Cooling and Warming of Climate of the Earth’s Northern Hemisphere (On the Basis of Fluctuations of the Oxygen Isotope Δ18O and Dendrological Data)
Content fluctuations of the oxygen isotope δ18O in the Devon Island ice core during the last 100 000 years are a measure of climate fluctuations in the Northern Hemisphere. The course of content of the oxygen isotope δ18O and the sums of solar radiation reaching the upper edge of the atmosphere are...
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ftdoajarticles:oai:doaj.org/article:da5abfd3591a45a59b070347b3659418 2023-05-15T16:00:47+02:00 Cooling and Warming of Climate of the Earth’s Northern Hemisphere (On the Basis of Fluctuations of the Oxygen Isotope Δ18O and Dendrological Data) Boryczka Jerzy Stopa-Boryczka Maria Unton-Pyziołek Arleta Gieszcz Piotr 2010-12-01T00:00:00Z https://doi.org/10.2478/mgrsd-2010-0005 https://doaj.org/article/da5abfd3591a45a59b070347b3659418 EN eng Sciendo https://doi.org/10.2478/mgrsd-2010-0005 https://doaj.org/toc/2084-6118 2084-6118 doi:10.2478/mgrsd-2010-0005 https://doaj.org/article/da5abfd3591a45a59b070347b3659418 Miscellanea Geographica: Regional Studies on Development, Vol 14, Iss 1, Pp 47-58 (2010) isotope δ18o devon island pinus sylvestris picea abies tree the ring widths solar radiation periods moment of inertia of planets mass momentum of largest planets forecast Geography (General) G1-922 article 2010 ftdoajarticles https://doi.org/10.2478/mgrsd-2010-0005 2022-12-31T15:21:24Z Content fluctuations of the oxygen isotope δ18O in the Devon Island ice core during the last 100 000 years are a measure of climate fluctuations in the Northern Hemisphere. The course of content of the oxygen isotope δ18O and the sums of solar radiation reaching the upper edge of the atmosphere are characterized by approximate minima and maxima (by positive correlation). This proves that, during the last hundred thousand years, climate fluctuations (cooling and warming) in the Northern Hemisphere were conditioned by long-term changes of the orbit and altitude of the Earth’s axis. Climate fluctuation forecasts for the Northern Hemisphere were developed for the next 40 000 years on the basis of the established periods of change of the oxygen isotope δ18O and the known solar radiation periodicity. Climate changes in Europe during the last 25000 years were presented together with a forecast for 1000 years (according to organic substances in deposits and radiation) as well as climate changes in Europe in the period from -500 years BP to 2100 AD (according to δ18O and pine tree-rings). It showed that climate changes depended on the concentration of planet mass in relation to the ecliptic plane (from the gravitational impact of planets on the Sun). Concentration courses of planet mass in the Solar System and climate fluctuations in the Northern Hemisphere were compared. Of interest are examples of synchronic fluctuations, i.e. dispersal of planet mass in the Solar System, the widths of pine and spruce tree rings and air temperatures in Europe. Article in Journal/Newspaper Devon Island ice core Directory of Open Access Journals: DOAJ Articles Devon Island ENVELOPE(-88.000,-88.000,75.252,75.252) Miscellanea Geographica 14 1 47 58 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
isotope δ18o devon island pinus sylvestris picea abies tree the ring widths solar radiation periods moment of inertia of planets mass momentum of largest planets forecast Geography (General) G1-922 |
spellingShingle |
isotope δ18o devon island pinus sylvestris picea abies tree the ring widths solar radiation periods moment of inertia of planets mass momentum of largest planets forecast Geography (General) G1-922 Boryczka Jerzy Stopa-Boryczka Maria Unton-Pyziołek Arleta Gieszcz Piotr Cooling and Warming of Climate of the Earth’s Northern Hemisphere (On the Basis of Fluctuations of the Oxygen Isotope Δ18O and Dendrological Data) |
topic_facet |
isotope δ18o devon island pinus sylvestris picea abies tree the ring widths solar radiation periods moment of inertia of planets mass momentum of largest planets forecast Geography (General) G1-922 |
description |
Content fluctuations of the oxygen isotope δ18O in the Devon Island ice core during the last 100 000 years are a measure of climate fluctuations in the Northern Hemisphere. The course of content of the oxygen isotope δ18O and the sums of solar radiation reaching the upper edge of the atmosphere are characterized by approximate minima and maxima (by positive correlation). This proves that, during the last hundred thousand years, climate fluctuations (cooling and warming) in the Northern Hemisphere were conditioned by long-term changes of the orbit and altitude of the Earth’s axis. Climate fluctuation forecasts for the Northern Hemisphere were developed for the next 40 000 years on the basis of the established periods of change of the oxygen isotope δ18O and the known solar radiation periodicity. Climate changes in Europe during the last 25000 years were presented together with a forecast for 1000 years (according to organic substances in deposits and radiation) as well as climate changes in Europe in the period from -500 years BP to 2100 AD (according to δ18O and pine tree-rings). It showed that climate changes depended on the concentration of planet mass in relation to the ecliptic plane (from the gravitational impact of planets on the Sun). Concentration courses of planet mass in the Solar System and climate fluctuations in the Northern Hemisphere were compared. Of interest are examples of synchronic fluctuations, i.e. dispersal of planet mass in the Solar System, the widths of pine and spruce tree rings and air temperatures in Europe. |
format |
Article in Journal/Newspaper |
author |
Boryczka Jerzy Stopa-Boryczka Maria Unton-Pyziołek Arleta Gieszcz Piotr |
author_facet |
Boryczka Jerzy Stopa-Boryczka Maria Unton-Pyziołek Arleta Gieszcz Piotr |
author_sort |
Boryczka Jerzy |
title |
Cooling and Warming of Climate of the Earth’s Northern Hemisphere (On the Basis of Fluctuations of the Oxygen Isotope Δ18O and Dendrological Data) |
title_short |
Cooling and Warming of Climate of the Earth’s Northern Hemisphere (On the Basis of Fluctuations of the Oxygen Isotope Δ18O and Dendrological Data) |
title_full |
Cooling and Warming of Climate of the Earth’s Northern Hemisphere (On the Basis of Fluctuations of the Oxygen Isotope Δ18O and Dendrological Data) |
title_fullStr |
Cooling and Warming of Climate of the Earth’s Northern Hemisphere (On the Basis of Fluctuations of the Oxygen Isotope Δ18O and Dendrological Data) |
title_full_unstemmed |
Cooling and Warming of Climate of the Earth’s Northern Hemisphere (On the Basis of Fluctuations of the Oxygen Isotope Δ18O and Dendrological Data) |
title_sort |
cooling and warming of climate of the earth’s northern hemisphere (on the basis of fluctuations of the oxygen isotope δ18o and dendrological data) |
publisher |
Sciendo |
publishDate |
2010 |
url |
https://doi.org/10.2478/mgrsd-2010-0005 https://doaj.org/article/da5abfd3591a45a59b070347b3659418 |
long_lat |
ENVELOPE(-88.000,-88.000,75.252,75.252) |
geographic |
Devon Island |
geographic_facet |
Devon Island |
genre |
Devon Island ice core |
genre_facet |
Devon Island ice core |
op_source |
Miscellanea Geographica: Regional Studies on Development, Vol 14, Iss 1, Pp 47-58 (2010) |
op_relation |
https://doi.org/10.2478/mgrsd-2010-0005 https://doaj.org/toc/2084-6118 2084-6118 doi:10.2478/mgrsd-2010-0005 https://doaj.org/article/da5abfd3591a45a59b070347b3659418 |
op_doi |
https://doi.org/10.2478/mgrsd-2010-0005 |
container_title |
Miscellanea Geographica |
container_volume |
14 |
container_issue |
1 |
container_start_page |
47 |
op_container_end_page |
58 |
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1766396795457372160 |