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Continental Shelf Research 24 (2004) 1047–1051
Erratum
Erratum to ‘‘Development and application of a threedimensional baroclinic model to the study of the seasonal circulation in the Celtic Sea’’ [Continental Shelf Research 24 (2004) 13–36]$ E.F. Younga,*, J. Browna, J.N. Aldridgea, K.J. Horsburghb, L. Fernanda a
The Centre for Environment, Fisheries and Aquaculture Science, Pakefield Road, Lowestoft, Suffolk NR33 0HT, UK b School of Ocean Sciences, University of Wales Bangor, Menai Bridge LL59 5EY, UK
The Publisher regrets that Figs. 6–8 and 14 were inadvertently reproduced in black and white in the printed version of the above article. The colour versions of these figures appear in the on-line article and are also printed below. Please accept our apologies for any inconvenience caused by this matter.
$
doi of original article 10.1016/j.csr.2003.009.003 *Corresponding author. Current address: Proudman Oceanographic Laboratory, Bidston Observatory, Bidston Hill, Prenton, Merseyside CH43 7RA. Tel.: +44-151-653-1532; fax: +44-151-653-6269. E-mail addresses:
[email protected],
[email protected] (E.F. Young). 0278-4343/$ - see front matter Crown Copyright r 2004 Published by Elsevier Ltd. All rights reserved. doi:10.1016/j.csr.2004.02.001
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Erratum / Continental Shelf Research 24 (2004) 1047–1051
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(c) Fig. 6. Geographical distribution of errors in temperature prediction (modelled minus observed) for the first 2 weeks of model simulation (days 80–94). (a) Near-surface temperatures, (b) near-bed temperatures and (c) surface to bed temperature difference. Errors (E) expressed as E>0.5 C (red +), 0.5 CXEX 0.5 C (black &), Eo 0:5 C (blue ).
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(c) Fig. 7. Geographical distribution of errors in temperature prediction (modelled minus observed) during spring (days 80–151). (a) Near-surface temperatures, (b) near-bed temperatures and (c) surface to bed temperature difference. Errors (E) expressed as E > 0:5 C (red +), 0:5 CXEX 0:5 C (black &), Eo 0:5 C (blue ).
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Erratum / Continental Shelf Research 24 (2004) 1047–1051
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Fig. 8. Geographical distribution of errors in surface to bed temperature difference (modelled minus observed) for: (a) summer (days 152–243) and (b) autumn (days 244–334). Errors (E) expressed as E > 0:5 C (red +), 0:5 CXEX 0:5 C (black &), Eo 0:5 C (blue ).
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Fig. 14. Drifter trajectories for buoys released in the Celtic Sea in 1998. (a) Observed, (b) predicted and (c) predicted (assuming constant density). Lighter and dotted lines indicate model bathymetry. Start and end positions are indicated by and , respectively.