A 139-year dendroclimatic cycle, cultural/environmental history, sunspots, and longer-term cycles

Higher resolution time-stratigraphic records suggest correlation of lower frequency paleoclimatic events with Milankovitch obliquity/precessional cycles and of higher frequency events with the evidently resonance-related Pettersson maximum tidal force (MTF) model. Subsequently published records, mainly pollen, seemingly confirm that atmospheric resonances may have modulated past climatic changes in phase with average MTF cycles of 1668, 1112, and 556 years, as calculated in anomalistic years from planetary movements by Stacey. Stacey accepts Pettersson's dating of AD 1433 (517 YBP) for the last major perihelian spring tide based solely on calculations of moon- and earth-orbital relations to the sun. Use of AD 1433 as an origin for the tidal resonance model seemingly continues to provide a best fit for the timing of cyclical patterns in the presented paleoclimate time series.

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Bibliographic Details
Main Author: Karlstrom, Thor
Format: conference_item biblioteca
Language:English
Published: 1995
Subjects:Atmospheric Sciences, Earth Sciences, Environment, Oceanography, PACLIM, dendrochronology, palynology,
Online Access:http://hdl.handle.net/1834/31569
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spelling dig-aquadocs-1834-315692021-07-10T01:59:01Z A 139-year dendroclimatic cycle, cultural/environmental history, sunspots, and longer-term cycles Karlstrom, Thor Atmospheric Sciences Earth Sciences Environment Oceanography PACLIM dendrochronology palynology Higher resolution time-stratigraphic records suggest correlation of lower frequency paleoclimatic events with Milankovitch obliquity/precessional cycles and of higher frequency events with the evidently resonance-related Pettersson maximum tidal force (MTF) model. Subsequently published records, mainly pollen, seemingly confirm that atmospheric resonances may have modulated past climatic changes in phase with average MTF cycles of 1668, 1112, and 556 years, as calculated in anomalistic years from planetary movements by Stacey. Stacey accepts Pettersson's dating of AD 1433 (517 YBP) for the last major perihelian spring tide based solely on calculations of moon- and earth-orbital relations to the sun. Use of AD 1433 as an origin for the tidal resonance model seemingly continues to provide a best fit for the timing of cyclical patterns in the presented paleoclimate time series. 2021-06-24T17:11:46Z 2021-06-24T17:11:46Z 1995 conference_item http://hdl.handle.net/1834/31569 en application/pdf application/pdf 137-159 http://aquaticcommons.org/id/eprint/15755 8 2014-11-26 20:41:02 15755
institution UNESCO
collection DSpace
country Francia
countrycode FR
component Bibliográfico
access En linea
databasecode dig-aquadocs
tag biblioteca
region Europa del Oeste
libraryname Repositorio AQUADOCS
language English
topic Atmospheric Sciences
Earth Sciences
Environment
Oceanography
PACLIM
dendrochronology
palynology
Atmospheric Sciences
Earth Sciences
Environment
Oceanography
PACLIM
dendrochronology
palynology
spellingShingle Atmospheric Sciences
Earth Sciences
Environment
Oceanography
PACLIM
dendrochronology
palynology
Atmospheric Sciences
Earth Sciences
Environment
Oceanography
PACLIM
dendrochronology
palynology
Karlstrom, Thor
A 139-year dendroclimatic cycle, cultural/environmental history, sunspots, and longer-term cycles
description Higher resolution time-stratigraphic records suggest correlation of lower frequency paleoclimatic events with Milankovitch obliquity/precessional cycles and of higher frequency events with the evidently resonance-related Pettersson maximum tidal force (MTF) model. Subsequently published records, mainly pollen, seemingly confirm that atmospheric resonances may have modulated past climatic changes in phase with average MTF cycles of 1668, 1112, and 556 years, as calculated in anomalistic years from planetary movements by Stacey. Stacey accepts Pettersson's dating of AD 1433 (517 YBP) for the last major perihelian spring tide based solely on calculations of moon- and earth-orbital relations to the sun. Use of AD 1433 as an origin for the tidal resonance model seemingly continues to provide a best fit for the timing of cyclical patterns in the presented paleoclimate time series.
format conference_item
topic_facet Atmospheric Sciences
Earth Sciences
Environment
Oceanography
PACLIM
dendrochronology
palynology
author Karlstrom, Thor
author_facet Karlstrom, Thor
author_sort Karlstrom, Thor
title A 139-year dendroclimatic cycle, cultural/environmental history, sunspots, and longer-term cycles
title_short A 139-year dendroclimatic cycle, cultural/environmental history, sunspots, and longer-term cycles
title_full A 139-year dendroclimatic cycle, cultural/environmental history, sunspots, and longer-term cycles
title_fullStr A 139-year dendroclimatic cycle, cultural/environmental history, sunspots, and longer-term cycles
title_full_unstemmed A 139-year dendroclimatic cycle, cultural/environmental history, sunspots, and longer-term cycles
title_sort 139-year dendroclimatic cycle, cultural/environmental history, sunspots, and longer-term cycles
publishDate 1995
url http://hdl.handle.net/1834/31569
work_keys_str_mv AT karlstromthor a139yeardendroclimaticcycleculturalenvironmentalhistorysunspotsandlongertermcycles
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