Temperature patterns over the past eight centuries in Northern Fennoscandia inferred from sedimentary diatoms
Dados Bibliográficos
| ID | 24085849 |
|---|---|
| Autores | Jan Weckström (0000-0001-5604-617X, University of Helsinki, autor correspondente), Atte Korhola (0000-0003-2577-6502, University of Helsinki), Panu Erästö (University of Helsinki), Lasse Holmström (University of Oulu) |
| Ano | 2006 |
| Volume | 66 |
| Fascículo | 1 |
| Páginas | 78-86 |
| Data de publicação | 2006-07-01 |
| Peer Reviewed | Sim |
| Open Access | Sim |
| Tipo | ARTICLE |
| Periódico | Quaternary Research (JOURNAL) |
| Identificadores do periódico | ISSN: 0033-5894 • E-ISSN: 1096-0287 |
| Editora | Cambridge University Press (CUP) (PUBLISHER) |
| DOI | 10.1016/j.yqres.2006.01.005 |
| OpenAlex | W2168560826 |
| Idioma | EN |
| Citações recebidas | 13 |
| Referências citadas | 33 |
Establishing natural climate variability becomes particularly important in remote polar regions, especially when considering questions regarding higher than average warming. We present a high-resolution record of temperature variability for the past 800 yr based on sedimentary diatoms from a treeline lake in Finnish Lapland. The BSiZer multiscale smoothing technique is applied to the data to identify significant features in the record at different temporal levels. The overall reconstruction shows relatively large multi-centennial temperature variability with a total range of about 0.6–0.8°C. At millennial scales, the temperatures exhibit a statistically significant long-term cooling trend prior to industrialization (Δ T = −0.03°C/century). At the centennial timescale, three warm time intervals were identified around AD 1200–1300 (terminal phase of the Medieval Warm Period, MWP), 1380–1550 and from 1920 until the present. Pronounced coolness occurred between AD 1600 and 1920, indicative of the Little Ice Age (LIA). At the decadal level, certain shorter-term climate excursions were revealed. The warmest ∼10–30 yr, non-overlapping periods occurred in AD 1220–1250, 1470–1500 and 1970–2000, respectively. The classic events of MWP and LIA are evident in our record, as is also the 20th century warming.
Archaeology · Centennial · Climate change · Climatology · Geography · Little ice age · Period (music) · Physical geography · Range (aeronautics) · Sedimentary rock · Climate change and permafrost · Geology · Geology and Paleoclimatology Research · Oceanography · Paleontology · Tree-ring climate responses
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| Obras citantes distintas | 13 |
|---|---|
| Citações por ano | 0,68 |
| Intervalo de citações | 2007 - 2026 (20) |
| Velocidade de citação | current |
| Altamente citado | Não |
| Tipos de citação | Neutras: 10 |