Dalton Minimum

E675175

The Dalton Minimum was a period of unusually low solar activity in the late 18th and early 19th centuries, associated with cooler global temperatures and climatic anomalies.

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All labels observed (1)

Label Occurrences
Dalton Minimum canonical 1

Statements (47)

Predicate Object
instanceOf climatic event
solar minimum
associatedWith Little Ice Age NERFINISHED
Tambora eruption
Year Without a Summer NERFINISHED
volcanic forcing
characterizedBy cooler Northern Hemisphere temperatures
frequent cold winters in some regions
low sunspot counts
reduced solar irradiance
classification grand solar minimum candidate
comparedTo Maunder Minimum NERFINISHED
Spörer Minimum NERFINISHED
documentedIn early instrumental temperature series
historical meteorological records
endTime circa 1830
fieldOfStudy climatology
paleoclimatology
solar physics
follows Maunder Minimum NERFINISHED
normal solar activity of the 18th century
hasApproximateDuration about 40 years
hasCause reduced sunspot activity
hasEffect climatic anomalies
cooler global temperatures
glacier advances in some mountain regions
harsh winters in parts of Europe
regional crop failures
hasLocation Sun NERFINISHED
hasLowerSolarActivityThan typical 20th century solar cycles
influences historical climate reconstructions
long-term climate variability
isDistinctFrom Maunder Minimum NERFINISHED
modern solar minimums
namedAfter John Dalton NERFINISHED
namedBy solar physicists and climatologists
observedIn climate proxy data
sunspot records
partOf periods of low solar activity
precedes modern maximum of solar activity
relevance study of solar–climate relationships
understanding natural climate variability
startTime circa 1790
temporalContext Industrial Revolution era
Napoleonic era NERFINISHED
timePeriod early 19th century
late 18th century

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Little Ice Age hasPart Dalton Minimum