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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esults, the guidance <strong>on</strong> the determinati<strong>on</strong> of threshold for binary forecast is proposed for each<br />
pattern.<br />
Using this guidance, the heavy snow forecast in Korea is c<strong>on</strong>sidered as a case study.<br />
Effects of daily MOC fluctuati<strong>on</strong>s <strong>on</strong> l<strong>on</strong>g-term MOC predictability<br />
Speaker: Jin-S<strong>on</strong>g v<strong>on</strong> Storch<br />
Jin-S<strong>on</strong>g v<strong>on</strong> Storch<br />
Max-Planck Institute for Meteorology<br />
jin-s<strong>on</strong>g.v<strong>on</strong>.storch@zmaw.de<br />
Helmuth Haak<br />
Max-Planck Institute for Meteorology<br />
<str<strong>on</strong>g>The</str<strong>on</strong>g> first c<strong>on</strong>tinuous assessment of the Atlantic meridi<strong>on</strong>al overturning circulati<strong>on</strong><br />
(MOC), achieved within the framework of the UK Rapid Climate Change Program, indicates<br />
str<strong>on</strong>g MOC variability <strong>on</strong> timescales of about a few weeks. A large part of this variability<br />
results from or is related to the wind stress forcing. Assume that this MOC variability is not<br />
predictable bey<strong>on</strong>d a few weeks, its presence will significantly limit the l<strong>on</strong>g-term MOC<br />
predicti<strong>on</strong>s which owe their skill to the slow ocean dynamics. To quantify this limitati<strong>on</strong>, daily<br />
and yearly MOC time series generated by the ECHAM/MPI-OM model are used to test two null<br />
hypothesis: <strong>on</strong>e addresses the existence of the slow dynamics and the other the strength of<br />
the variability generated by the slow dynamics relative to the low-frequency white-noise<br />
extensi<strong>on</strong> of the unpredictable short-term fluctuati<strong>on</strong>s. <str<strong>on</strong>g>The</str<strong>on</strong>g> analysis is carried out for different<br />
frequency ranges by decomposing the variances in frequency domain. It is found that the<br />
model slow dynamics start to operate <strong>on</strong> timescales l<strong>on</strong>ger than two to three years and the<br />
variance generated by the slow dynamics can <strong>on</strong>ly be over and above the low-frequency<br />
white-noise extensi<strong>on</strong> of the unpredictable noise when c<strong>on</strong>sidering timescales l<strong>on</strong>ger than 20<br />
years. <str<strong>on</strong>g>The</str<strong>on</strong>g> result suggests that when predicting the MOC by initializing the ECHAM/MPI-OM<br />
model using an ocean analysis, a l<strong>on</strong>g initializati<strong>on</strong> time period, preferably l<strong>on</strong>ger than 20<br />
years, is required to capture the state of slow dynamics at the initial time.<br />
On the reliability of ENSO dynamical predicti<strong>on</strong>s<br />
Speaker: Youmin Tang<br />
Youmin Tang<br />
University of Northern British Columbia, Canada<br />
ytang@unbc.ca<br />
Richard Kleeman<br />
Courant Institute, New York University, USA<br />
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