Enhanced climate variability in the tropics: a 200 000 yr annual record of monsoon variability from Pangea's equator

A continuous series of 209 000 evaporite varves from the equator of arid western Pangea (age = −255 ma), as a proxy for surface temperature, has a complete suite of Milankovitch cycles and harmonics as expected for a rectified reaction to precession-modulated insolation at the equator. Included are...

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Main Author: R. Y. Anderson
Format: Article
Language:English
Published: Copernicus Publications 2011-07-01
Series:Climate of the Past
Online Access:http://www.clim-past.net/7/757/2011/cp-7-757-2011.pdf
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spelling doaj-8c5685e362394bffa6bb97480f3260492020-11-25T00:59:40ZengCopernicus PublicationsClimate of the Past1814-93241814-93322011-07-017375777010.5194/cp-7-757-2011Enhanced climate variability in the tropics: a 200 000 yr annual record of monsoon variability from Pangea's equatorR. Y. AndersonA continuous series of 209 000 evaporite varves from the equator of arid western Pangea (age = −255 ma), as a proxy for surface temperature, has a complete suite of Milankovitch cycles and harmonics as expected for a rectified reaction to precession-modulated insolation at the equator. Included are modes of precession (23.4 kyr, 18.2 kyr), semi-precession (11.7 kyr, 9.4 kyr), and harmonics at ~7 kyr and 5.4 kyr. An oscillation of ~100 kyr, with 35 % of total variance, originates as an amplitude modulation of precession cycles. An exceptionally strong 2.3 kyr quasi-bi-millennial oscillation (QBMO) appears to have had its own source of forcing, possibly solar, with its amplitude enhanced at Milankovitch frequencies. Seasonal information in varves traces the rectifying process to asymmetrical distribution of Pangea relative to the equator, and its effect on monsoonal circulation and heat flow near the equator during summer solstices in the hemispheres.http://www.clim-past.net/7/757/2011/cp-7-757-2011.pdf
collection DOAJ
language English
format Article
sources DOAJ
author R. Y. Anderson
spellingShingle R. Y. Anderson
Enhanced climate variability in the tropics: a 200 000 yr annual record of monsoon variability from Pangea's equator
Climate of the Past
author_facet R. Y. Anderson
author_sort R. Y. Anderson
title Enhanced climate variability in the tropics: a 200 000 yr annual record of monsoon variability from Pangea's equator
title_short Enhanced climate variability in the tropics: a 200 000 yr annual record of monsoon variability from Pangea's equator
title_full Enhanced climate variability in the tropics: a 200 000 yr annual record of monsoon variability from Pangea's equator
title_fullStr Enhanced climate variability in the tropics: a 200 000 yr annual record of monsoon variability from Pangea's equator
title_full_unstemmed Enhanced climate variability in the tropics: a 200 000 yr annual record of monsoon variability from Pangea's equator
title_sort enhanced climate variability in the tropics: a 200 000 yr annual record of monsoon variability from pangea's equator
publisher Copernicus Publications
series Climate of the Past
issn 1814-9324
1814-9332
publishDate 2011-07-01
description A continuous series of 209 000 evaporite varves from the equator of arid western Pangea (age = −255 ma), as a proxy for surface temperature, has a complete suite of Milankovitch cycles and harmonics as expected for a rectified reaction to precession-modulated insolation at the equator. Included are modes of precession (23.4 kyr, 18.2 kyr), semi-precession (11.7 kyr, 9.4 kyr), and harmonics at ~7 kyr and 5.4 kyr. An oscillation of ~100 kyr, with 35 % of total variance, originates as an amplitude modulation of precession cycles. An exceptionally strong 2.3 kyr quasi-bi-millennial oscillation (QBMO) appears to have had its own source of forcing, possibly solar, with its amplitude enhanced at Milankovitch frequencies. Seasonal information in varves traces the rectifying process to asymmetrical distribution of Pangea relative to the equator, and its effect on monsoonal circulation and heat flow near the equator during summer solstices in the hemispheres.
url http://www.clim-past.net/7/757/2011/cp-7-757-2011.pdf
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