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	<journal>
		<journal_title>Ocean Science</journal_title>
		<journal_url>www.ocean-sci.net</journal_url>
		<issn>1812-0784</issn>
		<eissn>1812-0792</eissn>
		<volume_number>5</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/os-5-591-2009</doi>
	<article_url>http://www.ocean-sci.net/5/591/2009/</article_url>
	<abstract_html>http://www.ocean-sci.net/5/591/2009/os-5-591-2009.html</abstract_html>
	<fulltext_pdf>http://www.ocean-sci.net/5/591/2009/os-5-591-2009.pdf</fulltext_pdf>
	<start_page>591</start_page>
	<end_page>605</end_page>
	<publication_date>2009-11-17</publication_date>
	<article_title content_type="html">On the multiple time scales of variability in the Northeast Pacific Ocean</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>R. Tokmakian</name>
			<email>rtt@nps.edu</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Oceanography, Naval Postgraduate School, Monterey, California, USA</affiliation>
	</affiliations>
	<abstract content_type="html">The spatial and temporal sea surface height energy distribution of
the Northeast Pacific Ocean is described and discussed. Using an
altimetric data set covering 15 years (1993â€“2007), the energy
within the 3â€“9 month band is primarily located within 10&amp;deg; of
the coast. In the Gulf of Alaska, this energy signal is on the
shelf, while further south, west of the California/Oregon coast, the
significant energy in this band is west of the shelf break. In both
cases, it is primarily forced by the local wind. Within the 2â€“3
year band, the signal reflects energy generated by local changes to
the wind stress from large atmospheric shifts indicated by the
Pacific North American Index and by advective or propagating
processes related to El NiÃ±o-Southern Oscillation. Over the two
4â€“6 year periods within this data set, the change is primarily due
to the large scale shift in atmospheric systems north of about
30&amp;deg; N which also affect changes in current strengths. Based
on the distribution of the energy signal and its variability, a set
of three winter-time indices are suggested to characterize the
distinct differences in the SSH anomalies in these areas.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Barnston, A. G. and Livezey, R. E: Classification, seasonality and persistence of low-frequency atmospheric circulation patterns, Mon. Weather Rev., 115, 1083â€“1126, 1987. </reference>
		<reference numeration="2" content_type="text"> Beamish, R. J., Neville, C. E., and Cass, A. J.: Production of Fraser River sockeye salmon (Oncorhynchus nerka) in relation to decadal-scale changes in the climate and the ocean, Can. J. Fish. Aquat. Sci., 54, 543â€“554, 1997. </reference>
		<reference numeration="3" content_type="text"> Capotondi, A., Alexander, M. A., Deser, C., and Miller, A. J.: Low-frequency pycnocline variability in the northeast Pacific, J. Phys. Oceanogr., 35, 1403â€“1420, 2005. </reference>
		<reference numeration="4" content_type="text"> Chelton, D. B. and Davis, R. E.: Monthly mean sea-level variability along the west coast of North America, J. Phys. Ocean., 12, 757â€“784, 1982. </reference>
		<reference numeration="5" content_type="text"> Codiga, D. L. and Eriksen, C. C.: Observations of low-frequency circulation and amplified subinertial tidal currents at Cobb Seamount, J. Geophys. Res., 102, 22993â€“23007, 1997. </reference>
		<reference numeration="6" content_type="text"> Cummins, P. F. and Lagerloef, G. S. E.: Low frequency pycnocline depth variability at the Station P in the northeast Pacific, J. Phys. Oceanogr., 32, 3207â€“3215, 2002. </reference>
		<reference numeration="7" content_type="text"> Douglass, E., Roemmich, D., and Stammer, D.: Interannual variability in northeast Pacific circulation, J. Geophys. Res., 111, C04001, doi:10.1029/2005JC003015, 2006. </reference>
		<reference numeration="8" content_type="text"> Ducet, N., Le Traon, P.-Y., and Reverdin, G.: Global high resolution mapping of ocean circulation from TOPEX/Poseidon and ERS-1 and -2, J. Geophys. Res., 105, 19477â€“19498, 2000. </reference>
		<reference numeration="9" content_type="text"> Farge, M., Wavelet transforms and their applications to turbulence, Annu. Rev. Fluid Mech., 24, 395â€“457, 1992. </reference>
		<reference numeration="10" content_type="text"> Gu, D. and Philander, G. H.: Secular changes of annual and interannual variability in the Tropics during the past century, J. Climate, 8, 864â€“876, 1995. </reference>
		<reference numeration="11" content_type="text"> Haney, R., Hale, R., and Dietrich, D.: Offshore propagation of eddy kinetic energy in the California Current, J. Geophys. Res., 106, 11709â€“11717, 2001. </reference>
		<reference numeration="12" content_type="text"> Kelly, K.A., Beardsley, R., Limeburner, R. C., Brink, K. H., Paduan, J. D., and Chereskin, T. K.: Variability of the near surface eddy kinetic energy in the California Current based on altimeter, drifter, and moored current data, J. Geophys. Res., 103, 13067â€“13083, 1998. </reference>
		<reference numeration="13" content_type="text"> Liu, P. C.: Wavelet spectrum analysis and ocean wind waves, Wavelets in Geophysics, edited by: Foufoula-Georgiou, E. and Kumar, P., Academic Press, 151â€“166, 1994. </reference>
		<reference numeration="14" content_type="text"> Lluch-Belda, D., Lluch-Cota, D. B., and Lluch-Cota, S.: Scales of Interannual Variability in the California Current System: associated phyical mechanisms and ecological impacts, CalCOFI Rep., 44, 76â€“85, 2003. </reference>
		<reference numeration="15" content_type="text"> Mantua, N. J., Hare, S. R. , Zhang, Y., Wallace, J. M., and Francis, R. C.: A Pacific Interdecadal Climate Oscillation with Impacts on Salmon Production, B. Am. Meteorol. Soc., 78, 1069â€“1979, 1997. </reference>
		<reference numeration="16" content_type="text"> Meyers, S. D., Kelly, B. G., and O&apos;Brien, J. J.: An introduction to wavelet analysis in oceanography and meteorology: With application to the dispersion of Yanai waves, Mon. Weather Rev., 21, 2858â€“2866, 1993. \bibitem[Smith and Sandwell(1996)] smith1996 Smith, W. H. F. and Sandwell, D. T.: Global seafloor topography from satellite altimetry and ship depth soundings, Science, 277, 195â€“196, 1996. </reference>
		<reference numeration="17" content_type="text"> Strub, P. T. and James, C.: Altimeter-derived surface circulation in the large-scale NE Pacific Gyres. Part 1. seasonal variability, Deep-Sea Res. II, 53, 163â€“183, 2002a. </reference>
		<reference numeration="18" content_type="text"> Strub, P. T. and James, C.: Altimeter-derived surface circulation in the large-scale NE Pacific Gyres. Part 2: 1997â€“1998 El NiÃ±o anomalies, Prog. Oceanogr., 53, 185â€“214, 2002b. </reference>
		<reference numeration="19" content_type="text"> Strub, P. T. and James, C.: The 1997â€“1998 oceanic El NiÃ±o signal along the southeast and northeast Pacific boundaries Ð an altimetric view, Prog. Oceanogr., 54, 439â€“458, 2002c. </reference>
		<reference numeration="20" content_type="text"> Tanimoto, Y., Iwsaka, N., Hanawa, K. and Toba, Y.: Characteristic variations of sea surface temperature with multiple time scales in the North Pacific, J. Climate, 6, 1153â€“1160, doi:10.1175/1520-0442(1993)006, 1993. </reference>
		<reference numeration="21" content_type="text"> Tokmakian, R. and McClean, J. L.: How realistic is the high frequency signal of a 0.1 \degree resolution ocean model?, J. Geophys. Res., 108, 3115, doi:10.1029/2002JC0014462003, 2003. </reference>
		<reference numeration="22" content_type="text"> Torrence, C. and Compo, G. P.: A practical guide to wavelet analysis, B. Am. Meteorol. Soc., 79, 61â€“78, online available at: http://paos.colorado.edu/research/wavelets/bams_79_01_0061.pdf, 1998. </reference>
		<reference numeration="23" content_type="text"> Wolter, K. and Timlin, M. S.: Monitoring ENSO in COADS with a seasonally adjusted principal component index. Proc. of the 17th Climate Diagnostics Workshop, Norman, OK, NOAA/N MC/CAC, NSSL, Oklahoma Clim. Survey, CIMMS and the School of Meteor., Univ. of Oklahoma, 52â€“57, 1993. </reference>
	</references>
</article>

