Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Mehrshad Foroughan"'
Autor:
Seyed Mahmood Hamze-Ziabari, Mehrshad Foroughan, Ulrich Lemmin, Rafael Sebastian Reiss, David Andrew Barry
Publikováno v:
Frontiers in Marine Science, Vol 10 (2023)
Theoretical studies on oceans and large lakes have shown that submesoscale instabilities in frontal zones tend to reduce horizontal density gradients and enhance vertical density gradients, thereby re-stratifying the Surface Mixed Layer (SML). Submes
Externí odkaz:
https://doaj.org/article/56b7137062dc4357ae59a2e7778d44f8
Publikováno v:
Journal of Limnology, Vol 81, Iss 1 (2022)
The spatial variability of lake surface water temperature (LSWT) between smooth and rough surface areas and its potential association with the natural surfactant distribution in the surface microlayer were investigated for the first time in a lake. I
Externí odkaz:
https://doaj.org/article/e9a3c9312bf546bebff108a636bbdd1e
Publikováno v:
Remote Sensing, Vol 14, Iss 19, p 4967 (2022)
As in oceans, large-scale coherent circulations such as gyres and eddies are ubiquitous features in large lakes that are subject to the Coriolis force. They play a crucial role in the horizontal and vertical distribution of biological, chemical and p
Externí odkaz:
https://doaj.org/article/9d43b8da3a31418a8df99ed1723c4e2e
Publikováno v:
Proceedings of the Institution of Mechanical Engineers, Part C: Journal of Mechanical Engineering Science. 236:4015-4025
Although hydropower is a clean source of energy, in some cases, it can jeopardize the life of some species of riverine fish. Very Low Head (VLH) water turbine is an innovative design that aims at reducing the adverse effects of such hydroelectric fac
Autor:
Seyed Mahmood Hamze-Ziabari, Ulrich Lemmin, Mehrshad Foroughan, Rafael S. Reiss, D. Andrew Barry
Basin-scale quasi-geostrophic gyres are common features of large lakes subject to Coriolis force. Cyclonic gyres are often characterized by dome-shaped thermoclines that form due to pelagic upwelling which takes place in their center. At present, dyn
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eca45e2a2fb869b99a7f19062eee7ba9
https://doi.org/10.22541/essoar.167161029.94177941/v1
https://doi.org/10.22541/essoar.167161029.94177941/v1
Publikováno v:
Remote Sensing; Volume 14; Issue 19; Pages: 4967
As in oceans, large-scale coherent circulations such as gyres and eddies are ubiquitous features in large lakes that are subject to the Coriolis force. They play a crucial role in the horizontal and vertical distribution of biological, chemical and p
Autor:
Seyed Mahmood Hamze-Ziabari, Ulrich Lemmin, Frédéric Soulignac, Mehrshad Foroughan, David Andrew Barry
In large lakes subject to the Coriolis force, basin-scale gyres and mesoscale eddies, i.e. rotating coherent water masses, play a key role in spreading biochemical materials and energy throughout the lake. In order to assess the spatial and temporal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f53f9870f0aad293c7def6a14f2025b1
https://doi.org/10.5194/gmd-2022-104
https://doi.org/10.5194/gmd-2022-104
Randomly distributed patches of smooth or rough/rippled surfaces are readily observed on most water bodies. Smooth surface patches are called natural slicks and typically form under low wind conditions (< 6 m s-1) when biogenic surfactants in the sur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a4e3077efc4bfc89189a3eab5012737b
https://doi.org/10.5194/egusphere-egu22-12027
https://doi.org/10.5194/egusphere-egu22-12027
The spatial variability of lake surface water temperature (LSWT) between smooth and rough surface areas and its potential association with the natural surfactant distribution in the surface microlayer were investigated for the first time in a lake. I
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d272a837c648dbabff2b3f1c1d15fb15
https://infoscience.epfl.ch/record/295431
https://infoscience.epfl.ch/record/295431
Submesoscale fronts often become visible when the accumulation of biosurfactants in the water surface microlayer causes smooth surfaces, called frontal slicks, to develop. Based on in situ and remotely-sensed data, a frontal slick was documented for
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b45cffc85c723305bac7ea47c81df8df
https://infoscience.epfl.ch/record/297503
https://infoscience.epfl.ch/record/297503