| dc.description.abstract | Earth’s climate has varied through time, with orbital forcing as the most dominant force on the
climate system the last million years, causing glacial-interglacial cycles. The last glacial period
ended about 11.6 thousand years (kyr), ago and the last interglacial maximum around 6.5 kyr
ago. A cooling trend towards a new glacial period followed, interrupted by the present human
caused global warming, mainly due to burning of fossil carbon. The United Nations Framework
Convention on Climate Change (UNFCCC) agreed upon the goal of the Paris Agreement 2015,
with the aim of holding the increase in the global average temperature to below 1.5 – 2 ºC from
pre-industrial temperatures. The Intergovernmental Panel on Climate Change (IPCC) has
defined the pre-industrial baseline to values of 1850-1900 CE, a period when global emissions
of greenhouse gases already had raised since the industrial revolution ca 1750 CE, and possibly
already have had effects on the temperature.
The phenomenon of Arctic Amplification is a more pronounced warming in the Arctic region,
with a present temperature rise of more than doubled compared to the global mean. Indications
of an earlier transition from pre-industrial to industrial climate in high northern latitudes have
been noticed and the aim in this thesis was to further explore this timing of the transition from
pre-industrial to industrial climate in high northern latitudes. To do so, tree-rings have been
used to reconstruct past temperatures.
Tree-rings provides a variety of proxies used for climate reconstructions, with the benefit of
being easily accessed, well replicated and available in regions suitable for climate studies. In
the Fennoscandian region, correlation between climate and tree-rings has proven to be good,
which has led to an extensive tradition of dendroclimatology. Here, updated tree-ring width
(TRW) and maximum latewood density (MXD) chronologies from Ammarnäs are presented,
built from Scots Pine wood sources, living and dead (preserved on the ground). The MXD
chronology was used as a base to investigate the timing of the transition to industrial climate.
The current warming could be detected and well defined in the updated MXD chronology from
Ammarnäs. The warming rate of the present exceeded earlier warming rates throughout the
chronology and a predominance of positive annual temperature anomalies could be seen
between 1900 – 2021 (reference period 1971 – 2000), instead of the substantial predominance
of negative annual temperature anomalies seen in all other centuries, except from the 16th
century. A vague negative long-term trend represents the pre-industrial period, interrupted by a
significant warming trend in the latest part of the chronology.
To further explore the time of transition to industrial climate in relation to latitude, three other
sites in central to northern Sweden; Rogen, Jämtland and Torneträsk, were analysed. The timing
of when the current warming started to emerge in the different data sets were decided by a
change point analysis. This resulted in a latitudinal comparison, where a possible trend towards
an earlier shift to industrial climate could be seen in the two more northern locations. The time
of change was seen in 1916 in Torneträsk (68ºN), 1915 in Ammarnäs (66ºN), 1932 in Jämtland
(63ºN) and 1929 in Rogen (62 ºN). This result does support the hypothesis of a possibly earlier
transition to industrial climate in higher northern latitudes compared to lower, but the analysis
contains few samples and would benefit from further replication. | en_US |
