Skip to main content Accessibility help
×
Hostname: page-component-76fb5796d-9pm4c Total loading time: 0 Render date: 2024-04-29T08:37:07.007Z Has data issue: false hasContentIssue false

Chapter VII - Summary and outlook

Published online by Cambridge University Press:  22 January 2010

G. J. Komen
Affiliation:
Royal Dutch Meteorological Service (KNMI), de Bilt, Holland
L. Cavaleri
Affiliation:
Istituto per lo Studio della Dinamica delle Grandi Masse, CNR, Venice
M. Donelan
Affiliation:
Canadian Centre for Inland Waters, Burlington, Ontario
K. Hasselmann
Affiliation:
Max-Planck-Institut für Meteorologie, Hamburg
S. Hasselmann
Affiliation:
Max-Planck-Institut für Meteorologie, Hamburg
P. A. E. M. Janssen
Affiliation:
European Centre for Medium-Range Weather Forecasts, Reading
Get access

Summary

Summary and outlook

The WAM group has realized its objectives: a third generation wave model has been developed; it runs in global and regional modes; it extended our understanding of the underlying physics; and data assimilation schemes have been developed and tested. This book is testimony of what has been achieved. However, careful reading will also reveal open ends, which range from small inconsistencies to major open issues. In this chapter we give an outlook on expected developments.

Compared to the so-called second generation models considerable progress has been made regarding the formulation of the evolution equation for the wave spectrum. The present WAM model is based on an explicit formulation of the physics of generation of waves by wind, nonlinear wave-wave interactions and dissipation due to whitecapping and bottom processes, rather than on the approach of ad hoc modelling which was commonplace with second generation models. The latter approach was shown to be inadequate under extreme circumstances such as hurricanes (SWAMP, 1985), while the WAM model gives for rapidly varying wind fields very satisfactory results (see chapter IV). Nevertheless, under ‘normal’ circumstances both approaches give similar results for the wave height. The reason for this is that although second generation models have inadequate physics they have been tuned to a considerable extent. Thus, the benefits of a third generation model are mainly related to a better representation of the spectrum itself and to a more explicit formulation of the underlying physics of wave evolution.

Despite the progress, we still are not able to make wave predictions that always fall within the error bands of the observations.

Type
Chapter
Information
Publisher: Cambridge University Press
Print publication year: 1994

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Save book to Kindle

To save this book to your Kindle, first ensure coreplatform@cambridge.org is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.

Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

Available formats
×

Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

Available formats
×