Abstract
Waning annual seasonality is documented in an up to one-month advance in spring onset since the 1980’s in northern latitudes, perturbing ecosystems and socio-economic performance. Summer temperatures, in contrast, have been rising only recently, indicating an offset in seasonal warming. The limited time span of this observational data makes the asynchronous pattern difficult to quantify, hindering projections of intra-annual dynamics. We explore temporal phase relations of seasonal warming over the Late Pleniglacial/Bølling and the Younger Dryas/Holocene climate transitions that preceded present anthropogenic warming. We determine past spring onset and thermal properties from dwarf birch paleo-phenology. Reconstructed spring warming led maximum summer warming by about a century during both transitions. Long-term reconstruction of intra-annual temperature regimes provides the perspective required for seasonal response analysis. Our results document that multi-decadal spring season warming precedes sudden summer temperature rise also during natural climate change. The rapidity of present seasonality changes, however, is unprecedented.
Original language | English |
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Pages (from-to) | 175-180 |
Number of pages | 6 |
Journal | GFF |
Volume | 141 |
Issue number | 3 |
DOIs | |
Publication status | Published - 3 Jul 2019 |
Bibliographical note
Funding Information:This work was supported by the Vetenskapsr?det [NT7-2016 04905]. We thank B. Wohlfarth, F. Schenck, and W.M. K?rschner for useful discussions. M.S. acknowledges funding from the Swedish Research Council (Starting Grant NT7-2016 04905) and additional support from the Bolin Centre for Climate Research, Stockholm University. Kevos Subarctic Research Station staff is acknowledged for help with leaf sampling and phenological observations. T. Donders, F. Bunnik, J.H.H. Bos and A.F. Lotter are acknowledged for the SCH pollenanalysis and July temperature reconstruction.
Funding Information:
We thank B. Wohlfarth, F. Schenck, and W.M. Kürschner for useful discussions. M.S. acknowledges funding from the Swedish Research Council (Starting Grant NT7-2016 04905) and additional support from the Bolin Centre for Climate Research, Stockholm University. Kevos Subarctic Research Station staff is acknowledged for help with leaf sampling and phenological observations. T. Donders, F. Bunnik, J.H.H. Bos and A.F. Lotter are acknowledged for the SCH pollenanalysis and July temperature reconstruction.
Publisher Copyright:
© 2019, © 2019 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group.
Funding
This work was supported by the Vetenskapsr?det [NT7-2016 04905]. We thank B. Wohlfarth, F. Schenck, and W.M. K?rschner for useful discussions. M.S. acknowledges funding from the Swedish Research Council (Starting Grant NT7-2016 04905) and additional support from the Bolin Centre for Climate Research, Stockholm University. Kevos Subarctic Research Station staff is acknowledged for help with leaf sampling and phenological observations. T. Donders, F. Bunnik, J.H.H. Bos and A.F. Lotter are acknowledged for the SCH pollenanalysis and July temperature reconstruction. We thank B. Wohlfarth, F. Schenck, and W.M. Kürschner for useful discussions. M.S. acknowledges funding from the Swedish Research Council (Starting Grant NT7-2016 04905) and additional support from the Bolin Centre for Climate Research, Stockholm University. Kevos Subarctic Research Station staff is acknowledged for help with leaf sampling and phenological observations. T. Donders, F. Bunnik, J.H.H. Bos and A.F. Lotter are acknowledged for the SCH pollenanalysis and July temperature reconstruction.
Keywords
- arctic amplification
- birch
- Climate change
- global warming
- phenology
- quaternary warming episodes
- seasonality
- spring onset
- undulation index