Zobrazeno 1 - 10
of 997
pro vyhledávání: '"E. Grosch"'
Publikováno v:
Journal of Waterway, Port, Coastal, and Ocean Engineering; March 1987, Vol. 113 Issue: 2 p199-201, 3p
Publikováno v:
Journal of Waterway, Port, Coastal, and Ocean Engineering. 113:199-201
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::75da02526a9cbc22ad0606a201c8739e
https://doi.org/10.1061/(asce)0733-950x(1987)113:2(199)
https://doi.org/10.1061/(asce)0733-950x(1987)113:2(199)
Autor:
Stefan Schliep, Reinhard Dummer, Lucie Heinzerling, Gerhard Schuler, Frédéric Toussaint, Michael Erdmann, E. Grosch
Primary cutaneous CD8+ aggressive epidermotropic T-cell lymphoma (CD8+ AECTCL) is a very rare subtype of cutaneous T-cell lymphoma. The frequency is less than 1% of all primary cutaneous lymphomas and prognosis is poor with a 5-year disease specific
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c180ca53cd02baa85add983a72360aaa
https://doi.org/10.5167/uzh-201253
https://doi.org/10.5167/uzh-201253
Publikováno v:
Nonlinear Processes in Geophysics, Vol 4, Iss 2, Pp 71-91 (1997)
A particle-in-cell ansatz for solving the Euler equations in a rotating frame is described. The approach is ideally suited for 'layered' models of flows with sharp density and velocity fronts. The material and Coriolis accelerations in the Euler equa
Externí odkaz:
https://doaj.org/article/e067782e59dd485080f8bc30aa1b585f
Autor:
S. Wohlfart, E. Grosch, H. Schneider, J. Park, J. Hammersen, R. Mittwollen, Cristina Has, Erhard Hohenester
Publikováno v:
Journal of the European Academy of Dermatology and Venereology : JEADVReferences. 34(9)
Background A lack or dysfunction of the anchoring protein laminin-332 in the basement membrane leads to the skin blistering disorder junctional epidermolysis bullosa (JEB). The mutation c.628G>A in the gene LAMB3 encoding the laminin β3-chain is ass
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c2ae8c801dd83cf57e4d23b2f0002e46
https://pubmed.ncbi.nlm.nih.gov/32124492
https://pubmed.ncbi.nlm.nih.gov/32124492
Publikováno v:
Journal of Physical Oceanography. 46:2411-2436
Results are presented from the large-eddy simulations (LES) of a wind-driven flow representative of the shallow coastal ocean under the influences of Langmuir forcing and surface heating and cooling fluxes. Langmuir (wind and surface gravity wave) fo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a3299679d07882d5b5af1afcc02463a9
https://doi.org/10.1175/jpo-d-15-0168.1
https://doi.org/10.1175/jpo-d-15-0168.1
Publikováno v:
Journal of Physical Oceanography. 45:2869-2895
Interaction between the wind-driven shear current and the Stokes drift velocity induced by surface gravity waves gives rise to Langmuir turbulence in the upper ocean. Langmuir turbulence consists of Langmuir circulation (LC) characterized by a wide r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2bfe029379c8205716227f926a854764
https://doi.org/10.1175/jpo-d-14-0158.1
https://doi.org/10.1175/jpo-d-14-0158.1
Autor:
Chester E. Grosch, Ann E. Gargett
Publikováno v:
Journal of Physical Oceanography. 46:3595-3597
Existing large-eddy simulations (LES) of Langmuir supercells (LS) do not include rotational terms. Despite the fact that the actual coastal ocean is certainly affected by rotation, such simulations are found to provide excellent agreement with a wide
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::619db37c119bd1a1263bf171755c3de8
https://doi.org/10.1175/jpo-d-16-0092.1
https://doi.org/10.1175/jpo-d-16-0092.1
Publikováno v:
International Journal of Heat and Fluid Flow. 50:209-224
Results are presented from large-eddy simulations of an unstably stratified open channel flow, driven by a uniform pressure gradient and with zero surface shear stress and a no-slip lower boundary. The unstable stratification is applied by a constant
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b27172060ff3c547ab1b09681886e12a
https://doi.org/10.1016/j.ijheatfluidflow.2014.08.005
https://doi.org/10.1016/j.ijheatfluidflow.2014.08.005
Autor:
Chester E. Grosch, Ann E. Gargett
Publikováno v:
Journal of Physical Oceanography. 44:44-67
Turbulence in the ocean surface layer is generated by time-varying combinations of destabilizing surface buoyancy flux, wind stress forcing, and wave forcing through a vortex force associated with the surface wave field. Observations of time- and dep
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b1af9bd2525ebc48da088b1167c79d35
https://doi.org/10.1175/jpo-d-13-021.1
https://doi.org/10.1175/jpo-d-13-021.1