Zobrazeno 1 - 10
of 210
pro vyhledávání: '"Sutanu Sarkar"'
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 17, Pp n/a-n/a (2024)
Abstract A neutrally buoyant float deployed in an atmospherically driven turbulent ocean boundary layer on the dense side of a submesoscale front was repeatedly carried across the boundary layer by the turbulence and then trapped beneath the slumping
Externí odkaz:
https://doaj.org/article/53f65164c42741f287e4ad9d8bb9bffa
Publikováno v:
Biotechnology Reports, Vol 13, Iss C, Pp 26-29 (2017)
The present report explores the chromosomal patterns during meiosis as a fundamental cell division study in wild rice (Oryza rufipogon Griff.). Cytological assays revealed normal meiosis in most cases but in some instances meiotic abnormalities such
Externí odkaz:
https://doaj.org/article/50043397907a4cec8c33a68f8a615134
Publikováno v:
Journal of Physical Oceanography.
This work evaluates the fidelity of various upper ocean turbulence parameterizations subject to realistic monsoon forcing and presents a finite-time ensemble vector (EV) method to better manage the design and numerical principles of these parameteriz
Publikováno v:
Journal of Physical Oceanography. 52:1033-1048
Large-eddy simulations (LES) are employed to investigate the role of time-varying currents on the form drag and vortex dynamics of submerged 3D topography in a stratified rotating environment. The current is of the form Uc + Utsin(2πftt), where Uc i
Publikováno v:
South African Journal of Botany. 146:794-806
The high-Reynolds-number stratified wake of a slender body and its comparison with a bluff-body wake
Publikováno v:
Journal of Fluid Mechanics. 957
The high-Reynolds number stratified wake of a slender body is studied using a high-resolution hybrid simulation. The wake generator is a 6:1 prolate spheroid with a tripped boundary layer, the diameter-based body Reynolds number is $Re= U_\infty D/\n
Publikováno v:
3 Biotech. 13
Publikováno v:
XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
Thin Diurnal Warm Layers (DWLs) form near the surface of the ocean on days of large solar radiation, weak to moderate winds, and small surface waves. DWLs are characterized by complex dynamics, and are relevant to the ocean especially by modifying su
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::19a78d37223aeba85d68a0dd513b19ed
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017384
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5017384
Publikováno v:
Journal of Geophysical Research: Oceans. 128
Autor:
H.M. Aravind, Vicky Verma, Sutanu Sarkar, Mara A. Freilich, Amala Mahadevan, Patrick J. Haley, Pierre F.J. Lermusiaux, Michael R. Allshouse
Vertical transport in the ocean plays a critical role in the exchange of freshwater, heat, nutrients, and other biogeochemical tracers. While there are situations where vertical fluxes are important, studying the vertical transport and displacement o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::30287527164483c84032f06991f5b2f9
http://arxiv.org/abs/2209.10676
http://arxiv.org/abs/2209.10676