mervi Tuovinen, and 4 others.
Author(s): Tuovinen, Mervi.
Date: 2009.
In: Boreas. (2009.), Vol. 38(1) (2009)
Abstract: Examines spatial and temporal stability of climatic signal using pine tree-ring width and maximum density data from four sites in northern Sweden and Finland. Monthly and daily climate data indicate that ring widths at all sites have been strongly influenced by July temperatures throughout past century. Relationship between maximum temperature and density is stronger but much less stable across space and time. Concludes that palaeoclimatic reconstructions based on northern Fennoscandian pine tree-ring width chronologies should be restricted to temperature of midsummer (July), where maximum density should be used to reconstruct temperature of longer growth season (June-August).
Notes:

Boreas. Vol. 38(1) :1-12 (2009).

Keywords: 551.583 -- Climatic changes.
551.583.3 -- Climatic changes, Quaternary.
551.586 -- Climatology, biological aspects.
551.79 -- Quaternary.
574 -- Ecology.
56 -- Palaeontology.
634.0.561.24 -- Dendrochronology.
582.475 -- Pinaceae.
D -- Atmospheric sciences.
(*3) -- Arctic regions.
(*548) -- Scandinavia.
(*56) -- Finland.
(*57) -- Sweden.
SPRI record no.: 186983

MARCXML

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100 1# ‡aTuovinen, Mervi.
245 10 ‡aSpatial and temporal stability of the climatic signal in northern Fennoscandian pine tree-ring width and maximum density /‡cMervi Tuovinen, and 4 others.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2009.
300 ## ‡ap. 1-12 :‡bill., diags., tables.
500 ## ‡aBoreas. Vol. 38(1) :1-12 (2009).
520 3# ‡aExamines spatial and temporal stability of climatic signal using pine tree-ring width and maximum density data from four sites in northern Sweden and Finland. Monthly and daily climate data indicate that ring widths at all sites have been strongly influenced by July temperatures throughout past century. Relationship between maximum temperature and density is stronger but much less stable across space and time. Concludes that palaeoclimatic reconstructions based on northern Fennoscandian pine tree-ring width chronologies should be restricted to temperature of midsummer (July), where maximum density should be used to reconstruct temperature of longer growth season (June-August).
530 ## ‡aAlso issued online ‡uurn:doi:10.1111/j.1502-3885.2008.00046.x‡uhttps://dx.doi.org/10.1111/j.1502-3885.2008.00046.x
650 07 ‡a551.583 -- Climatic changes.‡2udc
650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc
650 07 ‡a551.586 -- Climatology, biological aspects.‡2udc
650 07 ‡a551.79 -- Quaternary.‡2udc
650 07 ‡a574 -- Ecology.‡2udc
650 07 ‡a56 -- Palaeontology.‡2udc
650 07 ‡a634.0.561.24 -- Dendrochronology.‡2udc
650 07 ‡a582.475 -- Pinaceae.‡2udc
650 07 ‡aD -- Atmospheric sciences.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*548) -- Scandinavia.‡2udc
651 #7 ‡a(*56) -- Finland.‡2udc
651 #7 ‡a(*57) -- Sweden.‡2udc
773 0# ‡7nnas ‡tBoreas. ‡gVol. 38(1) (2009) ‡wSPRI-56035
916 ## ‡a2009/04/09 -- JW
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221005 ‡bJW