Articles | Volume 21, issue 3
https://doi.org/10.5194/npg-21-617-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/npg-21-617-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Distinguishing the effects of internal and forced atmospheric variability in climate networks
J. I. Deza
Departament de Física i Enginyeria Nuclear, Universitat Politècnica de Catalunya, Colom 11, 08222, Terrassa, Barcelona, Spain
C. Masoller
Departament de Física i Enginyeria Nuclear, Universitat Politècnica de Catalunya, Colom 11, 08222, Terrassa, Barcelona, Spain
M. Barreiro
Instituto de Física, Facultad de Ciencias, Universidad de la República, Iguà 4225, Montevideo, Uruguay
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The dynamics of our climate involves multiple timescales, and while a lot of work has been devoted to quantifying variations in time-averaged variables or variations in their seasonal cycles, variations in daily variability that occur over several decades still remain poorly understood. Here we analyse daily surface air temperature and demonstrate that inter-decadal changes can be precisely identified and quantified with the Hilbert analysis tool.
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Manuscript not accepted for further review
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We analyze the dynamical and statistical properties of two surface air temperature (SAT) reanalysis datasets. For each SAT time-series we analyze i) the distance between the lagged SAT time series and the insolation, and ii) the Shannon entropy computed from the probability distribution function (pdf) of SAT values. We show that these simple measures uncover meaningful long-range coherent spatial structures that emerge from the local properties of SAT time-series.
Fernando Arizmendi, Marcelo Barreiro, and Cristina Masoller
Earth Syst. Dynam. Discuss., https://doi.org/10.5194/esd-2016-12, https://doi.org/10.5194/esd-2016-12, 2016
Manuscript not accepted for further review
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Understanding how surface air temperature (SAT) is controlled by the incoming solar radiation is a fundamental and challenging problem in climate dynamics. Here we analyze the response of monthly-averaged SAT to solar forcing, and we also quantify the level of randomness of SAT variability. We find coherent spatial patterns which can be interpreted in terms of known climate phenomena.