Digital Archives Initiative
Memorial University - Electronic Theses and Dissertations 4
menu off  add document to favorites : add page to favorites : reference url back to results : previous : next
 Search this object:
 0 hit(s) :: previous hit : next hit
  previous page : next page
Document Description
TitleRegional atmospheric dynamic downscaling over the subpolar North Atlantic
AuthorZhang, Ying, 1982-
DescriptionThesis (M.Sc.)--Memorial University of Newfoundland, 2010. Physics and Physical Oceanography
Paginationxiv, 108 leaves : col. ill., maps
SubjectAtmospheric circulation--North Atlantic Ocean--Mathematical models; Ocean circulation--North Atlantic Ocean--Mathematical models; Sea ice--North Atlantic Ocean--Computer simulation;
Degree GrantorMemorial University of Newfoundland. Dept. of Physics and Physical Oceanography
DisciplinePhysics and Physical Oceanography
Spatial CoverageNorth Atlantic Ocean
NotesIncludes bibliographical references (leaves 101-108).
AbstractThis study will present results from model simulations of high-resolution atmospheric seasonal and interannual variability in the subpolar North Atlantic from 1980 to 2005. A regional atmospheric model, the Weather Research and Forecasting (WRF) Model, is used in this study to downscale the NCEP/NCAR reanalysis for the subpolar North Atlantic Ocean. The WRF simulations represent realistically small-scale patterns in the surface water and heat fluxes in the central Labrador Sea and atmospheric variability related to the so-called Greenland tip jets. -- In the second part of this study the WRF model simulations are used to force an ocean coupled sea-ice model. The ocean model results are compared with the ocean simulation forced with the NCEP/NCAR reanalysis. It is shown that the winter deep convection and ocean subpolar circulation are improved in the simulations forced with the WRF atmospheric fields. In particular, the results show that severe winter events related to Greenland tip jets force intense winter convection in the Irminger Sea. The deep convection in the Labrador Sea and the Labrador Sea Water Mass properties are also more realistic in the ocean simulation force with the WRF results than in the simulation forced with the NCEP/NCAR reanalysis.
Resource TypeElectronic thesis or dissertation
FormatImage/jpeg; Application/pdf
SourcePaper copy kept in the Centre for Newfoundland Studies, Memorial University Libraries
Local Identifiera3496943
RightsThe author retains copyright ownership and moral rights in this thesis. Neither the thesis nor substantial extracts from it may be printed or otherwise reproduced without the author's permission.
CollectionElectronic Theses and Dissertations
Scanning StatusCompleted
PDF File(14.24 MB) --
CONTENTdm file name67805.cpd