Abstract
Abstract. Scania (Skåne in Swedish), southern Sweden, offers a particularly
interesting case for studying the historical relationship between climate
variability and grain production, given the favorable natural conditions in
terms of climate and soils for grain production, as well as the low share of
temperature-sensitive wheat varieties in its production composition. In this
article, a contextual understanding of historical grain production in
Scania, including historical, phenological, and natural geographic aspects,
is combined with a quantitative analysis of available empirical sources to
estimate the relationship between climate variability and grain production
between the years 1702 and 1911. The main result of this study is that grain production in Scania was primarily sensitive to climate variability during the high summer months of June and July, preferring cool and humid
conditions, and to some extent precipitation during the winter months,
preferring dry conditions. Diversity within and between historical grain
varieties contributed to making this risk manageable. Furthermore, no evidence is found for grain production being particularly
sensitive to climate variability during the spring, autumn, and harvest
seasons. At the end of the study period, these relationships were shifting
as the so-called early improved cultivars were being imported from other
parts of Europe. Finally, new light is shed on the climate history of
the region, especially for the late 18th century, previously argued to
be a particularly cold period, through homogenization of the early
instrumental temperature series from Lund (1753–1870).
Subject
Paleontology,Stratigraphy,Global and Planetary Change
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