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Associations between the thermal spring timing variability and atmospheric teleconnection patterns over the past six decades in Finland

Kaboli, Sadegh ; Kankare, Ville ; Haghighi, Ali Torabi ; Uvo, Cintia Bertacchi LU orcid and Kasvi, Elina (2026) In Atmospheric Research 334.
Abstract

The timing of the spring season in the boreal region is shifting under global warming, with profound impacts on ecosystems and hydrological processes. However, the mechanisms driving this transition and its considerable interannual variability are not well described, especially regarding the influence of large-scale atmospheric teleconnection patterns. This study examines the temporal variability of the observed thermal spring season across Finland, a boreal country warming faster than the global average. Key spring timing indices, including onset, end, duration, and growing season onset, were calculated and analyzed using high-resolution (1 km × 1 km) daily mean temperature data from 1961 to 2023. Spatial and temporal patterns were... (More)

The timing of the spring season in the boreal region is shifting under global warming, with profound impacts on ecosystems and hydrological processes. However, the mechanisms driving this transition and its considerable interannual variability are not well described, especially regarding the influence of large-scale atmospheric teleconnection patterns. This study examines the temporal variability of the observed thermal spring season across Finland, a boreal country warming faster than the global average. Key spring timing indices, including onset, end, duration, and growing season onset, were calculated and analyzed using high-resolution (1 km × 1 km) daily mean temperature data from 1961 to 2023. Spatial and temporal patterns were identified through Empirical Orthogonal Function (EOF) decomposition, and their associations with major atmospheric teleconnection patterns were examined. Results indicated that during the past six decades, the spring onset has advanced by 2–6 days/decade, with the most pronounced changes in the coastal and southwestern parts of the country. The duration of the spring season has extended by 3–6 days/decade in the northern areas and along the southwestern coast. The early spring onset was associated with a strong positive phase of the Arctic Oscillation (AO), and delayed spring end and growing season onset were linked to the positive phase of the East Atlantic–West Russia (EAWR) pattern. By contrast, an early growing season start was linked to the positive phase of the North Atlantic Oscillation (NAO). The duration of the thermal spring season showed a strong association with the Scandinavian (SCA) pattern.

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author
; ; ; and
organization
publishing date
type
Contribution to journal
publication status
published
subject
keywords
Atmospheric teleconnection patterns, Boreal regions, Finland, Global warming, Thermal seasons
in
Atmospheric Research
volume
334
article number
108752
pages
14 pages
publisher
Elsevier
external identifiers
  • scopus:105027104335
ISSN
0169-8095
DOI
10.1016/j.atmosres.2026.108752
language
English
LU publication?
yes
additional info
Publisher Copyright: © 2026 The Authors
id
fc6efb77-5f3e-4270-be28-4e6a12eeedd5
date added to LUP
2026-01-22 14:24:23
date last changed
2026-01-29 12:49:32
@article{fc6efb77-5f3e-4270-be28-4e6a12eeedd5,
  abstract     = {{<p>The timing of the spring season in the boreal region is shifting under global warming, with profound impacts on ecosystems and hydrological processes. However, the mechanisms driving this transition and its considerable interannual variability are not well described, especially regarding the influence of large-scale atmospheric teleconnection patterns. This study examines the temporal variability of the observed thermal spring season across Finland, a boreal country warming faster than the global average. Key spring timing indices, including onset, end, duration, and growing season onset, were calculated and analyzed using high-resolution (1 km × 1 km) daily mean temperature data from 1961 to 2023. Spatial and temporal patterns were identified through Empirical Orthogonal Function (EOF) decomposition, and their associations with major atmospheric teleconnection patterns were examined. Results indicated that during the past six decades, the spring onset has advanced by 2–6 days/decade, with the most pronounced changes in the coastal and southwestern parts of the country. The duration of the spring season has extended by 3–6 days/decade in the northern areas and along the southwestern coast. The early spring onset was associated with a strong positive phase of the Arctic Oscillation (AO), and delayed spring end and growing season onset were linked to the positive phase of the East Atlantic–West Russia (EAWR) pattern. By contrast, an early growing season start was linked to the positive phase of the North Atlantic Oscillation (NAO). The duration of the thermal spring season showed a strong association with the Scandinavian (SCA) pattern.</p>}},
  author       = {{Kaboli, Sadegh and Kankare, Ville and Haghighi, Ali Torabi and Uvo, Cintia Bertacchi and Kasvi, Elina}},
  issn         = {{0169-8095}},
  keywords     = {{Atmospheric teleconnection patterns; Boreal regions; Finland; Global warming; Thermal seasons}},
  language     = {{eng}},
  month        = {{04}},
  publisher    = {{Elsevier}},
  series       = {{Atmospheric Research}},
  title        = {{Associations between the thermal spring timing variability and atmospheric teleconnection patterns over the past six decades in Finland}},
  url          = {{http://dx.doi.org/10.1016/j.atmosres.2026.108752}},
  doi          = {{10.1016/j.atmosres.2026.108752}},
  volume       = {{334}},
  year         = {{2026}},
}