Holocene high-resolution monsoon climate fluctuations in the Mu Us desert, China

2021 ◽  
Vol 55 (4) ◽  
pp. 265-276
Author(s):  
Dongfeng Niu ◽  
Yuejun Si ◽  
Baosheng Li ◽  
Fengnian Wang ◽  
Peixian Shu ◽  
...  
The Holocene ◽  
2016 ◽  
Vol 26 (6) ◽  
pp. 917-934 ◽  
Author(s):  
Pål Ringkjøb Nielsen ◽  
Nicholas L Balascio ◽  
Svein Olaf Dahl ◽  
Henrik Løseth Jansen ◽  
Eivind WN Støren ◽  
...  

2012 ◽  
Vol 8 (5) ◽  
pp. 4269-4294 ◽  
Author(s):  
A. A. Cimatoribus ◽  
S. S. Drijfhout ◽  
V. Livina ◽  
G. van der Schrier

Abstract. The largest variability in temperature over the last sixty thousand years is connected with Dansgaard-Oeschger events. Various prototype models have been proposed to explain these rapid climate fluctuations, but until now no observational constraint has been forwarded to choose between different theories. We assess the bimodality of the system reconstructing the topology of the multi-dimensional attractor over which the climate system evolves. Furthermore, we show that Dansgaard-Oeschger events are compatible with the crossing of a tipping point in the climate system. We use high-resolution ice core isotope data to investigate the statistical properties of the climate fluctuations in the period before the onset of the abrupt change. We find that the statistics are consistent with the switches between two different climate equilibrium states in response to a changing external forcing.


2013 ◽  
Vol 9 (1) ◽  
pp. 323-333 ◽  
Author(s):  
A. A. Cimatoribus ◽  
S. S. Drijfhout ◽  
V. Livina ◽  
G. van der Schrier

Abstract. Dansgaard–Oeschger events are a prominent mode of variability in the records of the last glacial cycle. Various prototype models have been proposed to explain these rapid climate fluctuations, and no agreement has emerged on which may be the more correct for describing the palaeoclimatic signal. In this work, we assess the bimodality of the system, reconstructing the topology of the multi-dimensional attractor over which the climate system evolves. We use high-resolution ice core isotope data to investigate the statistical properties of the climate fluctuations in the period before the onset of the abrupt change. We show that Dansgaard–Oeschger events have weak early warning signals if the ensemble of events is considered. We find that the statistics are consistent with the switches between two different climate equilibrium states in response to a changing external forcing (e.g. solar, ice sheets), either forcing directly the transition or pacing it through stochastic resonance. These findings are most consistent with a model that associates Dansgaard–Oeschger with changing boundary conditions, and with the presence of a bifurcation point.


2015 ◽  
Vol 74 (2) ◽  
pp. 929-935 ◽  
Author(s):  
Xiaoyan Zhu ◽  
Meiliang Zhang ◽  
Hai Cheng ◽  
Xia Wu ◽  
R. L. Edwards

1999 ◽  
Vol 156 (1-4) ◽  
pp. 245-284 ◽  
Author(s):  
L Wang ◽  
M Sarnthein ◽  
H Erlenkeuser ◽  
J Grimalt ◽  
P Grootes ◽  
...  

Geology ◽  
2006 ◽  
Vol 34 (5) ◽  
pp. 361 ◽  
Author(s):  
Matthew D. Jones ◽  
C. Neil Roberts ◽  
Melanie J. Leng ◽  
Murat Türkeş

1967 ◽  
Vol 31 ◽  
pp. 45-46
Author(s):  
Carl Heiles

High-resolution 21-cm line observations in a region aroundlII= 120°,b11= +15°, have revealed four types of structure in the interstellar hydrogen: a smooth background, large sheets of density 2 atoms cm-3, clouds occurring mostly in groups, and ‘Cloudlets’ of a few solar masses and a few parsecs in size; the velocity dispersion in the Cloudlets is only 1 km/sec. Strong temperature variations in the gas are in evidence.


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