Skip to main content

Cooling and Warming of Climate of the Earth’s Northern Hemisphere (On the Basis of Fluctuations of the Oxygen Isotope Δ18O and Dendrological Data) Cover

.blurhash-client-img { display: none !important; }

Cooling and Warming of Climate of the Earth’s Northern Hemisphere (On the Basis of Fluctuations of the Oxygen Isotope Δ18O and Dendrological Data)

Miscellanea Geographica

Volume 14 (2010): Issue 1 (December 2010)

By: Jerzy Boryczka, Maria Stopa-Boryczka, Arleta Unton-Pyziołek and Piotr Gieszcz

Open Access

|Nov 2018

Articles in this issue

DOI: https://doi.org/10.2478/mgrsd-2010-0005 | Journal eISSN: 2084-6118 | Journal ISSN: 0867-6046 (formerly 2084-6118)

Journal RSS Feed

Language: English

Page range: 47 - 58

Published on: Nov 25, 2018

Published by: Faculty of Geography and Regional Studies, University of Warsaw

In partnership with: Paradigm Publishing Services

Keywords:

isotope δ¹⁸O,

Pinus sylvestris,

tree the ring widths,

solar radiation,

moment of inertia of planets,

mass momentum of largest planets,

Related subjects:

Geosciences, other

© 2018 Jerzy Boryczka, Maria Stopa-Boryczka, Arleta Unton-Pyziołek, Piotr Gieszcz, published by Faculty of Geography and Regional Studies, University of Warsaw
This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License.

Volume 14 (2010): Issue 1 (December 2010)

Previous article