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Results 1-10 of 10 (Search time: 0.002 seconds).
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Issue Date
Title
Author(s)
2011
Identification of dynamical transitions in marine palaeoclimate records by recurrence network analysis
Donges, J.F.
;
Donner, R.V.
;
Rehfeld, K.
;
Marwan, N.
;
Trauth, M.H.
;
Kurths, J.
2011
Comparison of correlation analysis techniques for irregularly sampled time series
Rehfeld, K.
;
Marwan, N.
;
Heitzig, J.
;
Kurths, J.
2014
Networks from Flows - From Dynamics to Topology
Molkenthin, N.
;
Rehfeld, K.
;
Marwan, N.
;
Kurths, J.
2014
Characterizing the evolution of climate networks
Tupikina, L.
;
Rehfeld, K.
;
Molkenthin, N.
;
Stolbova, V.
;
Marwan, N.
;
Kurths, J.
2014
On the influence of spatial sampling on climate networks
Molkenthin, N.
;
Rehfeld, K.
;
Stolbova, V.
;
Tupikina, L.
;
Kurths, J.
2014
Testing the detectability of spatio-temporal climate transitions from paleoclimate networks with the start model
Rehfeld, K.
;
Molkenthin, N.
;
Kurths, J.
2015
Non-linear regime shifts in Holocene Asian monsoon variability: Potential impacts on cultural change and migratory patterns
Donges, J. F.
;
Donner, R. V.
;
Marwan, N.
;
Breitenbach, S. F. M.
;
Rehfeld, K.
;
Kurths, J.
2014
Similarity estimators for irregular and age-uncertain time series
Rehfeld, K.
;
Kurths, J.
2012
Constructing proxy records from age models (COPRA)
Breitenbach, S. F. M.
;
Rehfeld, K.
;
Goswami, B.
;
Baldin, J. U. L.
;
Ridley, H. E.
;
Kennett, D. J.
;
Prufer, K. M.
;
Aquino, V. V.
;
Asmerom, Y.
;
Polyak, V. J.
;
Cheng, H.
;
Kurths, J.
;
Marwan, N.
2015
Estimation of sedimentary proxy records together with associated uncertainty
Goswami, B.
;
Heitzig, J.
;
Rehfeld, K.
;
Marwan, N.
;
Anoop, A.
;
Prasad, S.
;
Kurths, J.
Discover
Author
7
Marwan, N.
4
Molkenthin, N.
2
Breitenbach, S. F. M.
2
Goswami, B.
2
Heitzig, J.
2
Stolbova, V.
2
Tupikina, L.
1
Anoop, A.
1
Aquino, V. V.
1
Asmerom, Y.
.
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Subject
7
550
5
paleoclimate
4
climate variation
4
uncertainty analysis
3
530
3
dating method
3
monsoon
3
proxy climate record
3
reconstruction
3
time series analysis
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2014
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2011
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2012
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