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The tenth IMSC, Beijing, China, 2007 - International Meetings on ...

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European trends c<strong>on</strong>tain large NAO-related signals, of which a major unknown part may<br />

be unrelated to the anthropogenic signal. <str<strong>on</strong>g>The</str<strong>on</strong>g>refore, we also examine the c<strong>on</strong>sistency of<br />

recent and projected changes after subtracting the NAO signal in both the observati<strong>on</strong>s and in<br />

the projecti<strong>on</strong>s. It turns out that even after the removal of the NAO signal, the pattern of trends<br />

in the observati<strong>on</strong>s are similar to those projected by the models. At the same time, the<br />

magnitude of the trends is c<strong>on</strong>siderably reduced and closer to the magnitude of the change in<br />

the projecti<strong>on</strong>s.<br />

Detecti<strong>on</strong> of external influence <strong>on</strong> trends of atmospheric storminess and northern oceans wave<br />

heights<br />

Speaker: Xiaolan L. Wang<br />

Xiaolan L. Wang<br />

Climate Research Divisi<strong>on</strong>, ASTD, STB, Envir<strong>on</strong>ment Canada, Tor<strong>on</strong>to, Ontario<br />

Xiaolan.Wang@ec.gc.ca<br />

Val R. Swail, Francis W. Zwiers, Xuebin Zhang,Yang Feng<br />

Climate Research Divisi<strong>on</strong>, ASTD, STB, Envir<strong>on</strong>ment Canada, Tor<strong>on</strong>to, Ontario<br />

<str<strong>on</strong>g>The</str<strong>on</strong>g> atmospheric storminess (as inferred from geostrophic wind energy) and ocean<br />

wave heights have increased in the cold seas<strong>on</strong>s over the past half century in the<br />

high-latitudes of the northern hemisphere (especially the northeast North Atlantic in boreal<br />

winter), and have decreased in more southerly northern latitudes. This study shows that these<br />

trend patterns c<strong>on</strong>tain a detectable resp<strong>on</strong>se to external forcing (i.e., both natural and<br />

anthropogenic forcing). <str<strong>on</strong>g>The</str<strong>on</strong>g> signal of external influence is found to be str<strong>on</strong>gest in the winter<br />

hemisphere, that is, in the northern hemisphere in January-February-March and in the<br />

southern hemisphere in July-August-September. However, the magnitude of the estimated<br />

resp<strong>on</strong>se to the forcing, which was obtained directly from climate models in the case of<br />

geostrophic wind energy and indirectly via an empirical downscaling procedure in the case of<br />

ocean wave heights, is significantly less than the magnitude of the observed changes in these<br />

parameters.<br />

Detecti<strong>on</strong> of Human Influence <strong>on</strong> 20th Century Precipitati<strong>on</strong> Trends<br />

Speaker: Xuebin Zhang<br />

Xuebin Zhang<br />

Envir<strong>on</strong>ment Canada<br />

Xuebin.Zhang@ec.gc.ca<br />

48

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