Adaptive non uniform grid; Baltic Sea; dense inflows
Abstract :
[en] Dense inflows into the permanently stratified Baltic Sea are renewing the deep waters in the central basins. The present study evaluates the performance of terrain-following coordinates, which are resolving the along-bottom flow, in an annual simulation covering several inflows reaching the deeper basins of the Baltic Sea in 2003. Therefor the simulations are carried out using sigma-coordinates and vertically adaptive coordinates for two different horizontal resolutions (2 NM and 1 NM). The simulations with the sigma coordinates could not reproduce the hydrography of the major Baltic inflows realistically due to discretisation errors such as numerical mixing and pressure gradient errors. It is shown that the adaptive coordinates improve the simulation, because numerical mixing is reduced and the model’s discretisation supports a more physically-justified representation of the physical processes. For the higher-resolution simulations, adding a parameterisation of internal mixing enhances the effective mixing in the simulation and induces a reduction of the numerical mixing. Additionally to the analysis of the model performance, the inflows’ hydrography as projected by the higher-resolution model using adaptive coordinates is presented. The characteristic cross-channel circulation of gravity currents in channelised bathymetry is found to be an essential feature of the inflow dynamics in the Baltic Sea. The usage of adaptive coordinates reduces the numerical mixing in the simulation as effective as the doubling of the horizontal resolution for sigma-coordinates. However, the numerical mixing accounts for at least 50 % of the salinity mixing in the simulations.
Research Center/Unit :
Centre Interfacultaire de Recherches en Océanologie - MARE - GHER
Disciplines :
Earth sciences & physical geography
Author, co-author :
Hofmeister, R.
Beckers, Jean-Marie ; Université de Liège - ULiège > Département d'astrophys., géophysique et océanographie (AGO) > GeoHydrodynamics and Environment Research (GHER)
Burchard, H.
Language :
English
Title :
Realistic modelling of the exceptional inflows into the central Baltic Sea in 2003 using terrain-following coordinates
scite shows how a scientific paper has been cited by providing the context of the citation, a classification describing whether it supports, mentions, or contrasts the cited claim, and a label indicating in which section the citation was made.
Bibliography
Axell L. On the variability of Baltic Sea deepwater mixing. J. Geophys. Res. 1998, 103:21667-21682.
Burchard, H., Bolding, K., 2002. GETM - a general estuarine transport model. Scientific documentation. Tech. Rep. EUR 20253 EN, European Commission.
Burchard H., Janssen F., Bolding K., Umlauf L., Rennau H. Model simulations of dense bottom currents in the Western Baltic Sea. Cont. Shelf Res. 2009, 29:205-220.
Burchard H., Rennau H. Comparative quantification of physically and numerically induced mixing in ocean models. Ocean Modell. 2008, 20:293-311.
Chassignet E.P., Hurlburt H.E., Smedstad O.M., Halliwell G.R., Wallcraft A.J., Metzger E.J., Blanton B.O., Lozano C., Rao D.B., Hogan P.J., Srinivasan A. Generalized vertical coordinates for eddy-resolving global and coastal ocean forecasts. Oceanography 2006, 19:20-31.
Cheng Y., Canuto V.M., Howard A.M. An improved model for the turbulent PBL. J. Atmos. Sci. 2002, 59:1550-1565.
Feistel R., Nausch G., Hagen E. Unusual Baltic inflow activity 2002/3 and varying deep-water properties. Oceanologia 2006, 48:21-35.
Feistel R., Nausch G., Heene T., Piechura J., Hagen E. Evidence for a warm water inflow into the Baltic Proper in summer 2003. Oceanologia 2004, 46:581-598.
Feistel R., Nausch G., Matthäus W., Hagen E. Temporal and spatial evolution of the Baltic deep water renewal in spring 2003. Oceanologia 2003, 45:623-642.
Fennel W., Radtke H., Schmidt M., Neumann T. Transient upwelling in the central Baltic Sea. Cont. Shelf Res. 2010, 30:2015-2026.
Fennel W., Seifert T., Kayser B. Rossby radii and phase speeds in the Baltic Sea. Cont. Shelf Res. 1991, 11:23-36.
Galperin B., Kantha L.H., Hassid S., Rosati A. A quasi-equilibrium turbulent energy model for geophysical flows. J. Atmos. Sci. 1988, 45:55-62.
Golenko N., Paka V., Golenko M., Korzh A. Meso-scale water structure in the southern Baltic in the summer of 2006. J. Mar. Sys. 2008, 74:S13-S19.
Halliwell G.R. Evaluation of vertical coordinate and vertical mixing algorithms in the HYbrid-Coordinate Ocean Model (HYCOM). Ocean Modell. 2004, 7:285-322.
Hofmeister R., Burchard H., Beckers J.-M. Non-uniform adaptive vertical grids for 3D numerical ocean models. Ocean Modell. 2010, 33:70-86.
ICES, 2009. Dataset on Ocean Hydrography, International Council for the Exploration of the Sea, Copenhagen. Available from: http://www.ices.dk/ocean.
Kremp C., Seifert T., Mohrholz V., Fennel W. The oxygen dynamics during the Baltic inflow events in 2001 to 2003 and the effect of different meteorological forcing - a model study. J. Mar. Sys. 2007, 67:13-30.
Lass H.U., Prantke H., Liljebladh B. Dissipation in the Baltic proper during winter stratification. J. Geophys. Res. 2003, 108:3187.
Lehmann A., Hinrichsen H.-H. On the thermohaline variability of the Baltic Sea. J. Mar. Sys. 2000, 25:333-357.
Lehmann A., Lorenz P., Jacob D. Modelling the exceptional Baltic Sea inflow events in 2002-2003. Geophys. Res. Lett. 2004, 31. 10.1029/2004GL020830.
Martinho A.S., Batteen M.L. On reducing the slope parameter in terrain-following numerical ocean models. Ocean Modell. 2006, 13:166-175.
Matthäus W. Mixing across the primary Baltic halocline. Beitr. Meeresk. 1990, 61:21-31.
Matthäus W., Frank H. Characteristics of major Baltic inflows - a statistical analysis. Cont. Shelf Res. 1992, 12:1375-1400.
Meier H.E.M. Modeling the pathways and ages of inflowing salt- and freshwater in the Baltic Sea. Estuarine Coastal Shelf Sci. 2007, 74(4):610-627.
Meier H.E.M., Döscher R., Broman B., Piechura J. The major Baltic inflow in January 2003 and preconditioning by smaller inflows in summer/autumn 2002: a model study. Oceanologia 2004, 46(4):557-579.
Paka V.T., Zhurbas V.M., Golenko N.N., Stefantsev L.A. Effects of the Ekman transport on the overflow of saline waters through the Slupsk Furrow in the Baltic Sea. Izvestiva Atmos. Ocean Phys. 1998, 34:641-648.
Piechura J., Beszczynska-Möller A. Inflow waters in the deep regions of the southern Baltic Sea - transport and transformations. Oceanologia 2003, 45:593-621. http://www.iopan.gda.pl/oceanologia/454piech.pdf.
Reissmann J.H., Burchard H., Feistel R., Hagen E., Lass H.U., Mohrholz V., Nausch G., Umlauf L., Wieczorek G. Vertical mixing in the Baltic Sea and consequences for eutrophication - a review. Prog. Oceanogr. 2009, 82:47-80.
Rennau H., Burchard H. Quantitative analysis of numerically induced mixing in a coastal model application. Ocean Dynamics 2009, 59:671-687.
Riemenschneider U., Legg S. Regional simulations of the Faroe Bank Channel overflow in a level model. Ocean Modell. 2007, 17:93-122.
Schinke H., Matthäus W. On the causes of major Baltic inflows - an analysis of long time series. Cont. Shelf Res. 1998, 18:67-97.
Seifert T., Kayser B. A high resolution spherical grid topography of the Baltic Sea. Meereswiss. Ber., Warnemünde 1995, 9:73-88.
Shchepetkin A.F., McWilliams J.C. A method for computing horizontal pressure-gradient force in an oceanic model with a nonaligned vertical coordinate. J. Geophys. Res. 2003, 108. 10.1029/2001JC001047.
She J., Berg P., Berg J. Bathymetry impacts on water exchange modelling through the Danish Straits. J. Mar. Sys. 2007, 65:450-459.
Umlauf L., Arneborg L. Dynamics of rotating shallow gravity currents passing through a channel. Part I: observation of transverse structure. J. Phys. Oceanogr. 2009, 39:2385-2401.
Umlauf L., Arneborg L. Dynamics of rotating shallow gravity currents passing through a channel. Part II: analysis. J. Phys. Oceanogr. 2009, 39:2402-2416.
Umlauf L., Arneborg L., Burchard H., Fiekas V., Lass H.U., Mohrholz V., Prandke H. The transverse structure of turbulence in a rotating gravity current. Geophys. Res. Lett. 2007, 34:L08601. 10.1029/2007GL029521.
Umlauf L., Arneborg L., Hofmeister R., Burchard H. Entrainment in shallow rotating gravity currents: a modeling study. J. Phys. Oceanogr. 2010, 40:1819-1834.
Umlauf L., Burchard H. Second-order turbulence models for geophysical boundary layers. A review of recent work. Cont. Shelf Res. 2005, 25:795-827.
Wåhlin A.K., Cenedese C. How entraining density currents influence the stratification in a one-dimensional ocean basin. Deep-Sea Res. II 2006, 53:172-193.
Wieczorek G., Hagen E., Umlauf L. Eastern Gotland Basin case study of thermal variability in the wake of deep water intrusions. J. Mar. Sys. 2008, 74:65-74.
Similar publications
Sorry the service is unavailable at the moment. Please try again later.
This website uses cookies to improve user experience. Read more
Save & Close
Accept all
Decline all
Show detailsHide details
Cookie declaration
About cookies
Strictly necessary
Performance
Strictly necessary cookies allow core website functionality such as user login and account management. The website cannot be used properly without strictly necessary cookies.
This cookie is used by Cookie-Script.com service to remember visitor cookie consent preferences. It is necessary for Cookie-Script.com cookie banner to work properly.
Performance cookies are used to see how visitors use the website, eg. analytics cookies. Those cookies cannot be used to directly identify a certain visitor.
Used to store the attribution information, the referrer initially used to visit the website
Cookies are small text files that are placed on your computer by websites that you visit. Websites use cookies to help users navigate efficiently and perform certain functions. Cookies that are required for the website to operate properly are allowed to be set without your permission. All other cookies need to be approved before they can be set in the browser.
You can change your consent to cookie usage at any time on our Privacy Policy page.