12.08.2013 Views

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 ...

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

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 />

82

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!