EGU General Assembly 2008
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  List of Accepted Contributions - IS40 - NP3.04/HS1.8/NH10.5 Geophysical Extremes: scaling versus nonstationarity (co-organized by NP, HS & NH, co-listed in AS)

Please, click Abstract Number to find the corresponding abstract as PDF file; if necessary, download Adobe Acrobat Reader 4.0 first to open the file. Any abstract may be freely reproduced for non-commercial, scientific purposes; however, the moral right of the author(s) to be identified as the author(s) of such abstracts is asserted.

EGU2008-A-00008
Salami, T.
West African weather systems in the development of tropical cyclones

EGU2008-A-00570
Mukhamejanova, S.A.; Knyazeva, I.; Karimova, L.M.
Prediction of extreme geophysical events by methods of Markovian IFS

EGU2008-A-01298
García-Marín, A. P.; Ayuso-Muñoz, J. L.; Jiménez-Hornero, F.J.
Selecting the best intensity–duration-frequency model by using the multifractal approach

EGU2008-A-01527
Mori, S.
Tornado formation as geologically significant phenomena: interaction of geology to atmosphere series-1 (withdrawn)

EGU2008-A-02517
Hut, R.; Rutten, M.; Van de Giesen, N.
Non-stationarity of the Hurst coefficient in hydrological time series: Methodological artefact or observable property

EGU2008-A-04928
Radoane, M.; Feier, I.; Radoane, N.; Cristea, I.; Burdulea, A.
Fluvial deposits and environmental history of some large Romanian rivers

EGU2008-A-05615
Koutsoyiannis, D.
Emergence of antipersistence and persistence from a deterministic toy model

EGU2008-A-05634
Koutsoyiannis, D.
On detectability of nonstationarity from data using statistical tools

EGU2008-A-06387
Hamed, K. H.
Scaling versus deterministic trend in geophysical extremes: The case of river flow data

EGU2008-A-10682
Tchiguirinskaia, I.; Schertzer, D.; Lovejoy, S.
Multifractal flood frequency analysis

EGU2008-A-11451
Escandon, L.G.; Castro, J.J.; Carsteanu, A.A.
Effects of turbulence multifractality in pollutant dispersion

EGU2008-A-12223
Kerkhoven, E.; Gan, T. Y.
Estimating Unconditional Uncertainty of Streamflows of Athabasca and Fraser rivers of western Canada using Multifractal Analysis


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