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Mammoths lived in Arctic East Siberia. In this region there is not sufficient sunlight over the year for the growth of the plants on which these animals feed. Therefore the latitude of this region was lower before the end of the…

地球物理 · 物理学 2007-05-23 W. Woelfli , W. Baltensperger

The striking asymmetry of the ice cover during the Last Global Maximum suggests that the North Pole was in Greenland and then rapidly shifted to its present position in the Arctic See. A scenario which causes such a rapid geographic polar…

大气与海洋物理 · 物理学 2007-05-23 W. Woelfli , W. Baltensperger

In Arctic East Siberia many remains of mammoths have been found. In this region there is not sufficient sunlight over the year to allow for the growth of the plants on which these animals feed. Consequently the latitude of these regions…

地球物理 · 物理学 2007-05-23 W. Woelfli , W. Baltensperger

We propose a model for the Pleistocene Ice Age, assuming the following scenario: Between 3 Myr and 11.5 kyr BP a Mars-sized object existed which moved in a highly eccentric orbit. Originating from this object, gas clouds with a complex…

地球物理 · 物理学 2007-05-23 W. Woelfli , W. Baltensperger , R. Nufer

The astronomical theory of Milankovitch relates the changes of Earth' past climate to variations in insolation caused by oscillations of the orbital parameters. However, this theory has problems to account for some major observed phenomena…

大气与海洋物理 · 物理学 2007-05-23 W. Woelfli , W. Baltensperger

A comparison of northern and southern hemispheric paleotemperature profiles suggests that the Bolling-Allerod Interstadial, Younger Dryas stadial, and subsequent Preboreal warming which occurred at the end of the last ice age were…

综合物理 · 物理学 2007-05-23 Paul A. LaViolette

In Einstein's general relativity theory the metric component gxx in the direction of motion (x-direction) of the sun deviates from unity due to a tensor potential caused by the black hole existing around the center of the galaxy. Because…

综合物理 · 物理学 2008-10-14 Masataka Mizushima

Ice sheets appeared in the northern hemisphere around 3 million years ago and glacial-interglacial cycles have paced Earth's climate since then. Superimposed on these long glacial cycles comes an intricate pattern of millennial and…

地球物理 · 物理学 2015-03-19 Michel Crucifix

Reconstructions of the paleoclimate indicate that ancient climatic fluctuations on Earth are often correlated with variations in its orbital elements. However, the chaos inherent in the solar system's orbital evolution prevents numerical…

地球与行星天体物理 · 物理学 2024-02-15 Nathan A. Kaib , Sean N. Raymond

The solar activity in Cycle 23--24 shows differences from the previous cycles that were observed with modern instruments, e.g. long cycle duration and a small number of sunspots. To appreciate the anomalies further, we investigated the…

太阳与恒星天体物理 · 物理学 2015-06-16 Masumi Shimojo

We present a phase-space model that simulates Pleistocene ice volume changes based on Earth's orbital parameters. Terminations in the model are triggered by a combination of ice volume and orbital forcing and agree well with age estimates…

地球与行星天体物理 · 物理学 2015-03-19 John Z. Imbrie , Annabel Imbrie-Moore , Lorraine E. Lisiecki

Paleoclimate data help us assess climate sensitivity and potential human-made climate effects. We conclude that Earth in the warmest interglacial periods of the past million years was less than 1{\deg}C warmer than in the Holocene. Polar…

大气与海洋物理 · 物理学 2012-09-12 James E. Hansen , Makiko Sato

The Milankovitch theory states that the orbital eccentricity, precession, and obliquity of the Earth influence our climate by modulating the summer insolation at high latitudes in the northern hemisphere. Despite considerable success of…

地球与行星天体物理 · 物理学 2015-05-12 Fabo Feng , C. A. L. Bailer-Jones

Several researchers have previously identified a severe climatic upheaval in tropical North Africa that began just over 4000 years ago and lasted for about three centuries. The upheaval is known to have occurred shortly after a volcanic…

地球物理 · 物理学 2007-05-23 Douglas J. Keenan

The climate record preserved in polar glaciers, mountain glaciers, and widespread cave deposits shows repeated occurrence of abrupt global transitions between cold/dry stadial and warm/wet interstadial states during glacial periods. These…

大气与海洋物理 · 物理学 2009-07-03 Brian F. Farrell , Dorian S. Abbot

Recent work has provided ample evidence that nonlinear methods of time series analysis potentially allow for detecting periods of anomalous dynamics in paleoclimate proxy records that are otherwise hidden to classical statis- tical…

大气与海洋物理 · 物理学 2018-09-27 Jasper G. Franke , Reik V. Donner

Glaciations were attributed to variations of the Earths orbit (Milankovitch cycles). But the best ever dated paleoclimatic record (from a speleothem from Devils Hole, Nevada) demonstrated that the end of the last glacial period (termination…

地球物理 · 物理学 2009-09-10 Yavor Y. Shopov , Diana A. Stoykova , Katerina Stoitchkova , Anton Tanev

The Little Ice Age in Europe (between about 1350 and 1850) marked the largest glacier extent over the entire Holocene period. Although several authors have investigated the causes of the substantial glacier advances in the mid-19th century…

地球物理 · 物理学 2019-07-02 Matthias Huss , Simon Förster

The cause of the glacial cycles remains a mystery. The origin is widely accepted to be astronomical since paleoclimatic archives contain strong spectral components that match the frequencies of Earth's orbital modulation. Milankovitch…

大气与海洋物理 · 物理学 2007-05-23 J. Kirkby , A. Mangini , R. A. Muller

Glacial cycles redistribute water between oceans and continents causing pressure changes in the upper mantle, with consequences for melting of Earth's interior. Using Plio-Pleistocene sea-level variations as a forcing function, theoretical…

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