The tenth IMSC, Beijing, China, 2007 - International Meetings on ...
The tenth IMSC, Beijing, China, 2007 - International Meetings on ...
The tenth IMSC, Beijing, China, 2007 - International Meetings on ...
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Keywords: precipitati<strong>on</strong> trend, N<strong>on</strong>-parametric methods, Mann-Kendall, Sen's Estimator Slope,<br />
Iran<br />
L<strong>on</strong>g-range correlati<strong>on</strong>s of ERA-40 temperature data: Geographic patterns and height<br />
dependence<br />
Andrea Kiraly<br />
Department of Physics of Complex Systems, Lorand Eotvos University, Budapest, Hungary<br />
kiralya@lecso.elte.hu<br />
Imre M. Janosi<br />
Department of Physics of Complex Systems, Lorand Eotvos University, Budapest, Hungary<br />
Global temperature data from six pressure levels (1000hPa, 850hPa, 600hPa, 400hPa,<br />
200hPa, 100hPa) of the ERA-40 re-analisys data bank (temporal resoluti<strong>on</strong> of 6 hours,<br />
covered interval of 45 years, spatial resoluti<strong>on</strong> of 2.5°×2.5° lat/l<strong>on</strong>g) are analyzed in order to<br />
quantitatively characterize correlati<strong>on</strong> properties.<str<strong>on</strong>g>The</str<strong>on</strong>g> method of detrended fluctuati<strong>on</strong> analysis<br />
(DFA) is exploited, which has proven useful in revealing the extent of l<strong>on</strong>g-range correlati<strong>on</strong>s<br />
in various time series.<str<strong>on</strong>g>The</str<strong>on</strong>g> temperature records exhibit l<strong>on</strong>g-range temporal power-law<br />
correlati<strong>on</strong>s extending up to several years for all grid points.<str<strong>on</strong>g>The</str<strong>on</strong>g> correlati<strong>on</strong> exp<strong>on</strong>ent's<br />
geographic distributi<strong>on</strong> is quite complex at the lowermost pressure level 1000hPa, but it<br />
reproduces the spatial patterns detected for the observati<strong>on</strong>al data (e.g. several thousands of<br />
terrestrial daily temperature records from the Global Daily Climatology Network, GDCN).At<br />
higher levels the modifying effects of the surface are weaker, the spatial distributi<strong>on</strong> of<br />
exp<strong>on</strong>ent values becomes much smoother. Near the equator (between 15° S and 15° N) the<br />
level of correlati<strong>on</strong>s is str<strong>on</strong>g, inside the 30°-60° band exhibits a local minimum and towards<br />
the poles it becomes higher again <strong>on</strong> both hemispheres. This geographic pattern is similar to<br />
the distributi<strong>on</strong>s observed for some other meteorological parameters, e.g. the correlati<strong>on</strong><br />
exp<strong>on</strong>ent for oz<strong>on</strong>e c<strong>on</strong>centrati<strong>on</strong>s.<str<strong>on</strong>g>The</str<strong>on</strong>g>se results can serve as useful testbed for validating<br />
globally coupled numerical ocean-atmosphere models.<br />
Interpolati<strong>on</strong> methods of weather generator parameters<br />
Stanislava Kliegrova<br />
Czech Hydrometeorological Institute, Czech Republic<br />
stanislava.kliegrova@chmi.cz<br />
Martin Dubrovsky<br />
Institute of Atmospheric Physics, Czech Republic<br />
Ladislav Metelka<br />
Czech Hydrometeorological Institute, Czech Republic<br />
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