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The climate of Granada (southern Spain) during the first third of the 18th century (1706–1730) according to documentary sources
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Abstract. The climatic information recorded by the physician
Francisco Fernández Navarrete in Granada (southern Spain) during the
first third of the 18th century is analyzed in this work. His observations
are included in the book Cielo y suelo granadino ('Sky and soil in
Granada'), and consist of qualitative comments relating climatic conditions
to illness and diseases from 1706 to 1730, as well as instrumental
observations (using an “English barometer” and a “Florentine
thermometer”) from December 1728 to February 1730. To the best of our
knowledge, these are the earliest instrumental observations recorded in
Spain. An alternative methodology to Pfister indices, based on the frequency
of extreme events, was applied to study this new set of documentary data. The
analysis shows that seasonal mean values of temperature and precipitation
during the period 1706–1730 were very similar to those of periods of similar
length at the beginning of the 20th century, such as 1906–1930. However,
some years were especially extreme, such as the dry first half of the 1720s
or the winter of 1728–1729 when a strong cold wave affected the city.
Title: The climate of Granada (southern Spain) during the first third of the 18th century (1706–1730) according to documentary sources
Description:
Abstract.
The climatic information recorded by the physician
Francisco Fernández Navarrete in Granada (southern Spain) during the
first third of the 18th century is analyzed in this work.
His observations
are included in the book Cielo y suelo granadino ('Sky and soil in
Granada'), and consist of qualitative comments relating climatic conditions
to illness and diseases from 1706 to 1730, as well as instrumental
observations (using an “English barometer” and a “Florentine
thermometer”) from December 1728 to February 1730.
To the best of our
knowledge, these are the earliest instrumental observations recorded in
Spain.
An alternative methodology to Pfister indices, based on the frequency
of extreme events, was applied to study this new set of documentary data.
The
analysis shows that seasonal mean values of temperature and precipitation
during the period 1706–1730 were very similar to those of periods of similar
length at the beginning of the 20th century, such as 1906–1930.
However,
some years were especially extreme, such as the dry first half of the 1720s
or the winter of 1728–1729 when a strong cold wave affected the city.
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